{ "paleoData": [ { "measurementTable": [ { "googleWorkSheetKey": "o8xteeq", "tableName": "paleo1measurement1", "missingValue": "NaN", "d18O": { "archiveGenus": "Diploastrea", "archiveSpecies": "NA", "chronologyIntegrationTime": "1 to 2", "chronologyIntegrationTimeBasis": "chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. \"we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). \"", "chronologyIntegrationTimeUncertainty": "1 yr", "chronologyIntegrationTimeUncertaintyType": "chronological", "chronologyIntegrationTimeUnits": "months", "description": "carbonate", "hasChron": "0", "hasMaxValue": -3.345, "hasMeanValue": -4.0073, "hasMedianValue": -4.015, "hasMinValue": -4.562, "hasPaleoDepth": "0", "hasTimeTsid": "MATab972076e1", "inCompilation": "Ocean2k_v1.0.0 | PAGES2k_v1.12.0", "inferredMaterial": "surface seawater", "inferredMaterialGroup": "surface water", "inferredMaterialGroupOriginal": "surface seawater", "instrument": "Micromass Optima mass spectrometer with a Micromass Isocarb automated preparation system", "iso2kCertification": "DMT (1/14/19)", "iso2kPrimaryTimeseries": "TRUE", "iso2kUI": "CO06DATZ01A", "isPrimary": false, "longName": "AD", "measurementMaterial": "coral", "measurementMaterialDetail": "aragonite", "measurementStandard": "PDB", "measurementTableMD5": "7760ba0309c5e73af35c2e555efba121", "measurementTableName": "measurementTable1", "medianRes12k": "NA", "notes": "; climateInterpretation_seasonality changed - was originally monthly, bimonthly; archiveType changed - was originally Coral (CO)", "ocean2kID": "IndianMafiaDamassa2006", "pages2kId": "Ocn_077", "pages2kID": "Ocn_077", "paleoDataMD5": "a9139d3f63e6a78e966063f8161aa4ea", "paleoDataTableName": "pt1_1", "paleoMeasurementTableMD5": "7760ba0309c5e73af35c2e555efba121", "primaryAgeColumn": false, "proxy": "d18O", "proxyLumps": "isotope", "proxyLumpsOriginal": "d18O", "QCCertification": "DMT (1/14/19)", "QCnotes": "Note: floating fossil coral sections have greater uncertainty in absolute temperature for palaeoclimate reconstructions (NJA)", "TSid": "Ocean2kHR_007_iso2k", "uncertaintyAnalytical": "0.08permil (1sigma)", "units": "permil", "useInGlobalTemperatureAnalysis": "TRUE", "variableName": "d18O", "variableType": "measured", "values": [-3.967, -4.075, -4.001, -3.983, -3.952, -3.817, -3.755, -3.776, -3.823, -3.917, 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We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). \"", "integrationTimeUncertainty": "1 yr", "integrationTimeUncertaintyType": "chronological", "integrationTimeUnits": "months", "mathematicalRelation": "linear", "rank": 1, "scope": "isotope", "seasonality": "subannual", "variable": "temperature", "variableGroup": "Temperature", "variableGroupDirection": "negative", "variableGroupOriginal": "T_water" }, { "coefficient": "NA", "direction": "positive", "fraction": "NA", "inferredMaterial": "seawater", "integrationTime": "1 to 2", "integrationTimeBasis": "chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. \"we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. 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"https://lipdverse.org/data/hoNIMzXkyb2OxhlM7tD3/1_0_6", "maxYear": 1998.125, "minYear": 1622, "modernSystem_instrumentalDatasetCoordinates": "-8.0167, 39.5", "modernSystem_instrumentalDatasetURL": "https://www.ncdc.noaa.gov/cdo/f?p=519:1:0::::P1_STUDY_ID:10808", "nUniqueAges": 0, "nUniqueGoodAges": 0, "nUniqueOtherAges": 0, "originalDataUrl": "https://www.ncdc.noaa.gov/paleo/study/10808", "originalDataURL": "https://www.ncdc.noaa.gov/paleo/study/10808", "proxySystemModel_observationModel": "Comboul et al. 2015", "proxySystemModel_sensorModel": "Thompson et al. 2013", "studyName": "Mafia d18O composition 1896-1998, 1622-1722", "tagMD5": "498c3241d45fcb99c4a1aab2a34eea75", "lipdVersion": 1.3, "changelog": [ { "version": "1.0.6", "lastVersion": "1.0.5", "curator": "nicholas", "timestamp": "2025-05-20 16:18:33.601235 UTC", "changes": { "Paleo Interpretation metadata": [ ["year (MATab972076e1): interpretation4_scope: '' has been replaced by 'climate'"], ["year (MATab972076e1): interpretation5_scope: '' has been replaced by 'climate'"] ] } }, { "version": "1.0.5", "lastVersion": "1.0.4", "curator": "nicholas", "timestamp": "2025-04-17 20:03:57.680892 UTC", "changes": { "Paleo Column metadata": [ ["year (MATab972076e1): paleoData_isPrimary: '' has been replaced by 'TRUE'"], ["year (MATab972076e1): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'"], ["d18O (Ocean2kHR_007): paleoData_isPrimary: '' has been replaced by 'FALSE'"], ["d18O (Ocean2kHR_007): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'"] ] } }, { "version": "1.0.4", "lastVersion": "1.0.3", "curator": "nicholas", "timestamp": "2025-04-11 16:13:31.28898 UTC", "changes": { "Paleo Interpretation metadata": [ ["year (MATab972076e1): interpretation1_scope: '' has been replaced by 'climate'"], ["year (MATab972076e1): interpretation2_scope: '' has been replaced by 'climate'"], ["year (MATab972076e1): interpretation3_scope: '' has been replaced by 'climate'"], ["d18O (Ocean2kHR_007): interpretation2_basis: 'The coral captures approximately 60% of the full range of annual SST (4i¿½C = 0.88%).' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_direction: 'negative' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_fraction: '0.6' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_inferredMaterial: 'seawater' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_integrationTime: '1 to 2' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_integrationTimeBasis: 'chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. \"we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). \"' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_integrationTimeUncertainty: '1 yr' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_integrationTimeUncertaintyType: 'chronological' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_integrationTimeUnits: 'months' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_mathematicalRelation: 'linear' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_rank: '1' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_scope: 'isotope' has been replaced by 'climate'"], ["d18O (Ocean2kHR_007): interpretation2_seasonality: 'subannual' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_variable: 'temperature' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_variableGroup: 'Temperature' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_variableGroupDirection: 'negative' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_direction: 'positive' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_inferredMaterial: 'seawater' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_integrationTime: '1 to 2' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_integrationTimeBasis: 'chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. \"we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). \"' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_integrationTimeUncertainty: '1 yr' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_integrationTimeUncertaintyType: 'chronological' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_integrationTimeUnits: 'months' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_mathematicalRelation: 'linear' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_rank: '2' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_scope: 'isotope' has been replaced by 'climate'"], ["d18O (Ocean2kHR_007): interpretation3_variable: 'seawaterIsotope' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_variableGroupDirection: 'negative' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''"], ["d18O (Ocean2kHR_007): interpretation4_basis: '' has been replaced by 'The coral captures approximately 60% of the full range of annual SST (4i¿½C = 0.88%).'"], ["d18O (Ocean2kHR_007): interpretation4_direction: '' has been replaced by 'negative'"], ["d18O (Ocean2kHR_007): interpretation4_fraction: '' has been replaced by '0.6'"], ["d18O (Ocean2kHR_007): interpretation4_inferredMaterial: '' has been replaced by 'seawater'"], ["d18O (Ocean2kHR_007): interpretation4_integrationTime: '' has been replaced by '1 to 2'"], ["d18O (Ocean2kHR_007): interpretation4_integrationTimeBasis: '' has been replaced by 'chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. \"we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). \"'"], ["d18O (Ocean2kHR_007): interpretation4_integrationTimeUncertainty: '' has been replaced by '1 yr'"], ["d18O (Ocean2kHR_007): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronological'"], ["d18O (Ocean2kHR_007): interpretation4_integrationTimeUnits: '' has been replaced by 'months'"], ["d18O (Ocean2kHR_007): interpretation4_mathematicalRelation: '' has been replaced by 'linear'"], ["d18O (Ocean2kHR_007): interpretation4_rank: '' has been replaced by '1'"], ["d18O (Ocean2kHR_007): interpretation4_scope: '' has been replaced by 'isotope'"], ["d18O (Ocean2kHR_007): interpretation4_seasonality: '' has been replaced by 'subannual'"], ["d18O (Ocean2kHR_007): interpretation4_variable: '' has been replaced by 'temperature'"], ["d18O (Ocean2kHR_007): interpretation4_variableGroup: '' has been replaced by 'Temperature'"], ["d18O (Ocean2kHR_007): interpretation4_variableGroupDirection: '' has been replaced by 'negative'"], ["d18O (Ocean2kHR_007): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'"], ["d18O (Ocean2kHR_007): interpretation5_direction: '' has been replaced by 'positive'"], ["d18O (Ocean2kHR_007): interpretation5_inferredMaterial: '' has been replaced