index,Core_ID,lake,lat,lon,collection_year,core_length_m,uppermost_sample_depth,minimum_sample_spacing,mean_upper_core_spacing,lithology,grain_size,mineralogy,TOC/organic matter,carbonate,pollen,diatoms,molluscs,ostracods,foraminifera,metals/geochemistry,number_14C_dates,shallowest_date_depth,youngest_date,chronology_quality,published_study,archive_status,RoC_utility,record_type,approx_location,lake_relation,chronological_method,modern_time_span,sedimentation_rate,scoring_reason,source_url,DOI,evidence_status,data_recovery_status,target_lake_relevance,modern_chronology_score,resolution_score,quantitative_proxy_count,special_reanalysis_candidate,priority_action,confidence 0,S1,Manzala,31.448333333333334,31.778333333333332,1985,28.96,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,6.0,2.0,2360.0,6 successful 14C ages individually verified from Table 2; shallowest dated sample 2.0 m; youngest reported age 2360 yr BP. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In Abbas Zahir,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 1,S2,Manzala,31.305,31.605,1985,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,6.0,1.5,1830.0,6 successful 14C ages individually verified from Table 2; shallowest dated sample 1.5 m; youngest reported age 1830 yr BP. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.2 km ENE Abu Hammuda,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 2,S3,Manzala,31.296666666666667,31.723333333333333,1985,29.87,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,6.0,3.0,3030.0,6 successful 14C ages individually verified from Table 2; shallowest dated sample 3.0 m; youngest reported age 3030 yr BP. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.9 km SW El Ghuneimiya,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 3,S4,Manzala,31.22833333333333,31.515,1985,32.46,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,8.0,1.0,2150.0,8 successful 14C ages individually verified from Table 2; shallowest dated sample 1.0 m; youngest reported age 2150 yr BP. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.5 km NNW El Hisas,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 4,S5,Manzala,31.193333333333335,31.65833333333333,1985,27.43,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,8.0,2.0,1450.0,8 successful 14C ages individually verified from Table 2; shallowest dated sample 2.0 m; youngest reported age 1450 yr BP. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1 km NW Nasi Ez. Hasan Shakir,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 5,S6,Manzala,31.108333333333334,31.71,1985,26.37,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,5.0,1.5,1910.0,5 successful 14C ages individually verified from Table 2; shallowest dated sample 1.5 m; youngest reported age 1910 yr BP. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.5 km E El Gineina,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 6,S7,Manzala,31.13,31.871666666666666,1985,24.38,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,12.0,1.5,2110.0,12 successful 14C ages individually verified from Table 2; shallowest dated sample 1.5 m; youngest reported age 2110 yr BP. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,6.5 km SW Manzalah,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 7,S8,Manzala,31.21333333333333,32.038333333333334,1985,41.3,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,2.5 km N El Matariya,Manzala sector (preliminary; not necessarily in-lake),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 8,S9,Other/control,30.97833333333333,31.878333333333334,1985,15.7,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1 km E San El Hagar El Qibliya,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 9,S10,Other/control,30.85666666666667,32.019999999999996,1985,24.38,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,2 km NNE El Munagat El Kubra,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 10,S11,Other/control,30.92,32.306666666666665,1985,29.87,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,3.5 km SE Ez. El Cop,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 11,S12,Other/control,31.063333333333333,32.555,1985,23.77,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,2.5 km NE Tel El Farama,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 12,S13,Other/control,31.078333333333333,32.39333333333333,1985,30.48,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,Israeli Rd. 7.8 km E of Suez Canal,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 13,S14,Other/control,30.998333333333335,32.47,1985,23.16,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,7.5 km WSW Baluza,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 14,S15,Other/control,31.125,32.505,1985,35.36,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,9 km NW Tel El Farama,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 15,S16,Other/control,31.360000000000003,32.06333333333333,1985,28.04,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Coutellier & Stanley (1987); Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1 km WSW Ez. Shalabi El Rudi,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 16,S17,Other/control,31.378333333333334,31.965,1985,43.28,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Targeted in some Manzala-area long-core samples (Leroy 1992); core-specific coverage unresolved,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Coutellier & Stanley (1987); Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.7 km NE Geziret Umm Abdalla,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 17,S18,Other/control,31.078333333333333,32.34166666666667,1987,53.19,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,11.5 km WNW Tel Farama,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 18,S19,Other/control,31.048333333333336,32.55,1987,12.19,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,At Tel Farama,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 19,S20,Other/control,31.110000000000003,32.30166666666666,1987,50.29,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1 km W Suez Canal NE Extension,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 20,S21,Other/control,31.229999999999997,32.34166666666667,1987,49.38,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,3 km SE Port Fouad,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 21,S22,Other/control,31.021666666666665,32.208333333333336,1987,37.8,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,2 km W Ushash Arab Zeidan,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 22,S23,Other/control,30.83,32.25333333333333,1987,13.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,In Alawi Umm El Rish,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 23,S24,Other/control,30.851666666666667,32.17166666666667,1987,10.97,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,5.5 km SW Ushash Ibrahim Abu Muh,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 24,S25,Other/control,30.961666666666666,32.18,1987,14.33,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,4 km SW Ushash Arab El Gadadia,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 25,S26,Other/control,30.906666666666666,32.13,1987,13.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.2 km SE Minshat Abu Omar,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 26,S27,Other/control,31.006666666666668,32.031666666666666,1987,15.24,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley (1988b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,3 km S Ubash Mallaha,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 27,S28,Other/control,31.441666666666666,31.555,1987,36.58,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.7 km SSW Ez. El Gamasa El Shardya,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 28,S29,Other/control,31.361666666666668,31.451666666666664,1987,39.62,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.5 km W Ez. El Mazia,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 29,S30,Other/control,31.40833333333333,32.01166666666666,1987,42.67,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,4 km NW Ez. Shalabi Rudi,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 30,S31,Other/control,31.368333333333332,31.6,1988,45.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,2.5 km E Kafr Wastani,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 31,S32,Other/control,31.279999999999998,31.40833333333333,1988,21.34,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.3 km SW Hagg Shirbin Ez. Bahr El Ish,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 32,S33,Other/control,31.411666666666665,31.363333333333333,1988,25.91,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.5 km N Ez. El Gezira,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 33,S34,Other/control,31.453333333333333,31.388333333333332,1988,39.62,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,2 km N Abu Madi,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 34,S35,Other/control,31.528333333333332,31.308333333333334,1988,35.05,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1 km SE Qabr Sidi Durrgnam,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 35,S36,Other/control,31.46333333333333,31.256666666666668,1988,45.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Targeted NE Delta geochemistry reported; individual-core coverage unresolved,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley (1988b); Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.5 km W ruins Kom Niqueza,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 36,S37,Other/control,31.37,31.279999999999998,1988,21.34,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,3.3 km SE Kabira Gazireyet El Darfil,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 37,S38,Burullus,31.421666666666667,31.173333333333336,1988,27.43,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In Ez. El Baralsa,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 38,S39,Burullus,31.42,31.073333333333334,1988,18.29,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.75 km SE Kom El Masura,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 39,S40,Burullus,31.513333333333332,31.141666666666666,1988,28.19,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.7 km NNE Hammad Mahattet El Kasha,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 40,S41,Burullus,31.575,31.205,1988,51.82,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In Hammad Mahattet El Kasha,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 41,S42,Burullus,31.598333333333333,31.096666666666664,1988,45.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.7 km E Baltim Resort Center,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 42,S43,Burullus,31.586666666666666,30.97833333333333,1988,42.67,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In El Burg,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 43,S44,Burullus,31.436666666666667,30.991666666666667,1988,21.34,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.8 km SE Geziret El Isbiryas,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 44,S45,Burullus,31.508333333333333,31.031666666666666,1988,30.48,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In Rsa El Bar,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 45,S46,Burullus,31.4,30.981666666666666,1988,45.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,3.0,8.0,6620.0,3 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 8.0 m; youngest successful reported age 6620 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,"Stanley, Warne et al. (1992); Arbouille & Stanley (1991)","1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,3.5 km NNE Kom El Nashwein,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 46,S47,Burullus,31.540000000000003,30.836666666666666,1989,42.67,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,3.0,5.5,4270.0,3 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 5.5 m; youngest successful reported age 4270 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In Arab El Hanafi,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 47,S48,Burullus,31.503333333333334,30.775,1989,43.28,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,4.0,3.0,1610.0,4 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 3.0 m; youngest successful reported age 1610 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,4.5 km SW Kiman El Saiyar,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 48,S49,Burullus,31.474999999999998,30.685,1989,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,3.0,6.0,3190.0,3 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 6.0 m; youngest successful reported age 3190 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1 km SW Kom Mastaroh,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 49,S50,Burullus,31.435,30.581666666666667,1989,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,4.0,4.5,2870.0,4 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 4.5 m; youngest successful reported age 2870 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,3.5 km SSW Kom Mishtil,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 50,S51,Burullus,31.37,30.495,1989,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,3.0,5.5,3800.0,3 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 5.5 m; youngest successful reported age 3800 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.4 km S Ez. El Sakara,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 51,S52,Burullus,31.406666666666666,30.77,1989,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,5.0,2.0,1670.0,5 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 2.0 m; youngest successful reported age 1670 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,2 km NE Ras El Husan,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 52,S53,Burullus,31.395,30.67666666666667,1989,27.43,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,3.0,4.0,2470.0,3 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 4.0 m; youngest successful reported age 2470 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.4 km SW Atlet El Baqar,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 53,S54,Burullus,31.326666666666668,30.791666666666668,1989,19.51,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,4.0,5.0,3080.0,4 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 5.0 m; youngest successful reported age 3080 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.4 km N El Haddadi,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 54,S55,Burullus,31.315,30.671666666666667,1989,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,4.0,3.5,2420.0,4 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 3.5 m; youngest successful reported age 2420 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In Ez. El Saiyid Mansur,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 55,S56,Burullus,31.325,30.523333333333333,1989,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,1.0,8.5,1490.0,1 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 8.5 m; youngest successful reported age 1490 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1 km SW Minyet El Murshid,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 56,S57,Burullus,31.373333333333335,30.595,1989,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,3.0,6.0,3630.0,3 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 6.0 m; youngest successful reported age 3630 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,Fish market 1 km SE Gazayir El Minsirib,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 57,S58,Burullus,31.384999999999998,30.43,1989,22.86,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,4.0,3.0,3020.0,4 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 3.0 m; youngest successful reported age 3020 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.7 km N Giddiya,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 58,S59,Burullus,31.461666666666666,30.441666666666666,1989,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,3.0,11.5,3140.0,3 successful 14C ages transcribed from MEDIBA Table 2; shallowest dated sample 11.5 m; youngest successful reported age 3140 yr BP. Excellent Holocene framework but too coarse for direct 20th-century RoC.,Arbouille & Stanley (1991); Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,3 km NE Abu Khashaba,Burullus regional transect (S38–S59),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata + Table 2 chronology fields directly transcribed from MEDIBA catalogue.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 59,S60,Other/control,31.328333333333333,30.41,1989,30.48,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.4 km SE El Buseili Station,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 60,S61,Other/control,31.226666666666667,30.371666666666666,1989,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,6 km WSW Hamad Dumeih,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 61,S62,Other/control,31.275,30.328333333333333,1989,24.38,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,3.3 km SE Idku,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 62,S63,Other/control,31.35,30.315,1989,22.25,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1.6 km NE El Nawa Fort,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 63,S64,Other/control,31.40833333333333,30.345,1989,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.2 km SW El Farash Fort,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 64,S65,Other/control,31.476666666666667,30.358333333333334,1989,48.62,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,0.0,,,No 14C samples submitted (catalogue explicitly identifies S65 as the exception). Holocene chronostratigraphic context from regional correlations only; unsuitable for direct 100-year RoC.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.6 km SSE Sidi Mansur,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,0,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 65,S66,Other/control,31.26833333333333,30.456666666666667,1990,20.12,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,2.2 km W El Faiza,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 66,S67,Other/control,31.175,30.331666666666667,1990,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1.5 km S Ibr Zaiyat Ez. Kom Aziza,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 67,S68,Other/control,31.275,30.231666666666666,1990,44.2,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1.5 km NNE Gazayir El Tawila,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 68,S69,Other/control,31.193333333333335,30.275,1990,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1 km NNE Barsig Pumping Station,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 69,S70,Other/control,31.18166666666667,30.173333333333336,1990,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.5 km SE Minshat Bulin,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 70,S71,Other/control,31.265,30.173333333333336,1990,44.2,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.5 km SW El Miaddiya Outlet,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 71,S72,Other/control,31.231666666666666,30.133333333333333,1990,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,In Kom Tarfa,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 72,S73,Mariut,31.276666666666667,30.083333333333332,1990,44.2,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.6 km N Ez. Hod #4,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 73,S74,Mariut,31.223333333333333,30.078333333333333,1990,18.29,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992); Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,0.8 km NNE El Akhdar,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 74,S75,Mariut,31.273333333333333,30.046666666666667,1990,24.38,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992); Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,In Ez. Maqnas,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 75,S76,Mariut,31.229999999999997,30.013333333333332,1990,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992); Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,3 km SSE Ez. Farqon,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 76,S77,Mariut,31.18,29.93166666666667,1990,40.54,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992); Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1 km SW Fouad 1 Airport,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 77,S78,Mariut,31.15,30.040000000000003,1990,19.81,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen et al. (1992); Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.5 km NE Kom Lunsan,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 78,S79,Mariut,31.103333333333335,29.948333333333334,1990,42.67,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,"Potentially valuable modern upper section, but Flaux et al. report that Goodfriend & Stanley's ~20th-century interpretation of the upper ~2 m is complicated by abundant reworked shells. Do not treat depth as calendar time without re-dating.",Stanley & Hamza (1992); Warne & Stanley (1993b); Flaux et al. (2012) synthesis of S79 recent section,"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",B,MEDIBA long core — modern upper section candidate,3 km SW Prince Omar Tusan's kiosks,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),Historical-age interpretation + amino-acid racemization evidence of shell reworking,Upper ~2 m proposed as 20th century; interpretation contested by reworking,~19 mm/yr proposed for upper ~2 m (not a secure depositional age model),"B: unusual MEDIBA long core with a potentially 20th-century upper ~2 m, but age attribution is unreliable without modern re-dating.",https://www.sciencedirect.com/science/article/abs/pii/S030544031200249X,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,0,1,4,1,High-priority archive reanalysis: locate upper S79 material and apply modern radionuclide/SCP dating if preserved,"Moderate: recent-section interpretation published, but chronology is explicitly compromised by reworking" 79,S80,Mariut,31.101666666666667,29.853333333333335,1990,45.