{ "paleoData": [ { "measurementTable": [ { "googleWorkSheetKey": "o92vqwq", "tableName": "paleo1measurement1", "missingValue": "NaN", "d18O": { "chronologyIntegrationTime": "2", "chronologyIntegrationTimeBasis": "Sr/Ca data to monthly SST from the 2i¿½ i¿½ 2i¿½ grid square centered on 4i¿½N, 172i¿½E from the extended reconstructed SST version 3b (ERSSTv3b) data product [Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the coolest points in the SST record using Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data remained relatively constant throughout the record, and the chronology was verified against growth band counts from the X-radiograph. 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The resulting spacing of Sr/Ca data remained relatively constant throughout the record, and the chronology was verified against growth band counts from the X-radiograph. 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After converting depth to time in Analyseries, Sr/Ca were interpolated to six equally spaced samples per year using ARAND time series analysis software [Howell, 2001], corresponding to bimonthly resolution for the length of the record.' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_integrationTimeUnits: 'months' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_mathematicalRelation: 'linear' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_rank: '1' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_scope: 'isotope' has been replaced by 'climate'"], ["d18O (CO14CABT01B): interpretation2_seasonality: 'subannual' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_variable: 'seawaterIsotope' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_variableGroupDirection: 'negative' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation2_variableGroupOriginal: 'd18O_seawater' has been replaced by ''"], ["d18O (CO14CABT01B): interpretation3_scope: '' has been replaced by 'climate'"], ["d18O (CO14CABT01B): interpretation4_direction: '' has been replaced by 'positive'"], ["d18O (CO14CABT01B): interpretation4_inferredMaterial: '' has been replaced by 'seawater'"], ["d18O (CO14CABT01B): interpretation4_integrationTime: '' has been replaced by '2'"], ["d18O (CO14CABT01B): interpretation4_integrationTimeBasis: '' has been replaced by 'Sr/Ca data to monthly SST from the 2� � 2� grid square centered on 4�N, 172�E from the extended reconstructed SST version 3b (ERSSTv3b) data product [Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the coolest points in the SST record using Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data remained relatively constant throughout the record, and the chronology was verified against growth band counts from the X-radiograph. After converting depth to time in Analyseries, Sr/Ca were interpolated to six equally spaced samples per year using ARAND time series analysis software [Howell, 2001], corresponding to bimonthly resolution for the length of the record.'"], ["d18O (CO14CABT01B): interpretation4_integrationTimeUnits: '' has been replaced by 'months'"], ["d18O (CO14CABT01B): interpretation4_mathematicalRelation: '' has been replaced by 'linear'"], ["d18O (CO14CABT01B): interpretation4_rank: '' has been replaced by '1'"], ["d18O (CO14CABT01B): interpretation4_scope: '' has been replaced by 'isotope'"], ["d18O (CO14CABT01B): interpretation4_seasonality: '' has been replaced by 'subannual'"], ["d18O (CO14CABT01B): interpretation4_variable: '' has been replaced by 'seawaterIsotope'"], ["d18O (CO14CABT01B): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'"], ["d18O (CO14CABT01B): interpretation4_variableGroupDirection: '' has been replaced by 'negative'"], ["d18O (CO14CABT01B): interpretation4_variableGroupOriginal: '' has been replaced by 'd18O_seawater'"], ["d18O (CO14CABT01B): interpretation5_scope: '' has been replaced by 'isotope'"], ["d18O (CO14CABT01B): interpretation6_scope: '' has been replaced by 'isotope'"], ["d18O (CO14CABT01B2): interpretation2_direction: 'positive' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_inferredMaterial: 'seawater' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_integrationTime: '2' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_integrationTimeBasis: 'Sr/Ca data to monthly SST from the 2� � 2� grid square centered on 4�N, 172�E from the extended reconstructed SST version 3b (ERSSTv3b) data product [Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the coolest points in the SST record using Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data remained relatively constant throughout the record, and the chronology was verified against growth band counts from the X-radiograph. After converting depth to time in Analyseries, Sr/Ca were interpolated to six equally spaced samples per year using ARAND time series analysis software [Howell, 2001], corresponding to bimonthly resolution for the length of the record.' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_integrationTimeUnits: 'months' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_mathematicalRelation: 'linear' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_rank: '1' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_scope: 'isotope' has been replaced by 'climate'"], ["d18O (CO14CABT01B2): interpretation2_seasonality: 'subannual' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_variable: 'seawaterIsotope' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_variableGroupDirection: 'negative' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation2_variableGroupOriginal: 'd18O_seawater' has been replaced by ''"], ["d18O (CO14CABT01B2): interpretation3_scope: '' has been replaced by 'climate'"], ["d18O (CO14CABT01B2): interpretation4_direction: '' has been replaced by 'positive'"], ["d18O (CO14CABT01B2): interpretation4_inferredMaterial: '' has been replaced by 'seawater'"], ["d18O (CO14CABT01B2): interpretation4_integrationTime: '' has been replaced by '2'"], ["d18O (CO14CABT01B2): interpretation4_integrationTimeBasis: '' has been replaced by 'Sr/Ca data to monthly SST from the 2� � 2� grid square centered on 4�N, 172�E from the extended reconstructed SST version 3b (ERSSTv3b) data product [Smith et al., 2008; ttp://www.esrl.noaa.gov/psd] [?] Annual Sr/Ca maxima were tied to the coolest points in the SST record using Analyseries [Paillard et al., 1996]. The resulting spacing of Sr/Ca data remained relatively constant throughout the record, and the chronology was verified against growth band counts from the X-radiograph. After converting depth to time in Analyseries, Sr/Ca were interpolated to six equally spaced samples per year using ARAND time series analysis software [Howell, 2001], corresponding to bimonthly resolution for the length of the record.'"], ["d18O (CO14CABT01B2): interpretation4_integrationTimeUnits: '' has been replaced by 'months'"], ["d18O (CO14CABT01B2): interpretation4_mathematicalRelation: '' has been replaced by 'linear'"], ["d18O (CO14CABT01B2): interpretation4_rank: '' has been replaced by '1'"], ["d18O (CO14CABT01B2): interpretation4_scope: '' has been replaced by 'isotope'"], ["d18O (CO14CABT01B2): interpretation4_seasonality: '' has been replaced by 'subannual'"], ["d18O (CO14CABT01B2): interpretation4_variable: '' has been replaced by 'seawaterIsotope'"], ["d18O (CO14CABT01B2): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'"], ["d18O (CO14CABT01B2): interpretation4_variableGroupDirection: '' has been replaced by 'negative'"], ["d18O (CO14CABT01B2): interpretation4_variableGroupOriginal: '' has been replaced by 'd18O_seawater'"], ["d18O (CO14CABT01B2): interpretation5_scope: '' has been replaced by 'isotope'"], ["d18O (CO14CABT01B2): interpretation6_scope: '' has been replaced by 'isotope'"], ["depth (MAT4739320cb9): interpretation1_scope: '' has been replaced by 'climate'"], ["depth (MAT4739320cb9): interpretation2_scope: '' has been replaced by 'climate'"], ["year (MAT65e08c7772): interpretation1_scope: '' has been replaced by 'climate'"], ["year (MAT65e08c7772): interpretation2_scope: '' has been replaced by 'climate'"] ] } }, { "version": "1.0.3", "lastVersion": "1.0.2", "curator": "nicholas", "timestamp": "2025-04-09 21:04:55.869309 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Paleo Interpretation metadata": [ ["d18O (CO14CABT01A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'"], ["d18O (CO14CABT01A): interpretation2_variable: 'T_water' has been replaced by 'temperature'"], ["d18O (CO14CABT01A): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"], ["d18O (CO14CABT01B): interpretation1_variable: 'S' has been replaced by 'salinity'"], ["d18O (CO14CABT01B): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"], ["d18O (CO14CABT01B2): interpretation1_variable: 'S' has been replaced by 'salinity'"], ["d18O (CO14CABT01B2): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"] ] } }, { "version": "1.0.2", "lastVersion": "1.0.1", "curator": "nicholas", "timestamp": "2025-04-09 17:37:33.960296 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Interpretation metadata": [ ["d18O (CO14CABT01A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'"], ["d18O (CO14CABT01A): interpretation2_variable: 'T_water' has been replaced by 'temperature'"], ["d18O (CO14CABT01A): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"], ["d18O (CO14CABT01B): interpretation1_variable: 'S' has been replaced by 'salinity'"], ["d18O (CO14CABT01B): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"], ["d18O (CO14CABT01B2): interpretation1_variable: 'S' has been replaced by 'salinity'"], ["d18O (CO14CABT01B2): interpretation2_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nicholas", "timestamp": "2025-04-08 17:30:25.454229 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Column metadata": [ ["d18O (CO14CABT01A): paleoData_longName: '' has been replaced by 'AD'"], ["d18O (CO14CABT01B): paleoData_longName: '' has been replaced by 'AD'"], ["d18O (CO14CABT01B2): paleoData_longName: '' has been replaced by 'AD'"], ["depth (MAT4739320cb9): paleoData_longName: '' has been replaced by 'AD'"], ["year (MAT65e08c7772): paleoData_units: 'AD' has been replaced by 'yr AD'"], ["year (MAT65e08c7772): paleoData_longName: '' has been replaced by 'AD'"] ] } } ], "testField": null, "environmentInterpretation1_direction": null, "environmentInterpretation1_seasonality": null, "environmentInterpretation1_variable": null, "pub": [ { "author": { "name": "Carilli, Jessica E." }, "citation": "Carilli, J. E., McGregor, H. V., Gaudry, J. J., Donner, S. D., Gagan, M. K., Stevenson, S., Wong, H. and Fink, D.: Equatorial Pacific coral geochemical records show recent weakening of the Walker Circulation, Paleoceanography, 29(11), 1031–1045, doi:10.1002/2014pa002683, 2014.", "dataUrl": "https://www.ncdc.noaa.gov/cdo/f?p=519:1:::::P1_study_id:17289", "doi": "10.1002/2014PA002683", "year": 2014 } ], "geo": { "longitude": 172.7469, "latitude": 3.0731, "elevation": -5, "geometryType": "Point", "siteName": "Butaritari Atoll, Gilbert Islands" }, "@context": "context.jsonld" }