by 'seawater'"], ["d18O (Ocean2kHR_007): interpretation5_integrationTime: '' has been replaced by '1 to 2'"], ["d18O (Ocean2kHR_007): interpretation5_integrationTimeBasis: '' has been replaced by 'chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. \"we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). \"'"], ["d18O (Ocean2kHR_007): interpretation5_integrationTimeUncertainty: '' has been replaced by '1 yr'"], ["d18O (Ocean2kHR_007): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'chronological'"], ["d18O (Ocean2kHR_007): interpretation5_integrationTimeUnits: '' has been replaced by 'months'"], ["d18O (Ocean2kHR_007): interpretation5_mathematicalRelation: '' has been replaced by 'linear'"], ["d18O (Ocean2kHR_007): interpretation5_rank: '' has been replaced by '2'"], ["d18O (Ocean2kHR_007): interpretation5_scope: '' has been replaced by 'isotope'"], ["d18O (Ocean2kHR_007): interpretation5_variable: '' has been replaced by 'seawaterIsotope'"], ["d18O (Ocean2kHR_007): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'"], ["d18O (Ocean2kHR_007): interpretation5_variableGroupDirection: '' has been replaced by 'negative'"], ["d18O (Ocean2kHR_007): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'"], ["d18O (Ocean2kHR_007): interpretation6_scope: '' has been replaced by 'isotope'"] ] } }, { "version": "1.0.3", "lastVersion": "1.0.2", "curator": "nicholas", "timestamp": "2025-04-09 20:47:23.410028 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Paleo Interpretation metadata": [ ["d18O (Ocean2kHR_007): interpretation1_seasonality: 'not applicable (subannually resolved)' has been replaced by 'subannual'"], ["d18O (Ocean2kHR_007): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'"], ["d18O (Ocean2kHR_007): interpretation2_variable: 'T_water' has been replaced by 'temperature'"], ["d18O (Ocean2kHR_007): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"] ] } }, { "version": "1.0.2", "lastVersion": "1.0.1", "curator": "nicholas", "timestamp": "2025-04-09 17:25:57.598548 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Interpretation metadata": [ ["d18O (Ocean2kHR_007): interpretation1_seasonality: 'not applicable (subannually resolved)' has been replaced by 'subannual'"], ["d18O (Ocean2kHR_007): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'"], ["d18O (Ocean2kHR_007): interpretation2_variable: 'T_water' has been replaced by 'temperature'"], ["d18O (Ocean2kHR_007): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nicholas", "timestamp": "2025-04-08 17:30:22.88387 UTC", "notes": "Changes made as part of LiPDverse vocabulary standardization process", "changes": { "Paleo Column metadata": [ ["year (MATab972076e1): paleoData_units: 'AD' has been replaced by 'yr AD'"], ["year (MATab972076e1): paleoData_longName: '' has been replaced by 'AD'"], ["d18O (Ocean2kHR_007): paleoData_longName: '' has been replaced by 'AD'"] ] } } ], "environmentInterpretation1_direction": null, "environmentInterpretation1_seasonality": null, "environmentInterpretation1_variable": null, "testField": null, "pub": [ { "author": { "name": "Damassa, T.D." }, "citation": "Damassa, T. D., Cole, J. E., Barnett, H. R., Ault, T. R. and McClanahan, T. R.: Enhanced multidecadal climate variability in the seventeenth century from coral isotope records in the western Indian Ocean, Paleoceanography, 21(2), n/a–n/a, doi:10.1029/2005pa001217, 2006.", "citeKey": "damassa2006enhanced", "dataUrl": "https://www.ncdc.noaa.gov/cdo/f?p=519:1:0::::P1_STUDY_ID:10808", "doi": "10.1029/2005PA001217", "issue": "2-Jan", "journal": "Paleoceanography", "pages": "n/a-n/a", "publisher": "Wiley-Blackwell", "title": "Enhanced multidecadal climate variability in the seventeenth century from coral isotope records in the western Indian Ocean", "type": "article", "volume": 21, "year": 2006 }, { "author": { "name": "Tierney, Jessica E. , Abram, Nerilie J. , Anchukaitis, Kevin J. , Evans, Michael N. , Giry, Cyril , Kilbourne, K. Halimeda , Saenger, Casey P. , Wu, Henry C. , Zinke, Jens" }, "citation": "Tierney, J. E., Abram, N. J., Anchukaitis, K. J., Evans, M. N., Giry, C., Kilbourne, K. H., Saenger, C. P., Wu, H. C. and Zinke, J.: Tropical sea surface temperatures for the past four centuries reconstructed from coral archives, Paleoceanography, 30(3), 226–252, doi:10.1002/2014pa002717, 2015.", "citeKey": "tierney2015tropical", "doi": "10.1002/2014PA002717", "institution": "World Data Center for Paleoclimatology", "title": "Ocean2kHR-IndianMafiaDamassa2006", "type": "dataCitation", "url": "https://www.ncdc.noaa.gov/paleo/study/10808", "year": 2015 } ], "geo": { "longitude": 39.5, "latitude": -8.0167, "elevation": -6, "geometryType": "Point", "ocean": "Indian", "pages2kRegion": "Ocean", "siteName": "Mafia Archipelago, Tanzania" }, "@context": "context.jsonld" }