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.8 km NW Kom El Shuran,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 80,S81,Mariut,31.053333333333335,29.991666666666667,1990,21.34,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,1.8 km NE Prince Omar Tusan's house,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 81,S82,Mariut,31.05,29.873333333333335,1990,30.48,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",C,MEDIBA long core,2 km E Kom Mitauwh,Mariut/Alexandria sector (preliminary; verify against historical lake polygon),14C / lithostratigraphic framework,,,"C: target-lake regional long core with detailed Holocene sedimentology and 14C framework, but standard sampling (~50 cm in homogeneous units) and chronology are too coarse for direct 100-year RoC.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,1,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 82,S83,Other/control,31.05666666666667,29.77,1990,45.72,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,5.5 km NW El Gamiriya,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 83,S84,Other/control,30.993333333333336,29.618333333333332,1990,22.86,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.8 km SSW Manaret fish market,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 84,S85,Other/control,30.923333333333336,29.526666666666667,1990,10.21,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Stanley & Hamza (1992); Warne & Stanley (1993b),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,1.5 km NW Burg El Arab,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 85,S86,Other/control,30.855,30.796666666666667,1990,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen & Stanley (1993),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,3 km Kafr El Zaiyat,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 86,S87,Other/control,30.740000000000002,31.031666666666666,1990,41.15,,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","Not calculated; >2500 standard samples across 87 cores (~30/core overall), not an upper-core mean",Yes — detailed visual log + X-radiography,Yes — sand/silt/clay by sieve/pipette,Yes — sand-fraction point counts; targeted clay/heavy-mineral studies,No uniform quantitative TOC series; organic-rich/peat layers described and used for dating,Sand-fraction carbonate/biogenic components and targeted carbonate studies; no uniform bulk CaCO3 series,Not established at individual-core level in catalogue,Diatom counted as a sand-size compositional component; not a high-resolution diatom assemblage series,Shell/gastropod/pelecypod components in standard counts; targeted molluscan studies on subsets,Ostracod counted in standard sand-fraction composition; targeted studies on subsets,Foraminifera counted in standard sand-fraction composition; targeted studies on subsets,Not established as a uniform individual-core series in catalogue,,,,Per-core 14C data exist in Table 2 but exact count/depth/youngest age are not yet individually transcribed here. Holocene framework; insufficient for decadal–centennial 20th-century RoC without modern dating.,Chen & Stanley (1993),"1996 catalogue documents lab books, X-radiographs and colour slides at NMNH; present-day physical-core/sample availability requires Smithsonian collections verification",D,MEDIBA long core,0.7 km S El Malwani Mosque,Northern Delta control / other lagoon-distributary sector,14C / lithostratigraphic framework,,,"D: useful geomorphic/chronostratigraphic control, but outside the three target-lake sectors in this screening.",https://repository.si.edu/server/api/core/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/content,,Table 1 metadata verified; proxy fields are programme-level unless explicitly stated. 14C row-level details verified only where numeric cells are populated.,Metadata digitised; proxy raw data require publication/archive recovery,0,1,0,4,0,Use as long-term context,High for Table 1 metadata; variable for proxy coverage 87,Man-XX,Manzala,,,1990,0.94,Near-surface; exact first analytical depth varies by analysis,Centimetre-scale for radiochemistry; exact full interval scheme in paper,High-resolution upper 25–32 cm for radionuclide/carbonate chronology; no single mean calculated,Yes — X-radiography; laminated upper section and molluscan debris described,Yes — laser Coulter grain size,Yes — sand-size fraction composition,Not reported as a continuous TOC series in this study,Yes — carbonate-C; upper 32 cm characterized,No,No assemblage series,Molluscan debris described; not primary quantitative RoC series,No dedicated ostracod series,No dedicated foraminiferal series,"Yes — 210Pb/226Ra/228Ra/137Cs/239,240Pu + K; radionuclide geochemistry",,,,"Modern radionuclide chronology (excess 210Pb, 137Cs, Pu); directly relevant but qualified because tracer fluxes are low/anomalous. Estimated accumulation ~1.2 cm/yr.","Benninger, Suayah & Stanley (1998), Environmental Geology 34:183–193",Published core; current physical archive availability not verified,A,Smithsonian Manzala short core,"Central Manzala; ~9 km NE El-Mataria, 1 km NE Lagan Island, ~10 km SW El-Gameel outlet",Direct in-lagoon short core,"210Pb + 137Cs + 239,240Pu",Recent/subrecent; upper ~32 cm directly constrained by fallout radionuclides,~1.2 cm/yr published estimate,A: high-resolution recent/subrecent core with modern radionuclide chronology and multiple quantitative sediment/geochemical variables; propagate chronology uncertainty.,https://repository.si.edu/server/api/core/bitstreams/9f8c9bd0-4b55-434a-9a24-4c6cc1dcc8cc/content,10.1007/s002540050413,Verified from primary paper,Core paper located; numerical tables/figures require digitisation,1,2,2,5,0,"Immediate digitisation candidate; obtain depth-by-depth radionuclide, carbonate and grain-size values",High for methods; moderate for calendar chronology because fallout inventories are low 88,Man-XIV,Manzala,,,1990,1.0,Near-surface; 18 sampled intervals,18 intervals over ~100 cm; exact depths in published tables,Not calculated,Short-core sediment context available through Randazzo et al. suite,Petrologic texture in parent 30-core dataset; 2–6 petrologic samples/core,Sand-fraction composition in parent dataset,Not established as continuous TOC series,Biogenic carbonate shells analyzed isotopically,No,"Diatom as petrologic component in parent suite, not assemblage series",Yes — molluscan taxa identified; shells used for isotope analyses,Core-specific quantitative ostracod series not established,Core-specific quantitative foram series not established,Yes — 87Sr/86Sr plus stable O and C isotopes on biogenic carbonates,,,,No independent modern radionuclide age model reported for this core in the isotope study; useful subrecent gradient record but not yet a dated 100-year trajectory.,"Reinhardt, Stanley & Schwarcz (2001); parent suite: Randazzo et al. (1998)",Published short core; current physical archive availability not verified,B,Smithsonian Manzala short core,Near mouths of several large drains; freshwater end-member of Manzala,Direct in-lagoon short core,Biogenic carbonate Sr-O-C isotope stratigraphy; no independent fallout age model in this paper,Subrecent short-core sequence; calendar age unresolved,,"B: high-resolution quantitative short-core proxy record, but lacks independent modern age model; digitise sample depths/data and re-date/tie chronology.",https://repository.si.edu/server/api/core/bitstreams/bb903c5a-8de2-46ad-aaed-edafd7f23f76/content,10.1029/2000GC000172,Verified from primary paper,Primary isotope paper located; core interval data published,1,0,2,4,0,Digitise isotope/mollusc data; seek paired depth chronology or archived material for 210Pb/137Cs,"High for proxy data, low–moderate for calendar chronology" 89,Man-XXV,Manzala,,,1990,0.51,Near-surface; 18 sampled intervals,18 intervals over 51 cm; exact depths in published tables,Not calculated,Short-core sediment context available through Randazzo et al. suite,Petrologic texture in parent 30-core dataset; 2–6 petrologic samples/core,Sand-fraction composition in parent dataset,Not established as continuous TOC series,Biogenic carbonate shells analyzed isotopically,No,"Diatom as petrologic component in parent suite, not assemblage series",Yes — molluscan taxa identified; shells used for isotope analyses,Core-specific quantitative ostracod series not established,Core-specific quantitative foram series not established,Yes — 87Sr/86Sr plus stable O and C isotopes on biogenic carbonates,,,,No independent modern radionuclide age model reported for this core in the isotope study; useful subrecent gradient record but not yet a dated 100-year trajectory.,"Reinhardt, Stanley & Schwarcz (2001); parent suite: Randazzo et al. (1998)",Published short core; current physical archive availability not verified,B,Smithsonian Manzala short core,Near El-Gamil outlet; marine end-member of Manzala,Direct in-lagoon short core,Biogenic carbonate Sr-O-C isotope stratigraphy; no independent fallout age model in this paper,Subrecent short-core sequence; calendar age unresolved,,"B: high-resolution quantitative short-core proxy record, but lacks independent modern age model; digitise sample depths/data and re-date/tie chronology.",https://repository.si.edu/server/api/core/bitstreams/bb903c5a-8de2-46ad-aaed-edafd7f23f76/content,10.1029/2000GC000172,Verified from primary paper,Primary isotope paper located; core interval data published,1,0,2,4,0,Digitise isotope/mollusc data; seek paired depth chronology or archived material for 210Pb/137Cs,"High for proxy data, low–moderate for calendar chronology" 90,MANZ1,Manzala,,,1997,,0,1–2 cm sections,~1–2 cm,Yes — master/core stratigraphy and dry bulk density,Physical sediment properties; detailed sedimentology in CASSARINA sequence,Magnetic susceptibility / minerogenic signal; not a full mineralogical series,Yes — LOI/organic content; marked increase in organic-rich low-density sediment after ~1960,Yes — LOI carbonate component,No on MANZ1; parallel MANZ3 supplies pollen/event chronology,Yes — stratigraphic diatom analysis; preservation mainly in the recent upper part,Yes — macrofossil freshwater/brackish shifts used chronostratigraphically,Faunal remains studied in CASSARINA; verify exact MANZ1 count table before RoC,Faunal remains studied where marine-connected; verify exact MANZ1 count table,"210Pb, 226Ra, 137Cs, 241Am; SCP combustion particles; magnetic susceptibility; LOI",,,,"Credible composite 20th-century chronology: 210Pb/137Cs constrained after ~1960 and tied to pollen, macrofossil and SCP event stratigraphy earlier in the century. Egyptian fallout is weak, so uncertainty must be propagated.",Appleby et al. (2001); Flower et al. (2001); Birks et al. (2001); Peglar et al. (2001),CASSARINA/UCL research archive; current physical core/data availability should be requested,A,CASSARINA master short core,Central/south-western open-water Manzala sector; MANZ3 adjacent,Direct in-lagoon core,210Pb + 137Cs + 241Am + pollen + macrofossils + SCP,~20th century to 1997,Pre-1960 ~0.51 cm/yr; post-1960 ~0.20 cm/yr,A: centimetre-scale multi-proxy core with a published composite chronology spanning most of the 20th century.,https://link.springer.com/article/10.1023/A%3A1011938522939,10.1023/A:1011938522939,"Core identity, 1–2 cm sectioning, radiometric limitations, 20th-century composite chronology and sedimentation-rate shift verified from CASSARINA publications.",Publication series located; depth-wise data should be digitised and UCL archive queried,1,2,2,7,0,Top priority: recover/digitise MANZ1 multi-proxy series and chronology table,High 91,MANZ3,Manzala,,,1997,,0,High-resolution stratigraphic sampling; exact pollen interval to digitise,High-resolution; exact mean pending table recovery,Parallel core to MANZ1,Not primary published series for MANZ3,Not primary,Not primary,Not primary,"Yes — terrestrial pollen; Casuarina onset ~25 cm, Olea increase above ~15 cm",Not primary; MANZ1 is principal diatom/radiometric core,Macrofossil chronology paired across adjacent cores,Not primary,Not primary,No primary metal series; chronology transferred/correlated with MANZ1 event stratigraphy,,,,High-resolution pollen record with age control derived by correlation to adjacent MANZ1 composite chronology and historical vegetation markers; not independently radiometrically dated.,Peglar et al. (2001); Appleby et al. (2001),CASSARINA/UCL research archive; availability requires inquiry,B,CASSARINA parallel pollen core,Adjacent to MANZ1,Direct in-lagoon parallel core,Pollen event stratigraphy correlated to MANZ1,~20th century to 1997,Uses MANZ1 paired chronology,"B: excellent quantitative pollen record, but calendar ages are transferred/event-based rather than independently dated.",https://link.springer.com/article/10.1023/A%3A1011938522939,10.1023/A:1011988127627,Core relationship and key pollen markers verified from CASSARINA chronology paper.,Pollen publication located; recover depth-by-taxon matrix if available,1,1,2,2,0,Recover pollen matrix and align to MANZ1 age-depth model with uncertainty,High 92,BURL1,Burullus,,,1997,,0,1–2 cm sections,~1–2 cm,Yes — central/open-water master core,Physical sediment properties,Magnetic susceptibility / sediment properties,LOI/organic content,LOI carbonate component,Not primary; marginal BURL2/BULR2 carries key pollen record,Yes — principal Burullus diatom core in CASSARINA,Faunal remains studied,Faunal remains studied,Faunal remains studied,210Pb/226Ra/137Cs tested; fallout record very poor; SCP record available,,,,"Poor independent fallout-radionuclide chronology. Only the upper ~9 cm is confidently treated as recent in ecosystem synthesis; use stratigraphically, not as a standalone calendar series.",Appleby et al. (2001); Flower et al. (2001); Birks & Birks (2001),CASSARINA/UCL research archive; availability requires inquiry,B,CASSARINA master short core,"Open-water Burullus, distant from shore",Direct in-lagoon core,Weak fallout radionuclides + SCP/contextual cross-core comparison,Recent upper section; full calendar span unresolved,Not securely modelled,B: high-resolution biological/sediment sequence but inadequate independent chronology.,https://link.springer.com/article/10.1023/A%3A1011938522939,10.1023/A:1011938522939,Poor fallout record and recent upper ~9 cm documented in CASSARINA publications.,Publications located; recover diatom/faunal matrices and cross-core correlations,1,0,2,5,1,Recover BURL1 raw diatom/fauna data; consider cross-correlation to BULR2,High 93,BULR2,Burullus,,,1997,,0,1–2 cm sections,~1–2 cm,Yes — marginal/sheltered Burullus core,Physical sediment properties,Sediment properties; not full mineralogical series,LOI / dry bulk density; top ~7 cm much lower density,LOI carbonate component,Yes — Olea/Phoenix rise ~20 cm; Casuarina ~13 cm,Not the principal Burullus diatom core; BURL1 carries main diatom profile,"Yes — freshwater/brackish macrofossil changes at ~24, 16 and 7 cm",Faunal remains studied in CASSARINA suite,Faunal remains studied in CASSARINA suite,137Cs + 210Pb/226Ra screening; SCP; LOI/dry bulk density,,,,Credible composite 20th-century chronology despite weak fallout: 137Cs constrains ~1963 at 6–8 cm; pollen and macrofossil event markers extend chronology to ~1920.,Appleby et al. (2001); Birks et al. (2001); Peglar et al. (2001),CASSARINA/UCL research archive; availability requires inquiry,A,CASSARINA marginal short core,Sheltered/marginal bay near north shore,Direct in-lagoon marginal core,137Cs + pollen + macrofossils + SCP,~1920–1997,Pre-1960 ~0.39 cm/yr; post-1960 ~0.21 cm/yr,"A: high-resolution, multi-proxy Burullus record with a credible composite chronology covering most of the 20th century.",https://link.springer.com/article/10.1023/A%3A1011938522939,10.1023/A:1011938522939,Chronostratigraphic markers and pre/post-1960 rates verified from CASSARINA chronology paper.,Publication series located; recover full depth-by-proxy tables,1,2,2,6,0,Top priority: digitise BULR2 pollen/macrofauna/physical proxies and chronology,High 94,MANZ4,Manzala,,,2003,,0,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,High-resolution; digitise from paper tables,Yes,Yes / bulk sediment physical properties,Clastic fraction / magnetic and bulk properties,Yes — LOI organic matter,Yes — LOI carbonate,No primary pollen series,Siliceous microfossils examined; preservation generally poor,Shell debris quantified/described,Not primary,Not primary,210Pb + 137Cs; SCP/bulk sediment; trace-metal accumulation emphasized mainly at other MELMARINA sites,,,,Fallout record weak/negligible; useful paired physical core,"Flower et al. (2009), MELMARINA",MELMARINA/UCL archive; current data/core availability requires inquiry,B,MELMARINA short core,Lake Manzala; four-core 2003 spatial set,Direct in-lagoon core,210Pb/137Cs + sediment stratigraphy,20th century–2003 where chronology is successful,Spatially variable; MANZ5 documents recent acceleration after early 1980s,"B: short quantitative core valuable for spatial replication, but modern chronology is weaker than MANZ5.",https://link.springer.com/article/10.1007/s10750-008-9677-5,10.1007/s10750-008-9677-5,"Core IDs, four-core Manzala design, radionuclide dating strategy and bulk sediment analyses verified from MELMARINA paper.",Paper located; digitise core tables/figures and seek UCL project files,1,0,2,4,0,Digitise paired physical core; align cautiously to MANZ5,Moderate–high 95,MANZ5,Manzala,,,2003,,0,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,High-resolution; digitise from paper tables,Yes,Yes / bulk sediment physical properties,Clastic fraction / magnetic and bulk properties,Yes — LOI organic matter,Yes — LOI carbonate,No primary pollen series,Siliceous microfossils examined; preservation generally poor,Shell debris quantified/described,Not primary,Not primary,210Pb + 137Cs; SCP/bulk sediment; trace-metal accumulation emphasized mainly at other MELMARINA sites,,,,Best MELMARINA Manzala radionuclide core; 137Cs peak and corrected 210Pb chronology,"Flower et al. (2009), MELMARINA",MELMARINA/UCL archive; current data/core availability requires inquiry,A,MELMARINA short core,Lake Manzala; four-core 2003 spatial set,Direct in-lagoon core,210Pb/137Cs + sediment stratigraphy,20th century–2003 where chronology is successful,Spatially variable; MANZ5 documents recent acceleration after early 1980s,A: best-dated MELMARINA Manzala core with quantitative bulk proxies.,https://link.springer.com/article/10.1007/s10750-008-9677-5,10.1007/s10750-008-9677-5,"Core IDs, four-core Manzala design, radionuclide dating strategy and bulk sediment analyses verified from MELMARINA paper.",Paper located; digitise core tables/figures and seek UCL project files,1,2,2,4,0,Immediate digitisation of chronology + LOI/bulk series,High 96,MANZ7,Manzala,,,2003,,0,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,High-resolution; digitise from paper tables,Yes,Yes / bulk sediment physical properties,Clastic fraction / magnetic and bulk properties,Yes — LOI organic matter,Yes — LOI carbonate,No primary pollen series,Siliceous microfossils examined; preservation generally poor,Shell debris quantified/described,Not primary,Not primary,210Pb + 137Cs; SCP/bulk sediment; trace-metal accumulation emphasized mainly at other MELMARINA sites,,,,Fallout record weaker than MANZ5; paired spatial core,"Flower et al. (2009), MELMARINA",MELMARINA/UCL archive; current data/core availability requires inquiry,B,MELMARINA short core,Lake Manzala; four-core 2003 spatial set,Direct in-lagoon core,210Pb/137Cs + sediment stratigraphy,20th century–2003 where chronology is successful,Spatially variable; MANZ5 documents recent acceleration after early 1980s,"B: short quantitative core valuable for spatial replication, but modern chronology is weaker than MANZ5.",https://link.springer.com/article/10.1007/s10750-008-9677-5,10.1007/s10750-008-9677-5,"Core IDs, four-core Manzala design, radionuclide dating strategy and bulk sediment analyses verified from MELMARINA paper.",Paper located; digitise core tables/figures and seek UCL project files,1,1,2,4,0,Digitise paired physical core; align cautiously to MANZ5,Moderate–high 97,MANZ10,Manzala,,,2003,,0,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,High-resolution; digitise from paper tables,Yes,Yes / bulk sediment physical properties,Clastic fraction / magnetic and bulk properties,Yes — LOI organic matter,Yes — LOI carbonate,No primary pollen series,Siliceous microfossils examined; preservation generally poor,Shell debris quantified/described,Not primary,Not primary,210Pb + 137Cs; SCP/bulk sediment; trace-metal accumulation emphasized mainly at other MELMARINA sites,,,,Fallout record weak/negligible; useful paired physical core,"Flower et al. (2009), MELMARINA",MELMARINA/UCL archive; current data/core availability requires inquiry,B,MELMARINA short core,Lake Manzala; four-core 2003 spatial set,Direct in-lagoon core,210Pb/137Cs + sediment stratigraphy,20th century–2003 where chronology is successful,Spatially variable; MANZ5 documents recent acceleration after early 1980s,"B: short quantitative core valuable for spatial replication, but modern chronology is weaker than MANZ5.",https://link.springer.com/article/10.1007/s10750-008-9677-5,10.1007/s10750-008-9677-5,"Core IDs, four-core Manzala design, radionuclide dating strategy and bulk sediment analyses verified from MELMARINA paper.",Paper located; digitise core tables/figures and seek UCL project files,1,0,2,4,0,Digitise paired physical core; align cautiously to MANZ5,Moderate–high 98,B-1,Burullus,,,2006,0.55,0,5 cm for radionuclide samples,~5 cm,Yes — vibrocore sediment sections,Yes — laser particle size,Not a dedicated mineralogical series,Yes — total organic matter (TOM),Not primary,No,No,Shell fragments described,No,No,210Pb + 137Cs; same/core-related dataset later used for heavy-metal profiles,,,,Detectable 210Pb/137Cs in upper ~17.5 cm; published post-dam rate ~0.42–0.56 cm/yr. Low fallout and probable sediment reworking/seawater-seepage effects limit calendar precision.,Xu et al. (2008); Chen et al. (2010),Published core profiles; physical archive not verified,B,Burullus vibrocore,Burullus lagoon transect from drainage-influenced sector toward sea coast,Direct in-lagoon core,210Pb/137Cs screening; CIC estimate only robust for B-1 upper section,Upper ~15–18 cm interpreted as post-Aswan High Dam,~0.42–0.56 cm/yr for B-1 upper section,"B: useful centimetric sediment/organic/grain-size/geochemical profile, but fallout chronology is weak and irregular.",https://link.springer.com/article/10.1007/s11707-008-0059-0,10.1007/s11707-008-0059-0,"Core lengths, 5-cm radionuclide spacing, grain size, TOM and low-fallout chronology directly reported.",Core profiles published; digitisation feasible,1,1,2,4,1,Digitise down-core grain size/TOM/radionuclides/metals; do not overinterpret calendar ages,High for measurements; low–moderate for chronology 99,B-2,Burullus,,,2006,0.75,0,5 cm for radionuclide samples,~5 cm,Yes — vibrocore sediment sections,Yes — laser particle size,Not a dedicated mineralogical series,Yes — total organic matter (TOM),Not primary,No,No,Shell fragments described,No,No,210Pb + 137Cs; same/core-related dataset later used for heavy-metal profiles,,,,Very weak/irregular fallout; uppermost ~5 cm detectable. Low fallout and probable sediment reworking/seawater-seepage effects limit calendar precision.,Xu et al. (2008); Chen et al. (2010),Published core profiles; physical archive not verified,B,Burullus vibrocore,Burullus lagoon transect from drainage-influenced sector toward sea coast,Direct in-lagoon core,210Pb/137Cs screening; CIC estimate only robust for B-1 upper section,Upper ~15–18 cm interpreted as post-Aswan High Dam,Not securely measurable,"B: useful centimetric sediment/organic/grain-size/geochemical profile, but fallout chronology is weak and irregular.",https://link.springer.com/article/10.1007/s11707-008-0059-0,10.1007/s11707-008-0059-0,"Core lengths, 5-cm radionuclide spacing, grain size, TOM and low-fallout chronology directly reported.",Core profiles published; digitisation feasible,1,0,2,4,1,Digitise down-core grain size/TOM/radionuclides/metals; do not overinterpret calendar ages,High for measurements; low–moderate for chronology 100,B-3,Burullus,,,2006,0.8,0,5 cm for radionuclide samples,~5 cm,Yes — vibrocore sediment sections,Yes — laser particle size,Not a dedicated mineralogical series,Yes — total organic matter (TOM),Not primary,No,No,Shell fragments described,No,No,210Pb + 137Cs; same/core-related dataset later used for heavy-metal profiles,,,,Very weak/irregular fallout; uppermost ~5 cm detectable. Low fallout and probable sediment reworking/seawater-seepage effects limit calendar precision.,Xu et al. (2008); Chen et al. (2010),Published core profiles; physical archive not verified,B,Burullus vibrocore,Burullus lagoon transect from drainage-influenced sector toward sea coast,Direct in-lagoon core,210Pb/137Cs screening; CIC estimate only robust for B-1 upper section,Upper ~15–18 cm interpreted as post-Aswan High Dam,Not securely measurable,"B: useful centimetric sediment/organic/grain-size/geochemical profile, but fallout chronology is weak and irregular.",https://link.springer.com/article/10.1007/s11707-008-0059-0,10.1007/s11707-008-0059-0,"Core lengths, 5-cm radionuclide spacing, grain size, TOM and low-fallout chronology directly reported.",Core profiles published; digitisation feasible,1,0,2,4,1,Digitise down-core grain size/TOM/radionuclides/metals; do not overinterpret calendar ages,High for measurements; low–moderate for chronology 101,M-1,Manzala,,,2007–2008,,0,3 cm for grain-size series,~3 cm (grain size); metal sampling denser/variable,"Yes — texture, structure, colour and biogenic occurrences",Yes — 3 cm intervals,Al used as terrigenous/clay-normalization proxy,TOM considered in sediment interpretation; verify full core series,Not primary,No,No,Shell fragments described,No,No,"Al, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Zn by ICP-OES; 210Pb/137Cs on selected cores (M-1 and B-4 among dated set)",,,,Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,"Gu, Salem & Chen (2013)",Published core dataset; physical archive not verified,B,Short geochemical core,Manzala spatial pollution transect,Direct in-lagoon core,210Pb/137Cs constraints,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,Not resolved as a detailed time-varying series in this study,"B: strong 3-cm grain-size + nine-element geochemical sequence, but chronology is only broadly constrained.",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,10.1016/j.ecss.2012.06.012,"Core IDs, 25–50 cm overall length range, 3-cm grain-size sampling, nine metals and radiometric post-dam constraint verified.",Article figures/tables should be digitised; raw data availability unknown,1,1,2,3,1,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,High for analytical design; moderate for temporal alignment 102,M-2,Manzala,,,2007–2008,,0,3 cm for grain-size series,~3 cm (grain size); metal sampling denser/variable,"Yes — texture, structure, colour and biogenic occurrences",Yes — 3 cm intervals,Al used as terrigenous/clay-normalization proxy,TOM considered in sediment interpretation; verify full core series,Not primary,No,No,Shell fragments described,No,No,"Al, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Zn by ICP-OES; 210Pb/137Cs on selected cores (M-1 and B-4 among dated set)",,,,Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,"Gu, Salem & Chen (2013)",Published core dataset; physical archive not verified,B,Short geochemical core,Manzala spatial pollution transect,Direct in-lagoon core,Cross-core stratigraphic/radiometric context,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,Not resolved as a detailed time-varying series in this study,"B: strong 3-cm grain-size + nine-element geochemical sequence, but chronology is only broadly constrained.",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,10.1016/j.ecss.2012.06.012,"Core IDs, 25–50 cm overall length range, 3-cm grain-size sampling, nine metals and radiometric post-dam constraint verified.",Article figures/tables should be digitised; raw data availability unknown,1,0,2,3,1,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,High for analytical design; moderate for temporal alignment 103,M-3,Manzala,,,2007–2008,,0,3 cm for grain-size series,~3 cm (grain size); metal sampling denser/variable,"Yes — texture, structure, colour and biogenic occurrences",Yes — 3 cm intervals,Al used as terrigenous/clay-normalization proxy,TOM considered in sediment interpretation; verify full core series,Not primary,No,No,Shell fragments described,No,No,"Al, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Zn by ICP-OES; 210Pb/137Cs on selected cores (M-1 and B-4 among dated set)",,,,Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,"Gu, Salem & Chen (2013)",Published core dataset; physical archive not verified,B,Short geochemical core,Manzala spatial pollution transect,Direct in-lagoon core,Cross-core stratigraphic/radiometric context,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,Not resolved as a detailed time-varying series in this study,"B: strong 3-cm grain-size + nine-element geochemical sequence, but chronology is only broadly constrained.",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,10.1016/j.ecss.2012.06.012,"Core IDs, 25–50 cm overall length range, 3-cm grain-size sampling, nine metals and radiometric post-dam constraint verified.",Article figures/tables should be digitised; raw data availability unknown,1,0,2,3,1,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,High for analytical design; moderate for temporal alignment 104,B-4,Burullus,,,2007–2008,,0,3 cm for grain-size series,~3 cm (grain size); metal sampling denser/variable,"Yes — texture, structure, colour and biogenic occurrences",Yes — 3 cm intervals,Al used as terrigenous/clay-normalization proxy,TOM considered in sediment interpretation; verify full core series,Not primary,No,No,Shell fragments described,No,No,"Al, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Zn by ICP-OES; 210Pb/137Cs on selected cores (M-1 and B-4 among dated set)",,,,Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,"Gu, Salem & Chen (2013)",Published core dataset; physical archive not verified,B,Short geochemical core,Burullus short-core station,Direct in-lagoon core,210Pb/137Cs constraints,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,Not resolved as a detailed time-varying series in this study,"B: strong 3-cm grain-size + nine-element geochemical sequence, but chronology is only broadly constrained.",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,10.1016/j.ecss.2012.06.012,"Core IDs, 25–50 cm overall length range, 3-cm grain-size sampling, nine metals and radiometric post-dam constraint verified.",Article figures/tables should be digitised; raw data availability unknown,1,1,2,3,1,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,High for analytical design; moderate for temporal alignment 105,C-1,Burullus,31.4162998,30.7656002,2018,0.56,0,4 cm slices,4 cm,Yes — sediment core stratigraphy,Not the principal published variable,No multielement NAA series reported for C-1,Not the principal published series,Not primary,No,No,No,No,No,210Pb/137Cs chronology; no NAA heavy-metal profile used,,,,High-resolution modern radio-dating with 210Pb models and 137Cs marker interpretation; 4-cm slices. Event attribution of specific 137Cs peaks should be sensitivity-tested rather than treated as exact.,Ghanem et al. (2024),Open-access published data; physical cores not verified,C,Modern radio-dated Burullus core,Burullus 2018 four-core network,Direct in-lagoon core,210Pb CRS/CFCS + 137Cs,Approximately mid-20th century–2018 in dated sections,Mean linear sedimentation rate ~0.81 cm/yr,"B: excellent 4-cm chronology, but proxy breadth is limited relative to C-2–C-4.",https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,10.1007/s11356-024-33761-5,"Coordinates, lengths, 4-cm slicing and core-specific mean sedimentation rates reported in open-access primary paper.",Open-access article; tables can be directly digitised,1,2,2,1,0,Use as chronology/spatial sedimentation control,High 106,C-2,Burullus,31.4762993,30.8225002,2018,0.56,0,4 cm slices,4 cm,Yes — sediment core stratigraphy,Not the principal published variable,Elemental composition via NAA for C-2–C-4,Not the principal published series,Not primary,No,No,No,No,No,Yes — multi-element NAA + 210Pb/137Cs radio-dating,,,,High-resolution modern radio-dating with 210Pb models and 137Cs marker interpretation; 4-cm slices. Event attribution of specific 137Cs peaks should be sensitivity-tested rather than treated as exact.,Ghanem et al. (2024),Open-access published data; physical cores not verified,A,Modern radio-dated Burullus core,Burullus 2018 four-core network,Direct in-lagoon core,210Pb CRS/CFCS + 137Cs,Approximately mid-20th century–2018 in dated sections,Mean linear sedimentation rate ~0.96 cm/yr,A: 4-cm modern chronology plus quantitative multielement geochemistry.,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,10.1007/s11356-024-33761-5,"Coordinates, lengths, 4-cm slicing and core-specific mean sedimentation rates reported in open-access primary paper.",Open-access article; tables can be directly digitised,1,2,2,4,0,Immediate extraction of age-depth + elemental profiles,High 107,C-3,Burullus,31.5697002,30.9789009,2018,0.48,0,4 cm slices,4 cm,Yes — sediment core stratigraphy,Not the principal published variable,Elemental composition via NAA for C-2–C-4,Not the principal published series,Not primary,No,No,No,No,No,Yes — multi-element NAA + 210Pb/137Cs radio-dating,,,,High-resolution modern radio-dating with 210Pb models and 137Cs marker interpretation; 4-cm slices. Event attribution of specific 137Cs peaks should be sensitivity-tested rather than treated as exact.,Ghanem et al. (2024),Open-access published data; physical cores not verified,A,Modern radio-dated Burullus core,Burullus 2018 four-core network,Direct in-lagoon core,210Pb CRS/CFCS + 137Cs,Approximately mid-20th century–2018 in dated sections,Mean linear sedimentation rate ~0.70 cm/yr,A: 4-cm modern chronology plus quantitative multielement geochemistry.,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,10.1007/s11356-024-33761-5,"Coordinates, lengths, 4-cm slicing and core-specific mean sedimentation rates reported in open-access primary paper.",Open-access article; tables can be directly digitised,1,2,2,4,0,Immediate extraction of age-depth + elemental profiles,High 108,C-4,Burullus,31.4039001,30.5893002,2018,0.48,0,4 cm slices,4 cm,Yes — sediment core stratigraphy,Not the principal published variable,Elemental composition via NAA for C-2–C-4,Not the principal published series,Not primary,No,No,No,No,No,Yes — multi-element NAA + 210Pb/137Cs radio-dating,,,,High-resolution modern radio-dating with 210Pb models and 137Cs marker interpretation; 4-cm slices. Event attribution of specific 137Cs peaks should be sensitivity-tested rather than treated as exact.,Ghanem et al. (2024),Open-access published data; physical cores not verified,A,Modern radio-dated Burullus core,Burullus 2018 four-core network,Direct in-lagoon core,210Pb CRS/CFCS + 137Cs,Approximately mid-20th century–2018 in dated sections,Mean linear sedimentation rate ~0.75 cm/yr,A: 4-cm modern chronology plus quantitative multielement geochemistry.,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,10.1007/s11356-024-33761-5,"Coordinates, lengths, 4-cm slicing and core-specific mean sedimentation rates reported in open-access primary paper.",Open-access article; tables can be directly digitised,1,2,2,4,0,Immediate extraction of age-depth + elemental profiles,High index,Core_ID,lake,RoC_utility,record_type,modern_time_span,chronological_method,resolution,key_assets,main_limitation,priority_action,published_study,source_url,confidence 0,MANZ1,Manzala,A,CASSARINA master short core,~20th century to 1997,210Pb + 137Cs + 241Am + pollen + macrofossils + SCP,1–2 cm sections,"diatoms, grain size, organic/LOI, geochem/radionuclides, molluscs","Credible composite 20th-century chronology: 210Pb/137Cs constrained after ~1960 and tied to pollen, macrofossil and SCP event stratigraphy earlier in the century. Egyptian fallout is weak, so uncertainty must be propagated.",Top priority: recover/digitise MANZ1 multi-proxy series and chronology table,Appleby et al. (2001); Flower et al. (2001); Birks et al. (2001); Peglar et al. (2001),https://link.springer.com/article/10.1023/A%3A1011938522939,High 1,MANZ5,Manzala,A,MELMARINA short core,20th century–2003 where chronology is successful,210Pb/137Cs + sediment stratigraphy,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,"diatoms, grain size, organic/LOI, geochem/radionuclides, molluscs",Best MELMARINA Manzala radionuclide core; 137Cs peak and corrected 210Pb chronology,Immediate digitisation of chronology + LOI/bulk series,"Flower et al. (2009), MELMARINA",https://link.springer.com/article/10.1007/s10750-008-9677-5,High 2,Man-XX,Manzala,A,Smithsonian Manzala short core,Recent/subrecent; upper ~32 cm directly constrained by fallout radionuclides,"210Pb + 137Cs + 239,240Pu",Centimetre-scale for radiochemistry; exact full interval scheme in paper,"grain size, geochem/radionuclides, molluscs","Modern radionuclide chronology (excess 210Pb, 137Cs, Pu); directly relevant but qualified because tracer fluxes are low/anomalous. Estimated accumulation ~1.2 cm/yr.","Immediate digitisation candidate; obtain depth-by-depth radionuclide, carbonate and grain-size values","Benninger, Suayah & Stanley (1998), Environmental Geology 34:183–193",https://repository.si.edu/server/api/core/bitstreams/9f8c9bd0-4b55-434a-9a24-4c6cc1dcc8cc/content,High for methods; moderate for calendar chronology because fallout inventories are low 3,BULR2,Burullus,A,CASSARINA marginal short core,~1920–1997,137Cs + pollen + macrofossils + SCP,1–2 cm sections,"pollen, grain size, organic/LOI, geochem/radionuclides, molluscs",Credible composite 20th-century chronology despite weak fallout: 137Cs constrains ~1963 at 6–8 cm; pollen and macrofossil event markers extend chronology to ~1920.,Top priority: digitise BULR2 pollen/macrofauna/physical proxies and chronology,Appleby et al. (2001); Birks et al. (2001); Peglar et al. (2001),https://link.springer.com/article/10.1023/A%3A1011938522939,High 4,C-2,Burullus,A,Modern radio-dated Burullus core,Approximately mid-20th century–2018 in dated sections,210Pb CRS/CFCS + 137Cs,4 cm slices,geochem/radionuclides,High-resolution modern radio-dating with 210Pb models and 137Cs marker interpretation; 4-cm slices. Event attribution of specific 137Cs peaks should be sensitivity-tested rather than treated as exact.,Immediate extraction of age-depth + elemental profiles,Ghanem et al. (2024),https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,High 5,C-3,Burullus,A,Modern radio-dated Burullus core,Approximately mid-20th century–2018 in dated sections,210Pb CRS/CFCS + 137Cs,4 cm slices,geochem/radionuclides,High-resolution modern radio-dating with 210Pb models and 137Cs marker interpretation; 4-cm slices. Event attribution of specific 137Cs peaks should be sensitivity-tested rather than treated as exact.,Immediate extraction of age-depth + elemental profiles,Ghanem et al. (2024),https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,High 6,C-4,Burullus,A,Modern radio-dated Burullus core,Approximately mid-20th century–2018 in dated sections,210Pb CRS/CFCS + 137Cs,4 cm slices,geochem/radionuclides,High-resolution modern radio-dating with 210Pb models and 137Cs marker interpretation; 4-cm slices. Event attribution of specific 137Cs peaks should be sensitivity-tested rather than treated as exact.,Immediate extraction of age-depth + elemental profiles,Ghanem et al. (2024),https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,High 7,M-1,Manzala,B,Short geochemical core,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,210Pb/137Cs constraints,3 cm for grain-size series,"grain size, organic/LOI, geochem/radionuclides, molluscs",Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,"Gu, Salem & Chen (2013)",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,High for analytical design; moderate for temporal alignment 8,M-2,Manzala,B,Short geochemical core,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,Cross-core stratigraphic/radiometric context,3 cm for grain-size series,"grain size, organic/LOI, geochem/radionuclides, molluscs",Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,"Gu, Salem & Chen (2013)",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,High for analytical design; moderate for temporal alignment 9,M-3,Manzala,B,Short geochemical core,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,Cross-core stratigraphic/radiometric context,3 cm for grain-size series,"grain size, organic/LOI, geochem/radionuclides, molluscs",Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,"Gu, Salem & Chen (2013)",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,High for analytical design; moderate for temporal alignment 10,MANZ10,Manzala,B,MELMARINA short core,20th century–2003 where chronology is successful,210Pb/137Cs + sediment stratigraphy,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,"diatoms, grain size, organic/LOI, geochem/radionuclides, molluscs",Fallout record weak/negligible; useful paired physical core,Digitise paired physical core; align cautiously to MANZ5,"Flower et al. (2009), MELMARINA",https://link.springer.com/article/10.1007/s10750-008-9677-5,Moderate–high 11,MANZ3,Manzala,B,CASSARINA parallel pollen core,~20th century to 1997,Pollen event stratigraphy correlated to MANZ1,High-resolution stratigraphic sampling; exact pollen interval to digitise,"pollen, molluscs",High-resolution pollen record with age control derived by correlation to adjacent MANZ1 composite chronology and historical vegetation markers; not independently radiometrically dated.,Recover pollen matrix and align to MANZ1 age-depth model with uncertainty,Peglar et al. (2001); Appleby et al. (2001),https://link.springer.com/article/10.1023/A%3A1011938522939,High 12,MANZ4,Manzala,B,MELMARINA short core,20th century–2003 where chronology is successful,210Pb/137Cs + sediment stratigraphy,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,"diatoms, grain size, organic/LOI, geochem/radionuclides, molluscs",Fallout record weak/negligible; useful paired physical core,Digitise paired physical core; align cautiously to MANZ5,"Flower et al. (2009), MELMARINA",https://link.springer.com/article/10.1007/s10750-008-9677-5,Moderate–high 13,MANZ7,Manzala,B,MELMARINA short core,20th century–2003 where chronology is successful,210Pb/137Cs + sediment stratigraphy,Centimetre-scale/closely spaced bulk sediment sampling; exact interval varies by analysis,"diatoms, grain size, organic/LOI, geochem/radionuclides, molluscs",Fallout record weaker than MANZ5; paired spatial core,Digitise paired physical core; align cautiously to MANZ5,"Flower et al. (2009), MELMARINA",https://link.springer.com/article/10.1007/s10750-008-9677-5,Moderate–high 14,Man-XIV,Manzala,B,Smithsonian Manzala short core,Subrecent short-core sequence; calendar age unresolved,Biogenic carbonate Sr-O-C isotope stratigraphy; no independent fallout age model in this paper,18 intervals over ~100 cm; exact depths in published tables,"diatoms, grain size, geochem/radionuclides, molluscs",No independent modern radionuclide age model reported for this core in the isotope study; useful subrecent gradient record but not yet a dated 100-year trajectory.,Digitise isotope/mollusc data; seek paired depth chronology or archived material for 210Pb/137Cs,"Reinhardt, Stanley & Schwarcz (2001); parent suite: Randazzo et al. (1998)",https://repository.si.edu/server/api/core/bitstreams/bb903c5a-8de2-46ad-aaed-edafd7f23f76/content,"High for proxy data, low–moderate for calendar chronology" 15,Man-XXV,Manzala,B,Smithsonian Manzala short core,Subrecent short-core sequence; calendar age unresolved,Biogenic carbonate Sr-O-C isotope stratigraphy; no independent fallout age model in this paper,18 intervals over 51 cm; exact depths in published tables,"diatoms, grain size, geochem/radionuclides, molluscs",No independent modern radionuclide age model reported for this core in the isotope study; useful subrecent gradient record but not yet a dated 100-year trajectory.,Digitise isotope/mollusc data; seek paired depth chronology or archived material for 210Pb/137Cs,"Reinhardt, Stanley & Schwarcz (2001); parent suite: Randazzo et al. (1998)",https://repository.si.edu/server/api/core/bitstreams/bb903c5a-8de2-46ad-aaed-edafd7f23f76/content,"High for proxy data, low–moderate for calendar chronology" 16,B-1,Burullus,B,Burullus vibrocore,Upper ~15–18 cm interpreted as post-Aswan High Dam,210Pb/137Cs screening; CIC estimate only robust for B-1 upper section,5 cm for radionuclide samples,"grain size, organic/LOI, geochem/radionuclides, molluscs",Detectable 210Pb/137Cs in upper ~17.5 cm; published post-dam rate ~0.42–0.56 cm/yr. Low fallout and probable sediment reworking/seawater-seepage effects limit calendar precision.,Digitise down-core grain size/TOM/radionuclides/metals; do not overinterpret calendar ages,Xu et al. (2008); Chen et al. (2010),https://link.springer.com/article/10.1007/s11707-008-0059-0,High for measurements; low–moderate for chronology 17,B-2,Burullus,B,Burullus vibrocore,Upper ~15–18 cm interpreted as post-Aswan High Dam,210Pb/137Cs screening; CIC estimate only robust for B-1 upper section,5 cm for radionuclide samples,"grain size, organic/LOI, geochem/radionuclides, molluscs",Very weak/irregular fallout; uppermost ~5 cm detectable. Low fallout and probable sediment reworking/seawater-seepage effects limit calendar precision.,Digitise down-core grain size/TOM/radionuclides/metals; do not overinterpret calendar ages,Xu et al. (2008); Chen et al. (2010),https://link.springer.com/article/10.1007/s11707-008-0059-0,High for measurements; low–moderate for chronology 18,B-3,Burullus,B,Burullus vibrocore,Upper ~15–18 cm interpreted as post-Aswan High Dam,210Pb/137Cs screening; CIC estimate only robust for B-1 upper section,5 cm for radionuclide samples,"grain size, organic/LOI, geochem/radionuclides, molluscs",Very weak/irregular fallout; uppermost ~5 cm detectable. Low fallout and probable sediment reworking/seawater-seepage effects limit calendar precision.,Digitise down-core grain size/TOM/radionuclides/metals; do not overinterpret calendar ages,Xu et al. (2008); Chen et al. (2010),https://link.springer.com/article/10.1007/s11707-008-0059-0,High for measurements; low–moderate for chronology 19,B-4,Burullus,B,Short geochemical core,Upper ~10–15 cm post-1964; deeper sequence older but poorly dated,210Pb/137Cs constraints,3 cm for grain-size series,"grain size, organic/LOI, geochem/radionuclides, molluscs",Radiometric dating constrains the upper ~10–15 cm as post-Aswan High Dam; not a fully resolved annual/decadal age-depth model.,Digitise metals + grain size; use as replicated spatial RoC only after chronology harmonisation,"Gu, Salem & Chen (2013)",https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,High for analytical design; moderate for temporal alignment 20,BURL1,Burullus,B,CASSARINA master short core,Recent upper section; full calendar span unresolved,Weak fallout radionuclides + SCP/contextual cross-core comparison,1–2 cm sections,"diatoms, grain size, organic/LOI, geochem/radionuclides, molluscs","Poor independent fallout-radionuclide chronology. Only the upper ~9 cm is confidently treated as recent in ecosystem synthesis; use stratigraphically, not as a standalone calendar series.",Recover BURL1 raw diatom/fauna data; consider cross-correlation to BULR2,Appleby et al. (2001); Flower et al. (2001); Birks & Birks (2001),https://link.springer.com/article/10.1023/A%3A1011938522939,High 21,S79,Mariut,B,MEDIBA long core — modern upper section candidate,Upper ~2 m proposed as 20th century; interpretation contested by reworking,Historical-age interpretation + amino-acid racemization evidence of shell reworking,"Variable; at lithologic changes, otherwise nominal minimum ~0.50 m in homogeneous sections","diatoms, grain size, molluscs","Potentially valuable modern upper section, but Flaux et al. report that Goodfriend & Stanley's ~20th-century interpretation of the upper ~2 m is complicated by abundant reworked shells. Do not treat depth as calendar time without re-dating.",High-priority archive reanalysis: locate upper S79 material and apply modern radionuclide/SCP dating if preserved,Stanley & Hamza (1992); Warne & Stanley (1993b); Flaux et al. (2012) synthesis of S79 recent section,https://www.sciencedirect.com/science/article/abs/pii/S030544031200249X,"Moderate: recent-section interpretation published, but chronology is explicitly compromised by reworking" index,Core_ID,lake,depth_top_cm,depth_bottom_cm,calendar_age_or_range,anchor_type,interpretation,uncertainty_note,source_url 0,MANZ1,Manzala,27.0,27.0,1912–1930,Macrofossil/event,Onset of stronger freshwater influence; linked to effective Nile Delta barrages,Decadal event range,https://link.springer.com/article/10.1023/A%3A1011938522939 1,MANZ3,Manzala,25.0,25.0,~1930 or later,Pollen/event,Casuarina onset,"Historical planting marker, approximate",https://link.springer.com/article/10.1023/A%3A1011938522939 2,MANZ3,Manzala,15.0,15.0,~1940 or later,Pollen/event,Olea increase,"Historical land-use marker, approximate",https://link.springer.com/article/10.1023/A%3A1011938522939 3,MANZ1,Manzala,17.0,17.0,1933–1951 / pre-1954,Macrofossil/event,Further freshwater shift; below 137Cs onset,Broad historical attribution,https://link.springer.com/article/10.1023/A%3A1011938522939 4,MANZ1,Manzala,12.0,12.0,~1954,137Cs onset,Onset of weapons-fallout record,Low fallout / mobility uncertainty,https://link.springer.com/article/10.1023/A%3A1011938522939 5,MANZ1,Manzala,7.0,8.0,~1963,210Pb + 137Cs,1963 level,Composite radiometric interpretation,https://link.springer.com/article/10.1023/A%3A1011938522939 6,MANZ1,Manzala,3.0,4.0,~1986,210Pb model,Model places 1986 here; 137Cs subsurface peak may mix sources,Chernobyl/weapons-fallout ambiguity,https://link.springer.com/article/10.1023/A%3A1011938522939 7,BULR2,Burullus,24.0,24.0,~1920,Macrofossil/event,First marked freshwater shift,Approximate,https://link.springer.com/article/10.1023/A%3A1011938522939 8,BULR2,Burullus,20.0,20.0,~1930,Pollen/event,Olea/Phoenix increase,Approximate,https://link.springer.com/article/10.1023/A%3A1011938522939 9,BULR2,Burullus,16.0,16.0,1933–1951,Macrofossil/event,Second freshwater shift,Broad historical attribution,https://link.springer.com/article/10.1023/A%3A1011938522939 10,BULR2,Burullus,6.0,8.0,~1963,137Cs,1963 level inferred from 137Cs inventory,Weak fallout; composite chronology required,https://link.springer.com/article/10.1023/A%3A1011938522939 11,BULR2,Burullus,7.0,7.0,~1964+,Macrofossil/event,"Most recent freshwater shift, linked to High Dam completion",Approximate,https://link.springer.com/article/10.1023/A%3A1011938522939 12,B-1,Burullus,17.5,17.5,post-1963 interpretation,210Pb/137Cs,Upper section used to estimate ~0.42–0.56 cm/yr,Very low fallout; not an exact marker,https://link.springer.com/article/10.1007/s11707-008-0059-0 13,MANZ5,Manzala,11.5,11.5,~1963,137Cs,Well-resolved fallout maximum used in corrected chronology,Digitise exact uncertainty from paper,https://link.springer.com/article/10.1007/s10750-008-9677-5 14,M-1,Manzala,10.0,15.0,post-1964,Radiometric envelope,Upper core interpreted as post-Aswan High Dam,Broad temporal constraint,https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314 15,B-4,Burullus,10.0,15.0,post-1964,Radiometric envelope,Upper core interpreted as post-Aswan High Dam,Broad temporal constraint,https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314 16,C-2,Burullus,4.0,4.0,2016,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 17,C-2,Burullus,12.0,12.0,2011,210Pb/137Cs interpretation,Published age-depth point,Event attribution should be sensitivity-tested,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 18,C-2,Burullus,20.0,20.0,2003,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 19,C-2,Burullus,28.0,28.0,1993,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 20,C-2,Burullus,44.0,44.0,1954,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 21,C-2,Burullus,52.0,52.0,1937,210Pb model,Published age-depth point,Greater uncertainty at depth,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 22,C-3,Burullus,4.0,4.0,2017,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 23,C-3,Burullus,12.0,12.0,2011,210Pb/137Cs interpretation,Published age-depth point,Event attribution should be sensitivity-tested,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 24,C-3,Burullus,20.0,20.0,1998,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 25,C-3,Burullus,28.0,28.0,1983,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 26,C-3,Burullus,36.0,36.0,1951,210Pb model,Published age-depth point,Greater uncertainty at depth,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 27,C-3,Burullus,44.0,44.0,1944,210Pb model,Published age-depth point,Greater uncertainty at depth,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 28,C-4,Burullus,12.0,12.0,2011,210Pb/137Cs interpretation,Published age-depth point,Event attribution should be sensitivity-tested,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 29,C-4,Burullus,20.0,20.0,2004,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 30,C-4,Burullus,28.0,28.0,1995,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 31,C-4,Burullus,36.0,36.0,1963,210Pb model,Published age-depth point,Model-dependent,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ 32,C-4,Burullus,44.0,44.0,1941,210Pb model,Published age-depth point,Greater uncertainty at depth,https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/ index,lake,candidate_archive,verified_content,missing_metadata,next_action,potential_RoC_grade,source_url,status 0,Manzala,Randazzo 1990 short-core suite,"30 short percussion cores, 18–98 cm; 83 surface samples; 117 subsurface samples; lithology/X-ray, grain size, sand composition and molluscs","Individual Man-* IDs, coordinates and depth-by-variable table for all 30 cores",Recover Randazzo thesis/paper tables or Smithsonian field/lab books; add all IDs to Master,B / potentially A if chronology can be tied,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,Verified suite; incomplete core-level transcription 1,Manzala,Zalat & Servant-Vildary 19-core diatom archive,"565 samples from 19 cores across Manzala, Burullus and Edku; 263 diatom taxa; quantitative multivariate palaeoenvironmental data","Core IDs, coordinates, per-core depth resolution and chronology",Recover supplementary/raw diatom matrix and core metadata; evaluate youngest sections for 20th-century coverage,B–C depending chronology,https://link.springer.com/article/10.1007/s10933-006-9029-2,Verified publication; raw matrix unresolved 2,Mariut,Loizeau & Stanley recent/subrecent Mariut sediment work,Smithsonian-era study of changing bottom-sediment lithofacies/pollution in Mariut,"Individual short-core IDs, coordinates, lengths, depth intervals, chronology",Obtain full Journal of Coastal Research article + Smithsonian field records; reconstruct site/core table,Potential B,https://www.jstor.org/stable/4298225,High-priority unresolved archival lead 3,Mariut,S79 upper modern section,"Upper ~2 m proposed as 20th-century deposition (~19 mm/yr), but shells show substantial reworking",Independent modern chronology and archive availability,Locate S79 upper core/sample material; 210Pb/137Cs/SCP re-date if preserved,B if material survives,https://www.sciencedirect.com/science/article/abs/pii/S030544031200249X,Master row added; chronology unresolved 4,Manzala,Abdelhady 2021 unnamed ~120-cm core,~170-year environmental sequence; sediment + molluscan community change and pollution indicators,"Formal core ID/coordinates, exact sampling interval and age model details",Extract full methods/tables from primary paper; add as named/aliased core once location is verified,Potential A/B,https://www.sciencedirect.com/science/article/pii/S1470160X21003198,Verified publication lead 5,Burullus,Shetaia et al. 2022 four-core metal dataset,"Four sediment cores + 12 surface samples; Fe, Mn, Zn, Hg, Cu, Pb, Cd and ecological-risk metrics","Core IDs, lengths, sampling intervals and chronology status",Extract full paper tables and determine whether cores can be temporally calibrated,Potential B,https://www.sciencedirect.com/science/article/abs/pii/S0025326X2200248X,Verified publication lead 6,Mariut,Historical maps + Corona + modern satellite archive,Documentary/maps 1807–1958 plus Corona and later imagery can constrain lake extent independently of sediment age models,Georeferenced polygons and uncertainty envelopes,Build GIS shoreline/open-water/vegetation time slices and integrate with sediment-core RoC,Non-core forcing/validation dataset,https://egqsj.copernicus.org/articles/70/39/2021/,Verified complementary archive 7,All,Smithsonian/NMNH physical archive inquiry,"MEDIBA catalogue documents lab books, X-radiographs, colour slides and extensive short-core/surface sampling outside the long-core catalogue",Which physical short cores/residues still exist and can be resampled,Contact Smithsonian NMNH collections with core/site list from this workbook,Could convert B/C records to A/B,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download,Critical next logistical step index,Lake,A,B,C,D,A+B actionable,Interpretation 0,Manzala,3,9,8,0,12,"Best archival coverage: multiple dated/partially dated short cores with pollen, isotopes, sedimentology and geochemistry." 1,Burullus,4,5,23,0,9,"Strong modern coverage after CASSARINA, 2006/2008 cores and 2018 radio-dated geochemical cores; chronology quality varies." 2,Mariut,0,1,9,0,1,Major gap: mostly MEDIBA contextual cores; S79 is promising but reworked. No verified A-grade modern core yet. index,RoC grade,v2 operational rule,Scientific interpretation 0,A,Target lake + modern_chronology_score=2 + resolution_score=2 + >=2 quantitative proxy groups,"Immediately usable for modern/subrecent RoC, with chronology uncertainty propagated." 1,B,"Target lake + (resolution_score>=1 OR special_reanalysis_candidate=1) + >=2 quantitative proxy groups, but A not met","Useful after digitisation, cross-core alignment and/or re-dating. Includes high-resolution cores with weak chronology and special archival reanalysis candidates." 2,C,Target lake but A/B rules not met,Holocene/contextual or insufficiently resolved for direct 100-year RoC. 3,D,Outside target lake sectors,Geomorphic/chronostratigraphic control only. 4,,, 5,Helper,Scale,Meaning 6,modern_chronology_score,0–2,0 none/unreliable; 1 broad/event/partial modern constraint; 2 published modern age model/composite chronology. 7,resolution_score,0–2,0 long-core/coarse; 1 potentially modern but unresolved; 2 centimetre-scale or similarly high-resolution. 8,quantitative_proxy_count,integer,Screening count of independent quantitative proxy groups. This is not a statistical quality score. 9,special_reanalysis_candidate,0/1,"1 where existing archive material could plausibly become a modern RoC record after new dating/reanalysis (e.g., S79)." index,Source,URL,Core/data contribution,Reliability 0,"Stanley, McRea & Waldron (1996) MEDIBA catalogue",https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download,"S1–S87 coordinates, lengths, collection dates, methods, lithologic logs and 14C framework; S46–S59 Table 2 values additionally transcribed in v2.",Primary 1,Appleby et al. (2001) CASSARINA chronology,https://link.springer.com/article/10.1023/A%3A1011938522939,"MANZ1, BURL1/BULR2 chronology; 1–2 cm cores; 210Pb/137Cs/241Am plus pollen, macrofossil and SCP event dating; pre/post-1960 sedimentation rates.",Primary publisher 2,Birks et al. (2001) CASSARINA macrofossils,https://link.springer.com/article/10.1023/A%3A1013265310922,"Plant macrofossils, molluscs and faunal environmental changes used in composite Nile Delta chronologies.",Primary publisher 3,Ramdani et al. (2001) CASSARINA fauna,https://link.springer.com/article/10.1023/A%3A1011965226399,Cladocera/Ostracoda/Chironomidae/Mollusca/Foraminifera recent sediment records.,Primary publisher 4,Flower et al. (2009) MELMARINA,https://link.springer.com/article/10.1007/s10750-008-9677-5,"MANZ4, MANZ5, MANZ7, MANZ10; sediment bulk properties and radionuclide chronologies, spatial sedimentation variability.",Primary publisher 5,Xu et al. (2008) Burullus radionuclides,https://link.springer.com/article/10.1007/s11707-008-0059-0,"B-1/B-2/B-3 lengths, 5-cm radionuclide sampling, grain size, TOM, post-dam sediment-rate constraint.",Primary publisher 6,Gu et al. (2013),https://www.sciencedirect.com/science/article/abs/pii/S0272771412002314,"M-1/M-2/M-3/B-4; 3-cm grain size, nine metals, 210Pb/137Cs constraints.",Primary publisher 7,Ghanem et al. (2024),https://pmc.ncbi.nlm.nih.gov/articles/PMC11512863/,"C-1–C-4 coordinates, lengths, 4-cm slicing, 210Pb/137Cs chronology and C-2–C-4 multielement NAA.",Primary open access 8,Flaux et al. (2012),https://www.sciencedirect.com/science/article/abs/pii/S030544031200249X,S79 upper ~2 m modern interpretation and evidence for substantial shell reworking.,Primary publisher 9,Zalat & Servant-Vildary (2007),https://link.springer.com/article/10.1007/s10933-006-9029-2,565 samples from 19 cores; 263 diatom taxa across Manzala/Burullus/Edku; unresolved core-level archive lead.,Primary publisher index,Egyptian coastal-lake RoC archival reconstruction — v2,Unnamed: 1 0,What changed from v1,Added CASSARINA MANZ1/MANZ3/BURL1/BULR2; MELMARINA MANZ4/5/7/10; Burullus B-1/B-2/B-3; Gu M-1/M-2/M-3/B-4; Ghanem C-1–C-4; upgraded S79 as a special Mariut reanalysis candidate; added chronology anchors and unresolved archive leads. 1,Key correction,The strongest 20th-century cores are not the MEDIBA S1–S87 long cores. The CASSARINA and later short-core programmes provide the actual centimetre-scale modern sequences required for RoC. 2,Manzala status,"At least two A-grade archival cores are now identifiable (MANZ1 and MANZ5, in addition to Man-XX), with several B-grade replicate/proxy cores. MANZ3 is especially valuable for pollen-based land-use change." 3,Burullus status,"BULR2 is A-grade as a composite 20th-century palaeoecological sequence. C-2–C-4 are A-grade modern geochemical/radiometric cores. BURL1, B-1–B-3 and B-4 provide useful B-grade replication." 4,Mariut status,Mariut remains the limiting lake. S79 may contain an unusually thick modern section but is demonstrably reworked. The Loizeau–Stanley Mariut archive must be reconstructed before deciding on new coring. 5,14C audit,v2 adds safely parsed per-core Table 2 values for S46–S59. Other flattened Table 2 blocks are not auto-parsed where core boundaries are ambiguous; those cells remain blank rather than guessed. 6,Scoring revision,"v2 keeps the user's A–D definitions but permits B-grade 'special reanalysis candidates' even when they are long cores (e.g. S79), because new modern dating could make them useful." 7,Immediate analytical opportunity,A defensible first RoC analysis can already be built for Manzala and Burullus from high-resolution published cores; Mariut should initially be represented by landscape/historical data until a dated modern sediment sequence is verified. 8,Next archive actions,1) obtain/digitise CASSARINA raw matrices and chronology tables; 2) reconstruct all 30 Randazzo Manzala cores; 3) extract Loizeau & Stanley Mariut sites; 4) query Smithsonian/UCL physical archives; 5) harmonise all age models with uncertainty before RoC calculations. index,Core_ID,lake,lat,lon,RoC_utility,record_type,collection_year,core_length_m,modern_time_span,priority_action 0,S1,Manzala,31.448333333333334,31.778333333333332,C,MEDIBA long core,1985,28.96,,Use as long-term context 1,S2,Manzala,31.305,31.605,C,MEDIBA long core,1985,19.81,,Use as long-term context 2,S3,Manzala,31.296666666666667,31.723333333333333,C,MEDIBA long core,1985,29.87,,Use as long-term context 3,S4,Manzala,31.22833333333333,31.515,C,MEDIBA long core,1985,32.46,,Use as long-term context 4,S5,Manzala,31.193333333333335,31.65833333333333,C,MEDIBA long core,1985,27.43,,Use as long-term context 5,S6,Manzala,31.108333333333334,31.71,C,MEDIBA long core,1985,26.37,,Use as long-term context 6,S7,Manzala,31.13,31.871666666666666,C,MEDIBA long core,1985,24.38,,Use as long-term context 7,S8,Manzala,31.21333333333333,32.038333333333334,C,MEDIBA long core,1985,41.3,,Use as long-term context 8,S9,Other/control,30.97833333333333,31.878333333333334,D,MEDIBA long core,1985,15.7,,Use as long-term context 9,S10,Other/control,30.85666666666667,32.019999999999996,D,MEDIBA long core,1985,24.38,,Use as long-term context 10,S11,Other/control,30.92,32.306666666666665,D,MEDIBA long core,1985,29.87,,Use as long-term context 11,S12,Other/control,31.063333333333333,32.555,D,MEDIBA long core,1985,23.77,,Use as long-term context 12,S13,Other/control,31.078333333333333,32.39333333333333,D,MEDIBA long core,1985,30.48,,Use as long-term context 13,S14,Other/control,30.998333333333335,32.47,D,MEDIBA long core,1985,23.16,,Use as long-term context 14,S15,Other/control,31.125,32.505,D,MEDIBA long core,1985,35.36,,Use as long-term context 15,S16,Other/control,31.360000000000003,32.06333333333333,D,MEDIBA long core,1985,28.04,,Use as long-term context 16,S17,Other/control,31.378333333333334,31.965,D,MEDIBA long core,1985,43.28,,Use as long-term context 17,S18,Other/control,31.078333333333333,32.34166666666667,D,MEDIBA long core,1987,53.19,,Use as long-term context 18,S19,Other/control,31.048333333333336,32.55,D,MEDIBA long core,1987,12.19,,Use as long-term context 19,S20,Other/control,31.110000000000003,32.30166666666666,D,MEDIBA long core,1987,50.29,,Use as long-term context 20,S21,Other/control,31.229999999999997,32.34166666666667,D,MEDIBA long core,1987,49.38,,Use as long-term context 21,S22,Other/control,31.021666666666665,32.208333333333336,D,MEDIBA long core,1987,37.8,,Use as long-term context 22,S23,Other/control,30.83,32.25333333333333,D,MEDIBA long core,1987,13.72,,Use as long-term context 23,S24,Other/control,30.851666666666667,32.17166666666667,D,MEDIBA long core,1987,10.97,,Use as long-term context 24,S25,Other/control,30.961666666666666,32.18,D,MEDIBA long core,1987,14.33,,Use as long-term context 25,S26,Other/control,30.906666666666666,32.13,D,MEDIBA long core,1987,13.72,,Use as long-term context 26,S27,Other/control,31.006666666666668,32.031666666666666,D,MEDIBA long core,1987,15.24,,Use as long-term context 27,S28,Other/control,31.441666666666666,31.555,D,MEDIBA long core,1987,36.58,,Use as long-term context 28,S29,Other/control,31.361666666666668,31.451666666666664,D,MEDIBA long core,1987,39.62,,Use as long-term context 29,S30,Other/control,31.40833333333333,32.01166666666666,D,MEDIBA long core,1987,42.67,,Use as long-term context 30,S31,Other/control,31.368333333333332,31.6,D,MEDIBA long core,1988,45.72,,Use as long-term context 31,S32,Other/control,31.279999999999998,31.40833333333333,D,MEDIBA long core,1988,21.34,,Use as long-term context 32,S33,Other/control,31.411666666666665,31.363333333333333,D,MEDIBA long core,1988,25.91,,Use as long-term context 33,S34,Other/control,31.453333333333333,31.388333333333332,D,MEDIBA long core,1988,39.62,,Use as long-term context 34,S35,Other/control,31.528333333333332,31.308333333333334,D,MEDIBA long core,1988,35.05,,Use as long-term context 35,S36,Other/control,31.46333333333333,31.256666666666668,D,MEDIBA long core,1988,45.72,,Use as long-term context 36,S37,Other/control,31.37,31.279999999999998,D,MEDIBA long core,1988,21.34,,Use as long-term context 37,S38,Burullus,31.421666666666667,31.173333333333336,C,MEDIBA long core,1988,27.43,,Use as long-term context 38,S39,Burullus,31.42,31.073333333333334,C,MEDIBA long core,1988,18.29,,Use as long-term context 39,S40,Burullus,31.513333333333332,31.141666666666666,C,MEDIBA long core,1988,28.19,,Use as long-term context 40,S41,Burullus,31.575,31.205,C,MEDIBA long core,1988,51.82,,Use as long-term context 41,S42,Burullus,31.598333333333333,31.096666666666664,C,MEDIBA long core,1988,45.72,,Use as long-term context 42,S43,Burullus,31.586666666666666,30.97833333333333,C,MEDIBA long core,1988,42.67,,Use as long-term context 43,S44,Burullus,31.436666666666667,30.991666666666667,C,MEDIBA long core,1988,21.34,,Use as long-term context 44,S45,Burullus,31.508333333333333,31.031666666666666,C,MEDIBA long core,1988,30.48,,Use as long-term context 45,S46,Burullus,31.4,30.981666666666666,C,MEDIBA long core,1988,45.72,,Use as long-term context 46,S47,Burullus,31.540000000000003,30.836666666666666,C,MEDIBA long core,1989,42.67,,Use as long-term context 47,S48,Burullus,31.503333333333334,30.775,C,MEDIBA long core,1989,43.28,,Use as long-term context 48,S49,Burullus,31.474999999999998,30.685,C,MEDIBA long core,1989,41.15,,Use as long-term context 49,S50,Burullus,31.435,30.581666666666667,C,MEDIBA long core,1989,41.15,,Use as long-term context 50,S51,Burullus,31.37,30.495,C,MEDIBA long core,1989,41.15,,Use as long-term context 51,S52,Burullus,31.406666666666666,30.77,C,MEDIBA long core,1989,41.15,,Use as long-term context 52,S53,Burullus,31.395,30.67666666666667,C,MEDIBA long core,1989,27.43,,Use as long-term context 53,S54,Burullus,31.326666666666668,30.791666666666668,C,MEDIBA long core,1989,19.51,,Use as long-term context 54,S55,Burullus,31.315,30.671666666666667,C,MEDIBA long core,1989,19.81,,Use as long-term context 55,S56,Burullus,31.325,30.523333333333333,C,MEDIBA long core,1989,19.81,,Use as long-term context 56,S57,Burullus,31.373333333333335,30.595,C,MEDIBA long core,1989,19.81,,Use as long-term context 57,S58,Burullus,31.384999999999998,30.43,C,MEDIBA long core,1989,22.86,,Use as long-term context 58,S59,Burullus,31.461666666666666,30.441666666666666,C,MEDIBA long core,1989,41.15,,Use as long-term context 59,S60,Other/control,31.328333333333333,30.41,D,MEDIBA long core,1989,30.48,,Use as long-term context 60,S61,Other/control,31.226666666666667,30.371666666666666,D,MEDIBA long core,1989,41.15,,Use as long-term context 61,S62,Other/control,31.275,30.328333333333333,D,MEDIBA long core,1989,24.38,,Use as long-term context 62,S63,Other/control,31.35,30.315,D,MEDIBA long core,1989,22.25,,Use as long-term context 63,S64,Other/control,31.40833333333333,30.345,D,MEDIBA long core,1989,41.15,,Use as long-term context 64,S65,Other/control,31.476666666666667,30.358333333333334,D,MEDIBA long core,1989,48.62,,Use as long-term context 65,S66,Other/control,31.26833333333333,30.456666666666667,D,MEDIBA long core,1990,20.12,,Use as long-term context 66,S67,Other/control,31.175,30.331666666666667,D,MEDIBA long core,1990,19.81,,Use as long-term context 67,S68,Other/control,31.275,30.231666666666666,D,MEDIBA long core,1990,44.2,,Use as long-term context 68,S69,Other/control,31.193333333333335,30.275,D,MEDIBA long core,1990,19.81,,Use as long-term context 69,S70,Other/control,31.18166666666667,30.173333333333336,D,MEDIBA long core,1990,19.81,,Use as long-term context 70,S71,Other/control,31.265,30.173333333333336,D,MEDIBA long core,1990,44.2,,Use as long-term context 71,S72,Other/control,31.231666666666666,30.133333333333333,D,MEDIBA long core,1990,19.81,,Use as long-term context 72,S73,Mariut,31.276666666666667,30.083333333333332,C,MEDIBA long core,1990,44.2,,Use as long-term context 73,S74,Mariut,31.223333333333333,30.078333333333333,C,MEDIBA long core,1990,18.29,,Use as long-term context 74,S75,Mariut,31.273333333333333,30.046666666666667,C,MEDIBA long core,1990,24.38,,Use as long-term context 75,S76,Mariut,31.229999999999997,30.013333333333332,C,MEDIBA long core,1990,19.81,,Use as long-term context 76,S77,Mariut,31.18,29.93166666666667,C,MEDIBA long core,1990,40.54,,Use as long-term context 77,S78,Mariut,31.15,30.040000000000003,C,MEDIBA long core,1990,19.81,,Use as long-term context 78,S79,Mariut,31.103333333333335,29.948333333333334,B,MEDIBA long core — modern upper section candidate,1990,42.67,Upper ~2 m proposed as 20th century; interpretation contested by reworking,High-priority archive reanalysis: locate upper S79 material and apply modern radionuclide/SCP dating if preserved 79,S80,Mariut,31.101666666666667,29.853333333333335,C,MEDIBA long core,1990,45.72,,Use as long-term context 80,S81,Mariut,31.053333333333335,29.991666666666667,C,MEDIBA long core,1990,21.34,,Use as long-term context 81,S82,Mariut,31.05,29.873333333333335,C,MEDIBA long core,1990,30.48,,Use as long-term context 82,S83,Other/control,31.05666666666667,29.77,D,MEDIBA long core,1990,45.72,,Use as long-term context 83,S84,Other/control,30.993333333333336,29.618333333333332,D,MEDIBA long core,1990,22.86,,Use as long-term context 84,S85,Other/control,30.923333333333336,29.526666666666667,D,MEDIBA long core,1990,10.21,,Use as long-term context 85,S86,Other/control,30.855,30.796666666666667,D,MEDIBA long core,1990,41.15,,Use as long-term context 86,S87,Other/control,30.740000000000002,31.031666666666666,D,MEDIBA long core,1990,41.15,,Use as long-term context 87,C-1,Burullus,31.4162998,30.7656002,C,Modern radio-dated Burullus core,2018,0.56,Approximately mid-20th century–2018 in dated sections,Use as chronology/spatial sedimentation control 88,C-2,Burullus,31.4762993,30.8225002,A,Modern radio-dated Burullus core,2018,0.56,Approximately mid-20th century–2018 in dated sections,Immediate extraction of age-depth + elemental profiles 89,C-3,Burullus,31.5697002,30.9789009,A,Modern radio-dated Burullus core,2018,0.48,Approximately mid-20th century–2018 in dated sections,Immediate extraction of age-depth + elemental profiles 90,C-4,Burullus,31.4039001,30.5893002,A,Modern radio-dated Burullus core,2018,0.48,Approximately mid-20th century–2018 in dated sections,Immediate extraction of age-depth + elemental profiles index,Core_ID,depth_m,Smithsonian_sample,lab_sample_number,laboratory,age_raw,age_BP,one_sigma_error,age_status,lower_bound_BP,publication_page,pdf_page,table_side,source_url 0,S1,2.0,A,19414,Beta Analytic Inc.,2930 ± 90,2930.0,90.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 1,S7,12.5,J,SI7050A,Smithsonian Radiobiology Laboratory,14030 ± 240,14030.0,240.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 2,S1,8.0,B,19415,Beta Analytic Inc.,3230 ±160,3230.0,160.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 3,S7,15.5,K,SI7051A,Smithsonian Radiobiology Laboratory,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 4,S1,9.5,C,19416,Beta Analytic Inc.,2360 ±100,2360.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 5,S7,16.0,D,17246,Beta Analytic Inc.,32910 ±1740,32910.0,1740.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 6,S1,15.5,D,19417,Beta Analytic Inc.,6410 ±180,6410.0,180.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 7,S7,18.0,L,SI7052A,Smithsonian Radiobiology Laboratory,26800 ± 560,26800.0,560.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 8,S1,23.0,E,19418,Beta Analytic Inc.,7590 ±130,7590.0,130.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 9,S7,19.0,M,SI7053A,Smithsonian Radiobiology Laboratory,38220 ±800,38220.0,800.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 10,S1,28.0,F,19419,Beta Analytic Inc.,7440 ± 90,7440.0,90.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 11,S8,1.0,A,17248,Beta Analytic Inc.,4170 ±120,4170.0,120.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 12,S2,1.5,A,18554,Beta Analytic Inc.,1830 ±70,1830.0,70.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 13,S8,3.0,A',SI7106,Smithsonian Radiobiology Laboratory,4025 ±180,4025.0,180.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 14,S2,3.5,B,18555,Beta Analytic Inc.,3800 ±90,3800.0,90.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 15,S8,5.0,B,17249,Beta Analytic Inc.,4230 ±90,4230.0,90.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 16,S2,7.5,C,18556,Beta Analytic Inc.,5110±80,5110.0,80.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 17,S8,9.5,B,SI7107,Smithsonian Radiobiology Laboratory,4695 ±115,4695.0,115.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 18,S2,9.5,D,18557,Beta Analytic Inc.,6580 ±100,6580.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 19,S8,16.0,C,SI7108,Smithsonian Radiobiology Laboratory,5110 ±90,5110.0,90.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 20,S2,12.5,E,18558,Beta Analytic Inc.,7110±70,7110.0,70.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 21,S8,20.0,D,SI7109,Smithsonian Radiobiology Laboratory,6965 ±110,6965.0,110.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 22,S2,19.0,F,18559,Beta Analytic Inc.,14000 ±280,14000.0,280.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 23,S8,25.0,E,17110,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 24,S8,26.0,F,17111,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 25,S3,3.0,A,20255,Beta Analytic Inc.,3030 ± 80,3030.0,80.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 26,S8,27.0,E,17250,Beta Analytic Inc.,6760 ±140,6760.0,140.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 27,S3,8.5,B,20256,Beta Analytic Inc.,4200 ±100,4200.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 28,S8,36.0,F,17251,Beta Analytic Inc.,7300 ±110,7300.0,110.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 29,S3,11.0,C,20257,Beta Analytic Inc.,5950 ±100,5950.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 30,S8,40.0,G,SI7112,Smithsonian Radiobiology Laboratory,9060 ±90,9060.0,90.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 31,S3,15.5,D,20258,Beta Analytic Inc.,7510± 110,7510.0,110.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 32,S3,21.5,E,20259,Beta Analytic Inc.,7180± 110,7180.0,110.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 33,S9,2.0,A,17252,Beta Analytic Inc.,3740 ±150,3740.0,150.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 34,S3,26.0,F,20260,Beta Analytic Inc.,7480 ± 90,7480.0,90.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 35,S9,4.5,B,17253,Beta Analytic Inc.,5140±80,5140.0,80.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 36,S9,12.0,C,17254,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 37,S4,1.0,A,18905,Beta Analytic Inc.,2990 ± 90,2990.0,90.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 38,S4,2.5,B,18906,Beta Analytic Inc.,2150±100,2150.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 39,S10,7.0,A,17255,Beta Analytic Inc.,21880 ±970,21880.0,970.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 40,S4,5.5,C,18907,Beta Analytic Inc.,4080 ±130,4080.0,130.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 41,S10,8.0,B,17256,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 42,S4,7.5,D,18908,Beta Analytic Inc.,5330 ±120,5330.0,120.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 43,S11,2.0,A,16686,Beta Analytic Inc.,2550 ± 80,2550.0,80.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 44,S4,10.0,E,18909,Beta Analytic Inc.,5510±150,5510.0,150.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 45,S11,5.5,B,16687,Beta Analytic Inc.,4570 ±170,4570.0,170.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 46,S4,12.5,F,18910,Beta Analytic Inc.,6880 ±100,6880.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 47,S11,8.5,C,16688,Beta Analytic Inc.,5190 ±100,5190.0,100.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 48,S4,14.0,G,18911,Beta Analytic Inc.,7020 ±120,7020.0,120.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 49,S11,11.0,D,16689,Beta Analytic Inc.,6110 ±120,6110.0,120.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 50,S4,16.0,H,18912,Beta Analytic Inc.,7020 ±140,7020.0,140.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 51,S11,14.5,E,16690,Beta Analytic Inc.,6475 ± 90,6475.0,90.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 52,S5,2.0,A,20544,Beta Analytic Inc.,1450 ±80,1450.0,80.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 53,S11,23.0,F,16691,Beta Analytic Inc.,9820 ±400,9820.0,400.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 54,S5,4.5,B,20545,Beta Analytic Inc.,2450 ± 80,2450.0,80.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 55,S12,2.0,A,18115,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 56,S5,7.5,C,20546,Beta Analytic Inc.,4340±120,4340.0,120.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 57,S12,5.5,B,18116,Beta Analytic Inc.,1500 ±80,1500.0,80.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 58,S5,13.0,D,20547,Beta Analytic Inc.,6390 ±110,6390.0,110.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 59,S12,9.5,C,18117,Beta Analytic Inc.,3550 ±100,3550.0,100.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 60,S5,17.0,E,20548,Beta Analytic Inc.,7010± 140,7010.0,140.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 61,S5,21.5,F,20549,Beta Analytic Inc.,7620 ±110,7620.0,110.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 62,S12,13.5,D,18118,Beta Analytic Inc.,7280 ±490,7280.0,490.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 63,S12,18.0,E,18119,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 64,S5,28.5,G,20550,Beta Analytic Inc.,7500±110,7500.0,110.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 65,S12,24.0,F,,Not assigned,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 66,S5,29.0,H,20551,Beta Analytic Inc.,11290 ±160,11290.0,160.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 67,S13,5.0,A,16534,Beta Analytic Inc.,3760 ± 70,3760.0,70.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 68,S6,1.5,A,16340,Beta Analytic Inc.,1910 ±70 ',1910.0,70.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 69,S13,8.0,B,16535,Beta Analytic Inc.,3640 ±120,3640.0,120.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 70,S6,5.5,B,16341,Beta Analytic Inc.,3750 ±60,3750.0,60.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 71,S6,10.5,C,16342,Beta Analytic Inc.,6930 ±110,6930.0,110.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 72,S13,11.5,C,16536,Beta Analytic Inc.,4050 ±110,4050.0,110.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 73,S6,18.0,D,16343,Beta Analytic Inc.,7790 ±110,7790.0,110.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 74,S13,16.0,D,16537,Beta Analytic Inc.,3000±110,3000.0,110.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 75,S13,21.0,E,16538,Beta Analytic Inc.,5130 ±90,5130.0,90.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 76,S6,20.5,E,16344,Beta Analytic Inc.,24820 ± 400,24820.0,400.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 77,S14,1.5,A,18120,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 78,S7,1.5,A,SI7041A,Smithsonian Radiobiology Laboratory,2340 ± 90,2340.0,90.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 79,S7,2.0,A,17243,Beta Analytic Inc.,4230 ±100,4230.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 80,S14,5.0,B,18121,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 81,S7,2.5,B,SI7042B,Smithsonian Radiobiology Laboratory,3805 ± 40,3805.0,40.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 82,S14,6.5,E,18125,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 83,S7,3.5,C,SI7043B,Smithsonian Radiobiology Laboratory,2110± 100,2110.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 84,S14,7.5,C,18123,Beta Analytic Inc.,> 23210,23210.0,,lower_bound,23210.0,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 85,S7,5.0,B,17244,Beta Analytic Inc.,6300 ±100,6300.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 86,S14,8.5,D,18124,Beta Analytic Inc.,26270 ±3850,26270.0,3850.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 87,S7,5.5,E,17247,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 88,S14,13.0,F,18126,Beta Analytic Inc.,7440 ±370,7440.0,370.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 89,S14,16.0,G,18127,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 90,S7,6.0,E,SI7045B,Smithsonian Radiobiology Laboratory,6325 ±120,6325.0,120.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 91,S14,22.0,H,18128,Beta Analytic Inc.,Insufficient C,,,insufficient,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 92,S7,7.0,F,SI7046B,Smithsonian Radiobiology Laboratory,5720 ± 70,5720.0,70.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 93,S7,8.0,C,17245,Beta Analytic Inc.,6500 ±100,6500.0,100.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 94,S15,3.5,A,17831,Beta Analytic Inc.,1620 ±70,1620.0,70.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 95,S7,8.0,G,SI7047A,Smithsonian Radiobiology Laboratory,8215 ±155,8215.0,155.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 96,S15,7.0,B,17832,Beta Analytic Inc.,4370 ±160,4370.0,160.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 97,S7,8.0,G,SI7047B,Smithsonian Radiobiology Laboratory,7610 ±90,7610.0,90.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 98,S15,10.5,C,17833,Beta Analytic Inc.,2620 ±80,2620.0,80.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 99,S7,9.5,H,SI7048A,Smithsonian Radiobiology Laboratory,Insufficient C,,,insufficient,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 100,S15,14.5,D,17834,Beta Analytic Inc.,3870 ±80,3870.0,80.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 101,S7,10.0,H,SI7048B,Smithsonian Radiobiology Laboratory,5285 ±155,5285.0,155.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 102,S15,20.0,E,17835,Beta Analytic Inc.,4170 ± 9 0,4170.0,90.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 103,S7,11.0,I,SI7049A,Smithsonian Radiobiology Laboratory,12870 ±180,12870.0,180.0,dated,,14,20,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 104,S15,25.5,F,17836,Beta Analytic Inc.,6760 ±90,6760.0,90.0,dated,,14,20,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 105,S15,35.0,H,17838,Beta Analytic Inc.,7420 ±90,7420.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 106,S25,3.5,A,25463,Beta Analytic Inc.,3860 ±90,3860.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 107,S16,3.0,A,,Not assigned,16345,16345.0,,dated_unresolved_error,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 108,S25,8.0,B,25464,Beta Analytic Inc.,6630 ±110,6630.0,110.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 109,S16,9.0,B,16346,Beta Analytic Inc.,1940 ±90,1940.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 110,S25,12.5,C,25465,Beta Analytic Inc.,6760 ±100,6760.0,100.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 111,S16,14.0,C,16347,Beta Analytic Inc.,4500 ± 90,4500.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 112,S25,14.0,D,25466,Beta Analytic Inc.,6210±100,6210.0,100.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 113,S16,18.0,D,16348,Beta Analytic Inc.,4820 ±80,4820.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 114,S26,1.0,K,24895,Beta Analytic Inc.,2500 ±170,2500.0,170.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 115,S16,23.0,E,16349,Beta Analytic Inc.,7700 ±110,7700.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 116,S26,2.5,L,24896,Beta Analytic Inc.,2820 ±120,2820.0,120.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 117,S16,27.5,F,16350,Beta Analytic Inc.,7340 ±90,7340.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 118,S26,5.0,M,24897,Beta Analytic Inc.,4370 ±170,4370.0,170.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 119,S17,2.0,A,20079,Beta Analytic Inc.,1420 ±80,1420.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 120,S26,5.5,N,24898,Beta Analytic Inc.,4210 ±90,4210.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 121,S17,8.0,B,20080,Beta Analytic Inc.,4200 ±120,4200.0,120.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 122,S26,6.5,O,24899,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 123,S17,12.5,C,20081,Beta Analytic Inc.,4480 ±110,4480.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 124,S27,2.0,A,25537,Beta Analytic Inc.,3160 ±120,3160.0,120.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 125,S17,19.0,D,20082,Beta Analytic Inc.,4890 ±110,4890.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 126,S27,6.0,B,25538,Beta Analytic Inc.,2520 ±90,2520.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 127,S17,30.0,E,20083,Beta Analytic Inc.,7980 ±90,7980.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 128,S27,6.5,C,25539,Beta Analytic Inc.,2980 ±70,2980.0,70.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 129,S17,35.0,F,20084,Beta Analytic Inc.,7850 ±100,7850.0,100.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 130,S27,9.0,D,25540,Beta Analytic Inc.,3330 ± 90,3330.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 131,S17,42.5,G,20085,Beta Analytic Inc.,8940 ±120,8940.0,120.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 132,S27,10.5,E,25541,Beta Analytic Inc.,6560 ±90,6560.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 133,S17,30.0,F,16539,Beta Analytic Inc.,7150± 110,7150.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 134,S28,5.0,F,26381,Beta Analytic Inc.,4500 ±120,4500.0,120.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 135,S18,1.5,A,24004,Beta Analytic Inc.,1400 ±80,1400.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 136,S28,18.0,G,26382,Beta Analytic Inc.,8640±110,8640.0,110.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 137,S18,6.5,B,24005,Beta Analytic Inc.,4650 ±120,4650.0,120.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 138,S28,23.5,H,26383,Beta Analytic Inc.,7230 ±80,7230.0,80.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 139,S18,11.0,C,24006,Beta Analytic Inc.,4100 ±70,4100.0,70.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 140,S28,26.0,I,26384,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 141,S18,17.5,D,24007,Beta Analytic Inc.,4480 ±110,4480.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 142,S28,28.0,J,26385,Beta Analytic Inc.,10950 ±90,10950.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 143,S18,26.0,E,24008,Beta Analytic Inc.,7400 ±80,7400.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 144,S28,35.0,K,26386,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 145,S18,27.5,F,24009,Beta Analytic Inc.,4040 ±100,4040.0,100.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 146,S18,41.0,G,24010,Beta Analytic Inc.,11530 ±80,11530.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 147,S29,4.0,A,26387,Beta Analytic Inc.,3460 ±100,3460.0,100.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 148,S18,52.5,H,24011,Beta Analytic Inc.,12070 ±370,12070.0,370.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 149,S29,6.0,B,26388,Beta Analytic Inc.,4580 ±100,4580.0,100.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 150,S29,7.0,C,26389,Beta Analytic Inc.,5190 ±90,5190.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 151,S19,1.0,F,24890,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 152,S29,9.0,D,26390,Beta Analytic Inc.,4910 ±90,4910.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 153,S19,4.0,G,24891,Beta Analytic Inc.,3070 ±110,3070.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 154,S29,18.0,E,26391,Beta Analytic Inc.,8870 ±170,8870.0,170.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 155,S19,6.5,H,24892,Beta Analytic Inc.,3960 ±100,3960.0,100.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 156,S19,8.5,I,24893,Beta Analytic Inc.,4080 ± 90,4080.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 157,S30,18.5,A,26910,Beta Analytic Inc.,5270 ± 9 0,5270.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 158,S19,11.5,J,24894,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 159,S30,22.5,B,26911,Beta Analytic Inc.,5020 ±110,5020.0,110.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 160,S30,26.5,C,26912,Beta Analytic Inc.,8090 ±120,8090.0,120.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 161,S20,2.0,A,25256,Beta Analytic Inc.,2890 ±130,2890.0,130.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 162,S30,27.5,D,26913,Beta Analytic Inc.,8040 ±250,8040.0,250.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 163,S20,11.0,B,25257,Beta Analytic Inc.,4190 ± 90,4190.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 164,S30,28.5,E,26914,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 165,S20,22.0,C,25258,Beta Analytic Inc.,5110± 110,5110.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 166,S30,34.0,F,26915,Beta Analytic Inc.,10770 ±120,10770.0,120.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 167,S20,27.5,D,25259,Beta Analytic Inc.,7460 ± 80,7460.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 168,S20,34.0,E,25260,Beta Analytic Inc.,7260 ±90,7260.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 169,S31,4.5,A,32455,Beta Analytic Inc.,3260 ±90,3260.0,90.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 170,S20,40.0,F,25261,Beta Analytic Inc.,7630 ± 90,7630.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 171,S31,10.5,B,32456,Beta Analytic Inc.,5840 ±140,5840.0,140.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 172,S20,42.0,G,25262,Beta Analytic Inc.,7360 ± 90,7360.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 173,S31,15.0,C,32457,Beta Analytic Inc.,6590 ±110,6590.0,110.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 174,S20,45.0,H,25263,Beta Analytic Inc.,15110±640,15110.0,640.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 175,S31,19.5,D,32458,Beta Analytic Inc.,7650 ±150,7650.0,150.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 176,S31,25.0,E,32459,Beta Analytic Inc.,7850 ±140,7850.0,140.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 177,S21,1.0,A,25937,Beta Analytic Inc.,3400 ±140,3400.0,140.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 178,S31,27.0,F,32460,Beta Analytic Inc.,6880 ±80,6880.0,80.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 179,S21,9.5,B,25938,Beta Analytic Inc.,3530 ±90,3530.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 180,S31,28.0,G,32461,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 181,S21,16.0,C,25939,Beta Analytic Inc.,3870 ±100,3870.0,100.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 182,S31,28.5,H,33115,Beta Analytic Inc.,> 25670,25670.0,,lower_bound,25670.0,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 183,S21,25.0,D,25940,Beta Analytic Inc.,4520 ±110,4520.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 184,S21,34.0,E,25941,Beta Analytic Inc.,5780 ±130,5780.0,130.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 185,S32,7.5,A,33116,Beta Analytic Inc.,5880 ±170,5880.0,170.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 186,S21,40.5,F,25942,Beta Analytic Inc.,7140 ±110,7140.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 187,S32,11.5,B,33117,Beta Analytic Inc.,7100 ±130,7100.0,130.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 188,S21,46.0,G,25943,Beta Analytic Inc.,8190± 110,8190.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 189,S32,12.0,C,33118,Beta Analytic Inc.,7960 ±150,7960.0,150.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 190,S21,48.0,H,25944,Beta Analytic Inc.,8140± 130,8140.0,130.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 191,S32,19.0,D,33119,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 192,S22,0.5,A,23672,Beta Analytic Inc.,3630 ±110,3630.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 193,S33,12.0,A,30599,Beta Analytic Inc.,5500 ±190,5500.0,190.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 194,S22,3.0,B,23673,Beta Analytic Inc.,3770 ± 90,3770.0,90.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 195,S33,12.5,B,30600,Beta Analytic Inc.,3560 ±150,3560.0,150.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 196,S22,8.0,C,23674,Beta Analytic Inc.,4670 ±80,4670.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 197,S33,21.0,C,30601,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 198,S22,14.0,D,23675,Beta Analytic Inc.,6630 ±150,6630.0,150.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 199,S33,21.5,D,30602,Beta Analytic Inc.,34380 ±1740,34380.0,1740.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 200,S22,21.5,E,23676,Beta Analytic Inc.,7910 ±150,7910.0,150.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 201,S34,13.0,A,30603,Beta Analytic Inc.,8370 ±180,8370.0,180.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 202,S22,22.0,F,23677,Beta Analytic Inc.,7540 + 70,7540.0,,dated_unresolved_error,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 203,S34,13.5,B,30604,Beta Analytic Inc.,6710 ±190,6710.0,190.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 204,S22,31.0,G,23678,Beta Analytic Inc.,32920 ±930,32920.0,930.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 205,S34,24.0,C,30605,Beta Analytic Inc.,19450 ±840,19450.0,840.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 206,S22,37.0,H,23679,Beta Analytic Inc.,24320 ± 2030,24320.0,2030.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 207,S34,25.0,D,30606,Beta Analytic Inc.,21050 ±920,21050.0,920.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 208,S23,1.5,A,24885,Beta Analytic Inc.,2490 ±80,2490.0,80.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 209,S35,10.0,F,31486,Beta Analytic Inc.,6160 ±80,6160.0,80.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 210,S23,5.0,B,24886,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 211,S35,17.5,E,31485,Beta Analytic Inc.,7730 ±120,7730.0,120.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 212,S24,0.5,C,24887A,Beta Analytic Inc.,4130 ±180,4130.0,180.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 213,S35,21.0,A,30607,Beta Analytic Inc.,7260 ±110,7260.0,110.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 214,S24,7.5,D,24887B,Beta Analytic Inc.,9200 ±110,9200.0,110.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 215,S35,22.5,B,30608,Beta Analytic Inc.,4770 ±110,4770.0,110.0,dated,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 216,S24,10.0,E,24889,Beta Analytic Inc.,24240 ±1510,24240.0,1510.0,dated,,15,21,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 217,S35,30.0,C,30609,Beta Analytic Inc.,Insufficient C,,,insufficient,,15,21,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 218,S36,14.0,A,30610,Beta Analytic Inc.,7080 ±120,7080.0,120.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 219,S46,8.0,A,34478,Beta Analytic Inc.,7130 ±80,7130.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 220,S36,14.5,B,30611,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 221,S46,10.5,B,34479,Beta Analytic Inc.,6620 ±70,6620.0,70.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 222,S36,25.0,C,30612,Beta Analytic Inc.,27720 ± 670,27720.0,670.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 223,S46,12.0,C,34480,Beta Analytic Inc.,12940 ±240,12940.0,240.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 224,S36,34.5,D,30613,Beta Analytic Inc.,25570 ± 720,25570.0,720.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 225,S46,18.0,D,34481,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 226,S37,5.0,A,33120,Beta Analytic Inc.,3260 ± 80,3260.0,80.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 227,S47,5.5,A,36764,Beta Analytic Inc.,4270 ±110,4270.0,110.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 228,S37,12.5,B,33121,Beta Analytic Inc.,6870 ±170,6870.0,170.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 229,S47,15.0,B,36765,Beta Analytic Inc.,8050 ±140,8050.0,140.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 230,S47,23.0,C,36767,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 231,S38,12.0,G,31487,Beta Analytic Inc.,7240 ±90,7240.0,90.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 232,S38,13.0,A,30117,Beta Analytic Inc.,7210 ±130,7210.0,130.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 233,S47,30.0,D,36766,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 234,S38,14.0,B,30118,Beta Analytic Inc.,3380 ±200,3380.0,200.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 235,S47,37.0,E,36768,Beta Analytic Inc.,26820 ±1340,26820.0,1340.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 236,S38,18.0,C,30119,Beta Analytic Inc.,21090 ±600,21090.0,600.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 237,S48,3.0,A,37298,Beta Analytic Inc.,1610±60,1610.0,60.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 238,S38,23.0,D,30120,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 239,S48,4.5,B,37299,Beta Analytic Inc.,1670 ±50,1670.0,50.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 240,S38,29.5,E,30121,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 241,S48,7.5,C,37300,Beta Analytic Inc.,4480 ±80,4480.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 242,S38,31.0,F,30122,Beta Analytic Inc.,> 29260,29260.0,,lower_bound,29260.0,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 243,S48,14.0,D,37301,Beta Analytic Inc.,6340 ±100,6340.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 244,S39,1.5,D,33122,Beta Analytic Inc.,3840 ±100,3840.0,100.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 245,S49,6.0,A,36769,Beta Analytic Inc.,3190 ±90,3190.0,90.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 246,S39,2.5,A,29858,Beta Analytic Inc.,4540 ± 290,4540.0,290.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 247,S49,11.0,B,36770,Beta Analytic Inc.,5410 ±100,5410.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 248,S39,4.0,C,29860,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 249,S49,15.0,C,36771,Beta Analytic Inc.,7170 ±180,7170.0,180.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 250,S39,13.5,E,33123,Beta Analytic Inc.,21700 ±2460,21700.0,2460.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 251,S49,26.0,D,36772,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 252,S39,13.5,B,29859,Beta Analytic Inc.,11320 ±290,11320.0,290.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 253,S50,4.5,A,37302,Beta Analytic Inc.,2870 ±80,2870.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 254,S40,3.0,E,33124,Beta Analytic Inc.,3430 ±110,3430.0,110.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 255,S50,16.0,B,37303,Beta Analytic Inc.,6600 ±80,6600.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 256,S40,15.5,A,29861,Beta Analytic Inc.,7450 ±120,7450.0,120.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 257,S50,24.0,C,37304,Beta Analytic Inc.,7950 ±90,7950.0,90.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 258,S40,16.5,C,29863,Beta Analytic Inc.,3540 ±150,3540.0,150.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 259,S50,25.5,D,37305,Beta Analytic Inc.,11040 ±330,11040.0,330.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 260,S40,25.5,D,29864,Beta Analytic Inc.,6050 ±140,6050.0,140.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 261,S40,27.5,F,33125,Beta Analytic Inc.,19350 ±950,19350.0,950.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 262,S51,5.5,A,37747,Beta Analytic Inc.,3800 ±60,3800.0,60.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 263,S40,26.5,B,29862,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 264,S51,8.0,B,37748,Beta Analytic Inc.,5930 ±130,5930.0,130.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 265,S51,11.5,C,37749,Beta Analytic Inc.,6580 ±110,6580.0,110.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 266,S41,8.5,D,29867,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 267,S41,9.0,F,31489,Beta Analytic Inc.,3060 ±70,3060.0,70.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 268,S52,2.0,A,37750,Beta Analytic Inc.,1670 ±60,1670.0,60.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 269,S41,18.0,A,31488,Beta Analytic Inc.,6630 ±250,6630.0,250.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 270,S52,6.0,B,37751,Beta Analytic Inc.,3250 ±100,3250.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 271,S41,20.0,B,29865,Beta Analytic Inc.,6330 ±100,6330.0,100.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 272,S52,7.5,C,37752,Beta Analytic Inc.,4790 ±70,4790.0,70.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 273,S41,20.5,E,29868,Beta Analytic Inc.,3490 ±100,3490.0,100.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 274,S52,11.5,D,37753,Beta Analytic Inc.,6550 ±80,6550.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 275,S41,24.0,C,29866,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 276,S52,12.0,E,37754,Beta Analytic Inc.,10510 ±130,10510.0,130.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 277,S41,25.0,D,29867,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 278,S53,4.0,A,37755,Beta Analytic Inc.,2470 ±60,2470.0,60.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 279,S41,25.5,G,33126,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 280,S53,10.0,B,37756,Beta Analytic Inc.,5820 ±100,5820.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 281,S41,14.5,G,31490,Beta Analytic Inc.,3870 ±110,3870.0,110.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 282,S53,11.0,C,37757,Beta Analytic Inc.,11930 ±170,11930.0,170.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 283,S42,5.0,E,31492,Beta Analytic Inc.,3610 ±110,3610.0,110.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 284,S53,14.5,D,37758,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 285,S42,11.0,F,31493,Beta Analytic Inc.,4890 ±100,4890.0,100.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 286,S42,21.0,D,31491,Beta Analytic Inc.,7410 ±100,7410.0,100.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 287,S54,5.0,A,38098,Beta Analytic Inc.,3080 ±70,3080.0,70.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 288,S54,9.5,B,38099,Beta Analytic Inc.,5990 ±100,5990.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 289,S42,23.0,A,29869,Beta Analytic Inc.,8290 ±120,8290.0,120.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 290,S42,24.0,B,29870,Beta Analytic Inc.,6730 ±150,6730.0,150.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 291,S54,10.0,C,38100,Beta Analytic Inc.,12310 ±120,12310.0,120.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 292,S42,28.0,C,29871,Beta Analytic Inc.,7860 ±90,7860.0,90.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 293,S54,14.5,D,38101,Beta Analytic Inc.,22820 ± 770,22820.0,770.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 294,S42,4.0,E,31494,Beta Analytic Inc.,4620 ±130,4620.0,130.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 295,S55,3.5,A,37759,Beta Analytic Inc.,2420 ±110,2420.0,110.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 296,S43,7.0,F,31495,Beta Analytic Inc.,5610 ±110,5610.0,110.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 297,S55,6.0,B,37760,Beta Analytic Inc.,3400 ±100,3400.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 298,S43,14.0,A,29872,Beta Analytic Inc.,6970 ±110,6970.0,110.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 299,S55,7.0,C,37761,Beta Analytic Inc.,4170 ±90,4170.0,90.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 300,S43,14.5,D,29875,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 301,S55,9.5,D,37762,Beta Analytic Inc.,14120 ±160,14120.0,160.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 302,S43,18.0,B,29873,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 303,S56,8.5,A,37763,Beta Analytic Inc.,1490 ±80,1490.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 304,S43,18.5,E,33127,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 305,S43,25.0,F,33128,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 306,S57,6.0,A,38102,Beta Analytic Inc.,3630 ±70,3630.0,70.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 307,S43,24.5,C,29874,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 308,S57,12.0,B,38103,Beta Analytic Inc.,6310 ±90,6310.0,90.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 309,S57,13.5,C,38104,Beta Analytic Inc.,13630 ±100,13630.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 310,S44,2.0,A,46010,Beta Analytic Inc.,2570 ±70,2570.0,70.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 311,S44,5.0,B,46011,Beta Analytic Inc.,3980 ±80,3980.0,80.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 312,S58,3.0,A,38091,Beta Analytic Inc.,3020 ±80,3020.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 313,S44,6.5,C,46012,Beta Analytic Inc.,3260 ±90,3260.0,90.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 314,S58,5.5,B,38092,Beta Analytic Inc.,3770 ±80,3770.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 315,S44,10.5,A,30123,Beta Analytic Inc.,6370 ±180,6370.0,180.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 316,S58,11.5,c,38093,Beta Analytic Inc.,4890 ±80,4890.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 317,S44,14.0,B,30124,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 318,S58,16.0,D,38094,Beta Analytic Inc.,7500 ±70,7500.0,70.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 319,S44,14.5,C,33129,Beta Analytic Inc.,15600 ±290,15600.0,290.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 320,S59,11.5,A,37306,Beta Analytic Inc.,3140±100,3140.0,100.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 321,S59,17.0,B,37307,Beta Analytic Inc.,3560 ± 80,3560.0,80.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 322,S45,12.5,A,30125,Beta Analytic Inc.,7100±160,7100.0,160.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 323,S59,27.5,C,37308,Beta Analytic Inc.,9110 ±120,9110.0,120.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 324,S45,13.0,B,30126,Beta Analytic Inc.,Insufficient C,,,insufficient,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 325,S45,19.0,C,30127,Beta Analytic Inc.,24320 ±1080,24320.0,1080.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 326,S60,8.5,A,36773,Beta Analytic Inc.,4760 ±110,4760.0,110.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 327,S45,24.0,D,30128,Beta Analytic Inc.,29000 ±1380,29000.0,1380.0,dated,,16,22,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 328,S60,11.0,C,36774,Beta Analytic Inc.,5020 ± 90,5020.0,90.0,dated,,16,22,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 329,S61,1.5,A,37309,Beta Analytic Inc.,2990 ±80,2990.0,80.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 330,S76,8.0,B,45642,Beta Analytic Inc.,6680 ±100,6680.0,100.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 331,S61,6.0,B,37310,Beta Analytic Inc.,4220 ±100,4220.0,100.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 332,S77,5.5,A,46283,Beta Analytic Inc.,6430 ± 90,6430.0,90.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 333,S61,13.0,C,37311,Beta Analytic Inc.,3430 ±110,3430.0,110.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 334,S77,8.5,B,46284,Beta Analytic Inc.,6170± 110,6170.0,110.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 335,S61,16.5,D,37312,Beta Analytic Inc.,7310± 100,7310.0,100.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 336,S77,10.5,E,48367,Beta Analytic Inc.,>28000,28000.0,,lower_bound,28000.0,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 337,S62,6.0,A,38095,Beta Analytic Inc.,3660 ±70,3660.0,70.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 338,S77,11.5,C,46285,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 339,S62,13.0,B,38096,Beta Analytic Inc.,6220 ±100,6220.0,100.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 340,S77,17.0,D,46286,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 341,S62,17.5,C,38097,Beta Analytic Inc.,7160 ±70,7160.0,70.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 342,S78,4.5,A,46287,Beta Analytic Inc.,3250 ± 60,3250.0,60.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 343,S63,19.0,A,36775,Beta Analytic Inc.,6590 ±110,6590.0,110.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 344,S78,6.5,B,46288,Beta Analytic Inc.,6730 ±70,6730.0,70.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 345,S78,7.5,C,46289,Beta Analytic Inc.,15920 ±140,15920.0,140.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 346,S64,13.5,A,37313,Beta Analytic Inc.,2250 ±100,2250.0,100.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 347,S64,19.5,B,37314,Beta Analytic Inc.,3780 ±120,3780.0,120.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 348,S79,4.0,D,48368,Beta Analytic Inc.,3850 ±80,3850.0,80.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 349,S79,4.5,A,47331,Beta Analytic Inc.,4480 ± 70,4480.0,70.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 350,S79,5.0,B,47332,Beta Analytic Inc.,17900 ±220,17900.0,220.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 351,S66,6.5,A,45078,Beta Analytic Inc.,4020 ±100,4020.0,100.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 352,S79,6.5,C,47333,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 353,S66,9.0,B,45079,Beta Analytic Inc.,3950 ± 70,3950.0,70.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 354,S80,3.0,A,46290,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 355,S66,12.0,C,45080,Beta Analytic Inc.,5480 ±80,5480.0,80.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 356,S80,3.5,C,48369,Beta Analytic Inc.,3530 ± 6 0,3530.0,60.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 357,S66,14.5,D,45081,Beta Analytic Inc.,7230 ± 70,7230.0,70.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 358,S80,7.5,D,48370,Beta Analytic Inc.,23070 ±1880,23070.0,1880.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 359,S67,5.0,A,45633,Beta Analytic Inc.,11890 ±380,11890.0,380.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 360,S80,8.0,B,46291,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 361,S68,5.0,A,45082,Beta Analytic Inc.,2730 ± 80,2730.0,80.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 362,S81,1.5,A,48371,Beta Analytic Inc.,1350 ± 8 0,1350.0,80.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 363,S68,6.5,B,45083,Beta Analytic Inc.,4980 ± 70,4980.0,70.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 364,S81,2.5,D,48372,Beta Analytic Inc.,19630 ±140,19630.0,140.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 365,S68,13.5,C,45084,Beta Analytic Inc.,6830 ±80,6830.0,80.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 366,S81,3.0,B,47334,Beta Analytic Inc.,28200 ± 460,28200.0,460.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 367,S68,14.0,D,45085,Beta Analytic Inc.,7170 ±70,7170.0,70.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 368,S81,5.5,E,48373,Beta Analytic Inc.,29480 ± 330,29480.0,330.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 369,S81,11.0,F,48374,Beta Analytic Inc.,>38000,38000.0,,lower_bound,38000.0,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 370,S69,3.5,A,45634,Beta Analytic Inc.,4410±80,4410.0,80.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 371,S81,12.5,C,47335,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 372,S69,7.5,C,46282,Beta Analytic Inc.,23670 + 370,23670.0,,dated_unresolved_error,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 373,S69,12.5,B,45635,Beta Analytic Inc.,35260 ±610,35260.0,610.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 374,S82,3.0,C,48375,Beta Analytic Inc.,5050 ± 70,5050.0,70.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 375,S82,3.5,A,46292,Beta Analytic Inc.,5850 ±150,5850.0,150.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 376,S70,2.5,A,45086,Beta Analytic Inc.,3220+120,3220.0,,dated_unresolved_error,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 377,S82,4.0,D,48376,Beta Analytic Inc.,16540 ±220,16540.0,220.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 378,S70,4.0,B,45087,Beta Analytic Inc.,3690 ±140,3690.0,140.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 379,S82,4.5,B,46293,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 380,S71,2.0,C,48364,Beta Analytic Inc.,3030 ± 90,3030.0,90.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 381,S83,3.0,58280,,Not assigned,5410 ±120,5410.0,120.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 382,S71,5.5,A,45636,Beta Analytic Inc.,4660 ± 80,4660.0,80.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 383,S83,3.5,D,48379,Beta Analytic Inc.,8350 ±140,8350.0,140.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 384,S71,12.0,D,48365,Beta Analytic Inc.,6860 ± 50,6860.0,50.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 385,S83,4.0,A,47336,Beta Analytic Inc.,8860 ±130,8860.0,130.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 386,S71,12.5,B,45637,Beta Analytic Inc.,7250 ±100,7250.0,100.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 387,S83,4.5,B,48377,Beta Analytic Inc.,14990 ±100,14990.0,100.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 388,S72,4.5,A,46014,Beta Analytic Inc.,2900 ± 70,2900.0,70.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 389,S83,5.0,C,48378,Beta Analytic Inc.,24770 ± 240,24770.0,240.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 390,S72,8.5,B,46015,Beta Analytic Inc.,6420 ± 80,6420.0,80.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 391,S84,1.0,C,48380,Beta Analytic Inc.,2890 ±60,2890.0,60.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 392,S73,4.5,A,45638,Beta Analytic Inc.,3990 ±90,3990.0,90.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 393,S84,2.0,A,46294,Beta Analytic Inc.,16760 ±120,16760.0,120.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 394,S73,12.5,B,45639,Beta Analytic Inc.,7590 ±90,7590.0,90.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 395,S84,2.5,D,48381,Beta Analytic Inc.,23510 ±260,23510.0,260.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 396,S73,12.0,D,48366,Beta Analytic Inc.,12760 ±110,12760.0,110.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 397,S84,5.5,B,46295,Beta Analytic Inc.,39350 ± 800,39350.0,800.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 398,S73,14.5,C,45640,Beta Analytic Inc.,Insufficient C,,,insufficient,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 399,S85,2.5,B,48382,Beta Analytic Inc.,20330 ±270,20330.0,270.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 400,S74,3.5,A,45088,Beta Analytic Inc.,6290 ±140,6290.0,140.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 401,S85,6.5,A,46296,Beta Analytic Inc.,> 39730,39730.0,,lower_bound,39730.0,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 402,S74,8.5,B,45089,Beta Analytic Inc.,6420 ±90,6420.0,90.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 403,S86,1.5,A,51454,Beta Analytic Inc.,1690 ±80,1690.0,80.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 404,S75,2.5,A,46016,Beta Analytic Inc.,2900 ± 60,2900.0,60.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 405,S86,7.0,B,51455,Beta Analytic Inc.,4910 ±100,4910.0,100.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 406,S75,7.0,B,46017,Beta Analytic Inc.,5830 ±90,5830.0,90.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 407,S86,16.5,C,51456,Beta Analytic Inc.,6430 ±110,6430.0,110.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 408,S75,13.5,C,46018,Beta Analytic Inc.,6960 ±110,6960.0,110.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 409,S87,0.5,A,51457,Beta Analytic Inc.,1720 ± 8 0,1720.0,80.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 410,S76,5.0,A,45641,Beta Analytic Inc.,4950 ±130,4950.0,130.0,dated,,17,23,L,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 411,S87,9.0,B,51458,Beta Analytic Inc.,7030 ±130,7030.0,130.0,dated,,17,23,R,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download index,Core_ID,submitted_count,successful_numeric_or_lower_bound,dated_count,lower_bound_count,insufficient_count,shallowest_submitted_depth_m,shallowest_successful_depth_m,youngest_successful_age_BP,oldest_successful_age_BP,mean_1sigma_error,status,source_url 0,S1,6,6,6,0,0,2.0,2.0,2360.0,7590.0,125.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 1,S2,6,6,6,0,0,1.5,1.5,1830.0,14000.0,115.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 2,S3,6,6,6,0,0,3.0,3.0,3030.0,7510.0,98.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 3,S4,8,8,8,0,0,1.0,1.0,2150.0,7020.0,118.8,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 4,S5,8,8,8,0,0,2.0,2.0,1450.0,11290.0,113.8,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 5,S6,5,5,5,0,0,1.5,1.5,1910.0,24820.0,150.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 6,S7,19,16,16,0,3,1.5,1.5,2110.0,38220.0,290.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 7,S8,11,9,9,0,2,1.0,1.0,4025.0,9060.0,116.1,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 8,S9,3,2,2,0,1,2.0,2.0,3740.0,5140.0,115.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 9,S10,2,1,1,0,1,7.0,7.0,21880.0,21880.0,970.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 10,S11,6,6,6,0,0,2.0,2.0,2550.0,9820.0,160.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 11,S12,6,3,3,0,3,2.0,5.5,1500.0,7280.0,223.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 12,S13,5,5,5,0,0,5.0,5.0,3000.0,5130.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 13,S14,8,3,2,1,5,1.5,7.5,7440.0,26270.0,2110.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 14,S15,7,7,7,0,0,3.5,3.5,1620.0,7420.0,94.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 15,S16,6,6,6,0,0,3.0,3.0,1940.0,16345.0,92.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 16,S17,8,8,8,0,0,2.0,2.0,1420.0,8940.0,105.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 17,S18,8,8,8,0,0,1.5,1.5,1400.0,12070.0,126.2,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 18,S19,5,3,3,0,2,1.0,4.0,3070.0,4080.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 19,S20,8,8,8,0,0,2.0,2.0,2890.0,15110.0,165.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 20,S21,8,8,8,0,0,1.0,1.0,3400.0,8190.0,115.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 21,S22,8,8,8,0,0,0.5,0.5,3630.0,32920.0,505.7,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 22,S23,2,1,1,0,1,1.5,1.5,2490.0,2490.0,80.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 23,S24,3,3,3,0,0,0.5,0.5,4130.0,24240.0,600.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 24,S25,4,4,4,0,0,3.5,3.5,3860.0,6760.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 25,S26,5,4,4,0,1,1.0,1.0,2500.0,4370.0,137.5,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 26,S27,5,5,5,0,0,2.0,2.0,2520.0,6560.0,92.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 27,S28,6,4,4,0,2,5.0,5.0,4500.0,10950.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 28,S29,5,5,5,0,0,4.0,4.0,3460.0,8870.0,110.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 29,S30,6,5,5,0,1,18.5,18.5,5020.0,10770.0,138.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 30,S31,8,7,6,1,1,4.5,4.5,3260.0,7850.0,118.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 31,S32,4,3,3,0,1,7.5,7.5,5880.0,7960.0,150.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 32,S33,4,3,3,0,1,12.0,12.0,3560.0,34380.0,693.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 33,S34,4,4,4,0,0,13.0,13.0,6710.0,21050.0,532.5,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 34,S35,5,4,4,0,1,10.0,10.0,4770.0,7730.0,105.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 35,S36,4,3,3,0,1,14.0,14.0,7080.0,27720.0,503.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 36,S37,2,2,2,0,0,5.0,5.0,3260.0,6870.0,125.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 37,S38,7,5,4,1,2,12.0,12.0,3380.0,21090.0,255.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 38,S39,5,4,4,0,1,1.5,1.5,3840.0,21700.0,785.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 39,S40,6,5,5,0,1,3.0,3.0,3430.0,19350.0,294.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 40,S41,9,5,5,0,4,8.5,9.0,3060.0,6630.0,126.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 41,S42,7,7,7,0,0,4.0,4.0,3610.0,8290.0,114.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 42,S43,7,2,2,0,5,7.0,7.0,5610.0,6970.0,110.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 43,S44,6,5,5,0,1,2.0,2.0,2570.0,15600.0,142.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 44,S45,4,3,3,0,1,12.5,12.5,7100.0,29000.0,873.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 45,S46,4,3,3,0,1,8.0,8.0,6620.0,12940.0,130.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 46,S47,5,3,3,0,2,5.5,5.5,4270.0,26820.0,530.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 47,S48,4,4,4,0,0,3.0,3.0,1610.0,6340.0,72.5,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 48,S49,4,3,3,0,1,6.0,6.0,3190.0,7170.0,123.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 49,S50,4,4,4,0,0,4.5,4.5,2870.0,11040.0,145.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 50,S51,3,3,3,0,0,5.5,5.5,3800.0,6580.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 51,S52,5,5,5,0,0,2.0,2.0,1670.0,10510.0,88.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 52,S53,4,3,3,0,1,4.0,4.0,2470.0,11930.0,110.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 53,S54,4,4,4,0,0,5.0,5.0,3080.0,22820.0,265.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 54,S55,4,4,4,0,0,3.5,3.5,2420.0,14120.0,115.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 55,S56,1,1,1,0,0,8.5,8.5,1490.0,1490.0,80.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 56,S57,3,3,3,0,0,6.0,6.0,3630.0,13630.0,86.7,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 57,S58,4,4,4,0,0,3.0,3.0,3020.0,7500.0,77.5,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 58,S59,3,3,3,0,0,11.5,11.5,3140.0,9110.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 59,S60,2,2,2,0,0,8.5,8.5,4760.0,5020.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 60,S61,4,4,4,0,0,1.5,1.5,2990.0,7310.0,97.5,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 61,S62,3,3,3,0,0,6.0,6.0,3660.0,7160.0,80.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 62,S63,1,1,1,0,0,19.0,19.0,6590.0,6590.0,110.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 63,S64,2,2,2,0,0,13.5,13.5,2250.0,3780.0,110.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 64,S65,0,0,0,0,0,,,,,,No samples submitted,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 65,S66,4,4,4,0,0,6.5,6.5,3950.0,7230.0,80.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 66,S67,1,1,1,0,0,5.0,5.0,11890.0,11890.0,380.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 67,S68,4,4,4,0,0,5.0,5.0,2730.0,7170.0,75.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 68,S69,3,3,3,0,0,3.5,3.5,4410.0,35260.0,345.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 69,S70,2,2,2,0,0,2.5,2.5,3220.0,3690.0,140.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 70,S71,4,4,4,0,0,2.0,2.0,3030.0,7250.0,80.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 71,S72,2,2,2,0,0,4.5,4.5,2900.0,6420.0,75.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 72,S73,4,3,3,0,1,4.5,4.5,3990.0,12760.0,96.7,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 73,S74,2,2,2,0,0,3.5,3.5,6290.0,6420.0,115.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 74,S75,3,3,3,0,0,2.5,2.5,2900.0,6960.0,86.7,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 75,S76,2,2,2,0,0,5.0,5.0,4950.0,6680.0,115.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 76,S77,5,3,2,1,2,5.5,5.5,6170.0,6430.0,100.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 77,S78,3,3,3,0,0,4.5,4.5,3250.0,15920.0,90.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 78,S79,4,3,3,0,1,4.0,4.0,3850.0,17900.0,123.3,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 79,S80,4,2,2,0,2,3.0,3.5,3530.0,23070.0,970.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 80,S81,6,5,4,1,1,1.5,1.5,1350.0,29480.0,252.5,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 81,S82,4,3,3,0,1,3.0,3.0,5050.0,16540.0,146.7,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 82,S83,5,5,5,0,0,3.0,3.0,5410.0,24770.0,146.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 83,S84,4,4,4,0,0,1.0,1.0,2890.0,39350.0,310.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 84,S85,2,2,1,1,0,2.5,2.5,20330.0,20330.0,270.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 85,S86,3,3,3,0,0,1.5,1.5,1690.0,6430.0,96.7,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download 86,S87,2,2,2,0,0,0.5,0.5,1720.0,7030.0,105.0,Transcribed from Table 2,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download index,Check,Result,Interpretation 0,Literal Table 2 rows,412,"All sample determinations transcribed from publication Table 2, including insufficient-C rows." 1,Cores represented,86,S65 is the single core explicitly carrying no submitted samples. 2,Dated rows,351,Numeric finite age determinations. 3,Lower-bound rows,6,Open-ended >BP determinations. 4,Insufficient-C rows,55,Literal table transcription. 5,Successful numeric + lower-bound,357,'357 successful determinations from the printed table. 6,Catalogue prose summary,358 dates + 54 insufficient C,The catalogue text reports these totals. 7,Discrepancy,+1 successful / -1 insufficient in prose vs printed Table 2,The printed table instead yields 357 successful + 55 insufficient = 412. The workbook preserves the literal table and flags the mismatch; I cannot establish from the published material which count was intended. 8,Known visible example,S12 at 24.0 m = Insufficient C with no lab number,This row helps explain why automated count checks must use the printed table rather than the prose total. 9,Chronological caution,Uncorrected radiocarbon years BP,These are the catalogue's uncorrected ages; calibration and reservoir/context screening are required before age-depth modelling. index,record_type,archive_name,collection_year,core_inventory,core_length,diameter,subsurface_samples,samples_per_core,spatial_allocation,methods_or_time_bins,archive_gap_or_caution,source_url 0,Archive/suite,Randazzo Manzala short-core survey,1990,30 short percussion PVC cores at 30 of 83 grab-sample sites,18–98 cm,8 cm,117 subsurface samples,2–6 samples/core,Damietta–NW: 10 cores; El-Gamil north-central: 9; El-Mataria–SE: 11,X-radiographs before/after splitting; photographs; detailed visual logs; samples at grain-size/colour changes,"The 1998 paper explicitly states that the detailed individual core logs and sampled-section positions are in Randazzo (1992), not reproduced in the article.",https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download 1,Age model used in 1998 synthesis,Suite-wide extrapolation,1990,"Uses ~1.2 cm/yr modern accumulation estimate, not individual core-specific chronologies",,,,,,Approximate bins: surface=1990; 0–30 cm base≈1965; 30–55 cm base≈1940s; 55–80 cm base≈1920s,"These are working temporal bins for spatial comparison, not independently dated ages for each of the 30 cores.",https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download 2,,,,,,,,,,,, 3,,,,,,,,,,,, 4,Known_ID,lake,sample_type,collection_year,length_or_resolution,source_context,crosswalk_status,source_url,,,, 5,Man-IV,Manzala,short core,September 1989,~1 m in MEDIBA figure/caption context,MEDIBA monograph figure; may predate 1990 Randazzo suite,Crosswalk to Randazzo 30-core identifiers unresolved,https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download,,,, 6,Man-XIV,Manzala,short core,1990,~1.00 m; 18 analytical intervals,"Reinhardt, Stanley & Schwarcz isotope study",Likely part of Smithsonian short-core archive; exact Randazzo crosswalk unresolved,https://repository.si.edu/server/api/core/bitstreams/bb903c5a-8de2-46ad-aaed-edafd7f23f76/content,,,, 7,Man-XX,Manzala,short core,1990,0.94 m,"Benninger, Suayah & Stanley modern radionuclide study",Likely part of Smithsonian short-core archive; exact Randazzo crosswalk unresolved,https://repository.si.edu/server/api/core/bitstreams/9f8c9bd0-4b55-434a-9a24-4c6cc1dcc8cc/content,,,, 8,Man-XXV,Manzala,short core,1990,0.51 m; 18 analytical intervals,"Reinhardt, Stanley & Schwarcz isotope study",Likely part of Smithsonian short-core archive; exact Randazzo crosswalk unresolved,https://repository.si.edu/server/api/core/bitstreams/bb903c5a-8de2-46ad-aaed-edafd7f23f76/content,,,, 9,MZ-XIII,Manzala,illustrated short core / X-radiograph,1989–1990,,Bernasconi & Stanley molluscan study,Identifier system differs from Man-* notation; equivalence not established,https://www.jstor.org/stable/4298226,,,, 10,MZ-XXI,Manzala,illustrated short core / X-radiograph,1989–1990,,Bernasconi & Stanley molluscan study,Identifier system differs from Man-* notation; equivalence not established,https://www.jstor.org/stable/4298226,,,, 11,MZ-XXXI,Manzala,illustrated short core / X-radiograph,1989–1990,,Bernasconi & Stanley molluscan study,Identifier system differs from Man-* notation; equivalence not established,https://www.jstor.org/stable/4298226,,,, 12,,,,,,,,,,,, 13,Lithotype,dominant_sediment,typical_core_position,diagnostic_features,source_url,,,,,,, 14,A,Medium/fine sand to silty sand,Usually upper core; finer downward,Abundant mollusc shells and roots; lower laminae where shells decline,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,,, 15,B,Silt or sandy silt,Usually upper core,Bivalve fragments and gastropods commonly concentrated in layers,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,,, 16,C,Shelly soft muddy silt,Middle to lower core,Shells dispersed or layered,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,,, 17,D,Soft micaceous mud,Variable,Roots common; organic matter occurs as pockets/layers,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,,, 18,E,Medium-grained sand,Variable,Few mollusc shells,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,,, 19,F,Compact clay,Variable,Light-brown compact clay,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,,, 20,G,Gypsiferous silt,Variable,Gypsum-crystal layers in a silt matrix,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,,, 21,,,,,,,,,,,, 22,,,,,,,,,,,, 23,Microfacies,name,spatial_setting,recoverable_quantitative_summary,occurrence,source_url,,,,,, 24,I,Terrigenous well-sorted sand,NW sector / Damietta promontory and coastal-ridge margin,Sand up to 99%; light minerals 76–89% (mean 83%); heavy minerals 6–20% (mean 12%); biogenic components ~2%,Modern surface + subsurface,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,, 25,II,Micaceous muddy sand,Narrow zone landward of facies I,Silt 31–77% (mean 53%); sand 1–22% (mean 13%); light minerals 46–68% (mean 55%); mica 1–15% (mean 7%); plant fragments 2–10% (mean 6%); shell fragments 1–29% (mean 10%),Modern surface + subsurface,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,, 26,III/1,Shelly silty mud — freshwater subfacies,South of Damietta,"Biogenic component may reach ~66%; ostracods 12–52% (mean 32%); shell fragments 1–44% (mean 16%); foraminifera 2–28% (mean 13%); light minerals 13–43% (mean ~24%). Texture values in accessible OCR are incomplete, so not numerically reconstructed here.",Modern surface + subsurface,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,, 27,III/2,Shelly silty mud — central subfacies,Central lagoon; largest area,Sand 44–77% (mean 59%); silt 15–32% (mean 23%); biogenic ~54%; terrigenous ~42%; shell fragments 14–58% (mean 27%); light minerals 18–58% (mean 36%),Modern surface + subsurface,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,, 28,III/3,Shelly silty mud — SE subfacies,East and SE of El-Mataria,Sand 32–85% (mean 50%); silt 6–64% (mean 34%); terrigenous ~63%; biogenic ~39%; light minerals 27–73% (mean 52%); heavy minerals 1–12% (mean 5%); ostracods 3–36% (mean 11%),Modern surface + subsurface,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,, 29,IV,Plant-rich silty clayey mud,Southern margin near major drains; local interior patches,Silt 13–86% (mean 52%); clay 0–64% (mean 17%); sand 5–85% (mean 24%); ostracods 6–88% (mean 29%); plant fragments 0–19% (mean 6%); diatoms 0–6% (mean 1%); shells 4–42% (mean 17%),1990 surface; not recorded in subsurface cores in the paper,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,, 30,V,"Mica-, foraminifera- and plant-rich silty mud",Subsurface only,Clay 18–69% (mean 45%); silt 3–71% (mean 43%); sand 1–40% (mean 12%); mica 0–6% (mean 1.2%); foraminifera 8–66% (mean 40%); ostracods 1–34% (mean 12%); plant fragments 0–3% (mean 0.3%),Subsurface only,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,,,,,, index,Site_or_Core_ID,waterbody,sample_type,collection_year,position_description,chronology,analysis,RoC_interpretation,source_url 0,BU1,Burullus,surface sediment,1989–1990,Near the Mediterranean outlet,Undated surface snapshot,Molluscan assemblage abundance/dominance; herbivores prominent,NOT a short core; spatial baseline only,https://www.jstor.org/stable/4298226 1,BU2,Burullus,surface sediment,1989–1990,Western/open-water Burullus sector; exact distance assignment unresolved in accessible text,Undated surface snapshot,Molluscan assemblage abundance/dominance; herbivores prominent,NOT a short core; spatial baseline only,https://www.jstor.org/stable/4298226 2,BU3,Burullus,surface sediment,1989–1990,Southwestern marsh/freshwater setting,Undated surface snapshot,Molluscan assemblage; entirely freshwater assemblage in paper,NOT a short core; spatial baseline only,https://www.jstor.org/stable/4298226 3,BU4,Burullus,surface sediment,1989–1990,Western/open-water Burullus sector; exact distance assignment unresolved in accessible text,Undated surface snapshot,Molluscan assemblage; endofaunal component emphasized,NOT a short core; spatial baseline only,https://www.jstor.org/stable/4298226 4,MR1,Mariut,surface sediment,1989–1990,Southwestern salt-basin sector close to Desert Road,Undated surface snapshot,Molluscan assemblage,NOT a short core; spatial baseline only,https://www.jstor.org/stable/4298226 5,MR2,Mariut,surface sediment,1989–1990,Open-water subbasin SSE of El-Mex pumping station,Undated surface snapshot,Molluscan assemblage,Freshwater influence increases generally from MR2 toward MR6,https://www.jstor.org/stable/4298226 6,MR3,Mariut,surface sediment,1989–1990,Open-water subbasin SSE of El-Mex pumping station,Undated surface snapshot,Molluscan assemblage,Freshwater influence gradient toward NE/El-Umoum drain,https://www.jstor.org/stable/4298226 7,MR4,Mariut,surface sediment,1989–1990,Open-water subbasin SSE of El-Mex pumping station,Undated surface snapshot,Molluscan assemblage,Freshwater influence gradient toward NE/El-Umoum drain,https://www.jstor.org/stable/4298226 8,MR5,Mariut,surface sediment,1989–1990,Open-water subbasin SSE of El-Mex pumping station,Undated surface snapshot,Molluscan assemblage,Freshwater influence gradient toward NE/El-Umoum drain,https://www.jstor.org/stable/4298226 9,MR6,Mariut,surface sediment,1989–1990,Open-water subbasin; most NE/freshwater-influenced end of MR2–MR6 gradient,Undated surface snapshot,Molluscan assemblage,NOT a short core; spatial baseline only,https://www.jstor.org/stable/4298226 10,AQ1,Former Abu Qir lagoon,short core,1992,Former Abu Qir lagoon,Up to ~70 cm; no target-lake modern chronology in this paper,Molluscan assemblages,"Short core, but not Burullus/Mariut/Manzala",https://www.jstor.org/stable/4298226 11,AQ2,Former Abu Qir lagoon,short core,1992,Former Abu Qir lagoon,Up to ~70 cm; no target-lake modern chronology in this paper,Molluscan assemblages,"Short core, but not Burullus/Mariut/Manzala",https://www.jstor.org/stable/4298226 12,AQ3,Former Abu Qir lagoon,short core,1992,Former Abu Qir lagoon,Up to ~70 cm; no target-lake modern chronology in this paper,Molluscan assemblages,"Short core, but not Burullus/Mariut/Manzala",https://www.jstor.org/stable/4298226 13,AQ4,Former Abu Qir lagoon,short core,1992,Former Abu Qir lagoon,Up to ~70 cm; no target-lake modern chronology in this paper,Molluscan assemblages,"Short core, but not Burullus/Mariut/Manzala",https://www.jstor.org/stable/4298226 14,S-62,NW Nile Delta,MEDIBA long core residue,pre-1994,NW Delta,Holocene long-core framework,Coarse-fraction molluscan residues,Not a lagoon short core,https://www.jstor.org/stable/4298226 15,S-72,NW Nile Delta/Mariut sector,MEDIBA long core residue,pre-1994,NW Delta near Mariut sector,Holocene long-core framework,Coarse-fraction molluscan residues,Contextual only,https://www.jstor.org/stable/4298226 16,S-74,NW Nile Delta/Mariut sector,MEDIBA long core residue,pre-1994,NW Delta near Mariut sector,Holocene long-core framework,Coarse-fraction molluscan residues,Contextual only,https://www.jstor.org/stable/4298226 17,MZ-XIII,Manzala,illustrated short core / X-radiograph,1989–1990,Manzala,No independent chronology supplied in Bernasconi & Stanley,Sedimentary structure + molluscan context,Potential crosswalk to Randazzo archive; identifier equivalence unresolved,https://www.jstor.org/stable/4298226 18,MZ-XXI,Manzala,illustrated short core / X-radiograph,1989–1990,Manzala,No independent chronology supplied in Bernasconi & Stanley,Sedimentary structure + molluscan context,Potential crosswalk to Randazzo archive; identifier equivalence unresolved,https://www.jstor.org/stable/4298226 19,MZ-XXXI,Manzala,illustrated short core / X-radiograph,1989–1990,Manzala,No independent chronology supplied in Bernasconi & Stanley,Sedimentary structure + molluscan context,Potential crosswalk to Randazzo archive; identifier equivalence unresolved,https://www.jstor.org/stable/4298226 index,Site_or_Core_ID,lake,sample_type,depth_interval,location_or_context,sample_count,analyses,chronology,extraction_status,source_url 0,Study suite,Mariut,surficial + short-core samples,,,82 total samples,Grain-size and sand-size petrographic composition; lithofacies/statistical analysis,No modern radiometric chronology identified in accessible indexed text,Full site/core identifier table is not exposed by accessible index text; article PDF is required for exact reconstruction.,https://www.jstor.org/stable/4298225 1,Core I,Mariut,short core,24–26 cm,Depth interval explicitly indexed in figure/caption,,Charophyte oogonia/biogenic components illustrated; lithofacies/petrographic variables analyzed,No independent calendar age recovered,"Verified core identifier and depth interval only; total core length, coordinates, and full sample-depth list remain unresolved.",https://www.jstor.org/stable/4298225 index,lake,snapshot_type,source_dataset_or_map,snapshot_year,geometry_or_feature,scale_or_resolution,CRS,published_area_km2,geometry_availability,uncertainty_or_use_note,source_url 0,All target lakes,Modern reference,HydroLAKES v1.0,~2016 compilation,polygon shoreline,global lake polygons,geographic lat/lon,,Downloadable GIS geometry,"CC BY 4.0; suitable as consistent modern reference, but not necessarily the best date-specific shoreline for rapidly changing delta lakes",https://www.hydrosheds.org/products/hydrolakes 1,All target lakes,Modern reference,Egypt Lakes (HydroSHEDS) 2016 — UN Geoportal,portal item current 2026; description states boundaries observed in 2023,polygon shoreline,Egypt national subset,,,Downloadable/hosted GIS item,Use as a second contemporary boundary source; verify item geometry date before quantitative area-change calculation,https://geoportal.un.org/arcgis/home/item.html?id=049cdbfccb604a7f898965d5933c68cf 2,All target lakes,Modern/historical benchmark,"CAPMAS Lake and Sea Boundaries, Egypt",2006,polygon shoreline,national Egypt lake/sea boundaries,WGS84,,Polygon shapefile metadata available; access may require repository workflow,Valuable common 2006 benchmark for all three lakes,https://earthworks.stanford.edu/catalog/stanford-mx699xz9947 3,Manzala,Historical map,Survey of Egypt Sheet 17 — Lake Manzala West,1912,map shoreline,"1:50,000",,,High-resolution raster map available; vectorisation required,Georeference and digitise water/marsh boundary with uncertainty buffer,https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~317289~90086578%3ASheet-17-Lake-Manzala-West 4,Manzala,Historical map,Survey of Egypt Sheet 18 — Lake Manzala East,1914,map shoreline,"1:50,000",,,High-resolution raster map available; vectorisation required,Mosaic with Sheet 17 and adjacent Port Said/Manzala sheets,https://www.davidrumsey.com/luna/servlet/view/all/who/Egypt.%2BWizarat%2Bal-Maliyah/Government%2BPress/?sort=Pub_List_No_InitialSort%2CPub_Date%2CPub_List_No 5,Burullus,Historical map,Survey of Egypt Sheet 3 — Lake Borollos East,1909,map shoreline,"1:50,000",,,Historical atlas map available; vectorisation required,Pair with western sheet for early-20th-century polygon,https://www.davidrumsey.com/luna/servlet/view/all/what/Atlas%2BMap/Ottoman%2BMapping/where/Egypt 6,Burullus,Historical map,Survey of Egypt Sheet 2 — Lake Burullus West,1918,map shoreline,"1:50,000",,,High-resolution raster map available; vectorisation required,Pair with eastern 1909 sheet; mosaic-year mismatch must be carried as uncertainty,https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~317275~90086565%3ASheet-2-Lake-Burullus-West 7,Mariut,Historical polygon source,French Campaign Carte d’Alexandrie,1801 (pre-flood limit; map also shows flood limit),digitised historical lake extent,"1:100,000",,890.0,Digitised by Awad/CEAlex; vector geometry not openly exposed in accessible source,Area ~890 km² for pre-flood state; map also records 1801 flood expansion,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 8,Mariut,Historical polygon source,"Mahmoud Bey El-Falaki, Carte des Environs d’Alexandrie",1866,digitised historical lake extent,"1:200,000",,450.0,Digitised by Awad/CEAlex; vector geometry not openly exposed,~50% of 1801 area,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 9,Mariut,Historical polygon source,Survey of Egypt,1911/1914,digitised historical lake extent,"1:50,000",,340.0,Digitised by Awad/CEAlex; vector geometry not openly exposed,Eight map sheets used in original reconstruction,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 10,Mariut,Historical polygon source,Survey of Egypt,1930,digitised historical lake extent,"1:100,000",,,Digitised by Awad/CEAlex; vector geometry not openly exposed,Salt marsh first appears prominently; area continued to decline,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 11,Mariut,Historical polygon source,Survey of Egypt,1949,digitised historical lake extent,"1:100,000",,210.0,Digitised by Awad/CEAlex; vector geometry not openly exposed,"~51,000 feddans; about one-quarter of 1801 area",https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 12,Mariut,Historical polygon source,Egyptian General Survey Authority,1970s,digitised historical lake extent,"1:25,000",,,Digitised by Awad/CEAlex; vector geometry not openly exposed,High-resolution contour/map series; major canal/drain development,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 13,Mariut,Historical polygon source,Egyptian General Survey Authority,1991,digitised historical lake extent,"1:50,000",,,Digitised by Awad/CEAlex; vector geometry not openly exposed,Six sheets used by Awad,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 14,Mariut,Satellite-derived polygon source,Landsat,2001,digitised lake/marsh/fish-farm extent,15 m/pixel,,210.0,Digitised by Awad/CEAlex; source imagery reproducible independently,"Lake reported ~210 km²; length ~66 km, width ~11 km",https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps index,lake,point_layer,polygon_layer,intended_overlay_metric,execution_status,scientific_caution,source_url 0,Manzala,MEDIBA/short-core points,1912 west + 1914 east Survey of Egypt mosaic,Historical point-in-polygon / distance-to-shore,Pending vectorisation,Do not classify cores as 'inside historical lake' until map sheets are georeferenced and digitised,https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~317289~90086578%3ASheet-17-Lake-Manzala-West 1,Manzala,MEDIBA/short-core points,HydroLAKES / UN Egypt lakes / CAPMAS 2006,Modern point-in-polygon / distance-to-shore,Modern polygon source identified; geometry not cached locally,Use WGS84 point coordinates; calculate distance to modern water edge and historical 1912/1914 edge,https://www.hydrosheds.org/products/hydrolakes 2,Burullus,MEDIBA/short-core points,1909 east + 1918 west Survey of Egypt mosaic,Historical point-in-polygon / distance-to-shore,Pending vectorisation,Treat 9-year difference between sheets as explicit temporal uncertainty,https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~317275~90086565%3ASheet-2-Lake-Burullus-West 3,Burullus,MEDIBA/short-core points,HydroLAKES / UN Egypt lakes / CAPMAS 2006,Modern point-in-polygon / distance-to-shore,Modern polygon source identified; geometry not cached locally,Use for modern lake relation and shoreline migration metrics,https://www.hydrosheds.org/products/hydrolakes 4,Mariut,MEDIBA/short-core points,"Awad 1801, 1866, 1911, 1930, 1949, 1970s, 1991, 2001 series",Multi-date point-in-polygon / distance-to-shore,"Published digitised polygons exist, but vector files not exposed in accessible source",Request CEAlex/Awad vector data or re-digitise cited maps before formal overlay,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 5,Mariut,MEDIBA/short-core points,HydroLAKES / UN Egypt lakes / CAPMAS 2006,Modern point-in-polygon / distance-to-shore,Modern polygon source identified; geometry not cached locally,Modern shoreline highly engineered; document basin partitions and pumping infrastructure separately,https://www.hydrosheds.org/products/hydrolakes index,source_or_archive,lake,missing_item,why_not_extracted_here,recovery_route,priority,source_url 0,Randazzo (1992) thesis,Manzala,"Full 30 individual core IDs, exact coordinates, detailed logs, and sampled-section depths",Not present in the 1998 article; article explicitly points to 1992 thesis for detailed logs,Università di Messina thesis/library or Smithsonian field/lab archive,High — required to claim a complete 30-core reconstruction,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download 1,Loizeau & Stanley (1994) full article/site table,Mariut,"All short-core IDs, coordinates, lengths, and depth-by-sample table","Accessible index confirms 82 surficial+core samples and Core I 24–26 cm, but full site table is not exposed",JSTOR/library PDF or author/Smithsonian archive,High — Mariut remains the main sedimentary archive gap,https://www.jstor.org/stable/4298225 2,Bernasconi & Stanley (1994) station coordinates,Burullus/Mariut,Exact coordinates for BU1–BU4 and MR1–MR6,Identifiers and relative positions are recoverable; exact coordinate table is not available in accessible indexed text used here,Full JCR PDF / original station map,"Medium — useful for spatial baseline, not temporal RoC",https://www.jstor.org/stable/4298226 3,Historical polygon vectors,All,Actual GIS polygon geometries for historical snapshots,"Historical maps/digitised reconstructions are identified, but vector geometries are not openly exposed in the accessible sources",Georeference/digitise map sheets or request CEAlex/Awad vectors,High for formal point-in-polygon and shoreline-migration metrics,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps 4,Modern polygon geometry cached locally,All,HydroLAKES/UN/CAPMAS polygon files,Authoritative/open polygon sources identified; network sandbox did not provide a local geometry file during this run,Download in QGIS/ArcGIS from indexed source and join to Map_Data points,Low–medium; easy to complete outside this restricted runtime,https://www.hydrosheds.org/products/hydrolakes 5,Mariut modern palaeoecological cores,Mariut,Potential 3-/5-core diatom archives not part of 1994 extraction,Later literature reports high-value Mariut diatom core datasets,Add Zalat modern/historical Mariut cores as a separate v4 extraction,High scientific value beyond the requested 1994 archive,https://www.sciencedirect.com/science/article/abs/pii/S0277379124004809 index,Source,URL,Use in v3 0,"Stanley, McRea & Waldron 1996 MEDIBA catalogue",https://repository.si.edu/bitstreams/f26cc498-1b6f-4b31-a431-88441cd021d0/download,Full printed Table 2; long-core metadata and archive context 1,Randazzo et al. 1998 / Randazzo 1992 archive pointer,https://repository.si.edu/bitstreams/ab4256f3-8633-4769-885a-9d07027ac25c/download,"30 Manzala short-core suite methods, sector counts, temporal bins, lithotypes A–G and microfacies; article points to 1992 thesis for full logs" 2,Bernasconi & Stanley 1994,https://www.jstor.org/stable/4298226,BU1–BU4 and MR1–MR6 surface sites; AQ1–AQ4 Abu Qir short cores; Manzala illustrated core identifiers; molluscan biofacies 3,Loizeau & Stanley 1994,https://www.jstor.org/stable/4298225,Mariut 82-sample surficial/core study; indexed Core I 24–26 cm; full site table still requires article PDF 4,HydroLAKES,https://www.hydrosheds.org/products/hydrolakes,Open modern lake shoreline polygon source; CC BY 4.0 5,UN Geoportal Egypt Lakes,https://geoportal.un.org/arcgis/home/item.html?id=049cdbfccb604a7f898965d5933c68cf,Egypt lake polygon layer reference 6,CAPMAS/Stanford EarthWorks 2006,https://earthworks.stanford.edu/catalog/stanford-mx699xz9947,National 2006 lake/sea boundary polygon benchmark 7,Awad 2010 Maryut maps,https://www.academia.edu/101039805/A_Study_of_the_Evolution_of_the_Maryut_Lake_through_Maps,Georeferenced/digitised Maryut historical map series and published areas 1801–2001 8,David Rumsey — Burullus West,https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~317275~90086565%3ASheet-2-Lake-Burullus-West,"1918 Survey of Egypt 1:50,000 historical map" 9,David Rumsey — Manzala West,https://www.davidrumsey.com/luna/servlet/detail/RUMSEY~8~1~317289~90086578%3ASheet-17-Lake-Manzala-West,"1912 Survey of Egypt 1:50,000 historical map" 10,David Rumsey — Manzala East listing,https://www.davidrumsey.com/luna/servlet/view/all/who/Egypt.%2BWizarat%2Bal-Maliyah/Government%2BPress/?sort=Pub_List_No_InitialSort%2CPub_Date%2CPub_List_No,"1914 Survey of Egypt 1:50,000 historical map" index,Egypt coastal-lake archival reconstruction — v3,Unnamed: 1 0,Version,v3 archival extraction / GIS source reconstruction 1,MEDIBA 14C,All 412 printed Table 2 determinations have been transcribed. Printed-table totals are 357 successful numeric/lower-bound determinations + 55 insufficient-C rows; this differs from the catalogue prose statement of 358 + 54. Both are documented rather than silently reconciled. 2,Randazzo,"The 1998 paper allows a robust suite-level reconstruction (30 cores, 117 subsurface samples, sector allocation, methods, lithotypes, microfacies and approximate temporal bins). It does not reproduce all 30 logs; it explicitly directs readers to Randazzo (1992). Therefore a 'full 30 individual core log table' cannot be honestly reconstructed without that thesis/archive." 3,Bernasconi correction,"BU1–BU4 and MR1–MR6 are surface sediment stations, not Burullus/Mariut short cores. AQ1–AQ4 are the short cores and they are from former Abu Qir lagoon. This prevents a serious sample-type error in RoC design." 4,Loizeau,"Accessible indexing verifies an 82-sample Mariut surficial/core study and Core I at 24–26 cm, but does not expose the complete core/site table. Unresolved fields are left blank/flagged, not invented." 5,GIS,Modern polygon sources and historical map/polygon sources are indexed. Actual point-in-polygon overlay is deliberately marked pending where polygon geometry was not locally retrievable. Historical vector geometries must be obtained/digitised before formal shoreline-distance calculations. 6,RoC implication,"The Table 2 14C archive strengthens Holocene context, while Randazzo/Bernasconi/Loizeau primarily identify modern archive material. A reproducible 100-year RoC analysis still requires core-specific modern chronologies; do not infer calendar ages from the 14C long-core framework."