The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.
"isotope ratio mass spectrometer with automatic carbonate preparation system"
X-ray diffraction, petrographic thin-section, and scanning electron microscope (SEM) analyses
; climateInterpretation_seasonality changed - was originally seasonal; archiveType changed - was originally Coral (CO); archiveType changed - was originally Coral (CO)
This tracer responds to water temperature through a temperature- dependent fractionation [;?0.2? d18O/i¿½C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.
This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.
; archiveType changed - was originally Coral (CO)
Laing Island, Papua New Guinea oxygen isotope record 1884-1993
year (LPD5024de7f): interpretation4_scope: '' has been replaced by 'climate'
year (LPDdcf3abca): interpretation4_scope: '' has been replaced by 'climate'
Column 'CO01TUNG-chron-NA1', with variable name 'yearEnsemble', was added to the dataset
Column 'CO01TUNG-chron-NA2', with variable name 'yearEnsemble', was added to the dataset
Column 'CO01TUNG-chron-NA3', with variable name 'yearEnsemble', was added to the dataset
Column 'CO01TUNG-chron-NA4', with variable name 'yearEnsemble', was added to the dataset
year (LPD5024de7f): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (LPD5024de7f): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
year (LPDdcf3abca): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (LPDdcf3abca): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
d18O (Ocean2kHR_140): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (Ocean2kHR_140): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (Ocean2kHR_141): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (Ocean2kHR_141): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
year (LPD5024de7f): interpretation1_scope: '' has been replaced by 'climate'
year (LPD5024de7f): interpretation2_scope: '' has been replaced by 'climate'
year (LPD5024de7f): interpretation3_scope: '' has been replaced by 'climate'
year (LPDdcf3abca): interpretation1_scope: '' has been replaced by 'climate'
year (LPDdcf3abca): interpretation2_scope: '' has been replaced by 'climate'
year (LPDdcf3abca): interpretation3_scope: '' has been replaced by 'climate'
d18O (Ocean2kHR_140): interpretation2_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_direction: 'negative' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_integrationTime: '3' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_rank: '1' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_140): interpretation2_seasonality: 'subannual' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variable: 'temperature' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_direction: 'positive' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_integrationTime: '3' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_rank: '2' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_140): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (Ocean2kHR_140): interpretation4_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_140): interpretation4_direction: '' has been replaced by 'negative'
d18O (Ocean2kHR_140): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_140): interpretation4_integrationTime: '' has been replaced by '3'
d18O (Ocean2kHR_140): interpretation4_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_140): interpretation4_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_140): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_140): interpretation4_rank: '' has been replaced by '1'
d18O (Ocean2kHR_140): interpretation4_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_140): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (Ocean2kHR_140): interpretation4_variable: '' has been replaced by 'temperature'
d18O (Ocean2kHR_140): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (Ocean2kHR_140): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_140): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (Ocean2kHR_140): interpretation5_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_140): interpretation5_direction: '' has been replaced by 'positive'
d18O (Ocean2kHR_140): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_140): interpretation5_integrationTime: '' has been replaced by '3'
d18O (Ocean2kHR_140): interpretation5_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_140): interpretation5_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_140): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_140): interpretation5_rank: '' has been replaced by '2'
d18O (Ocean2kHR_140): interpretation5_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_140): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (Ocean2kHR_140): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (Ocean2kHR_140): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_140): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (Ocean2kHR_140): interpretation6_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_141): interpretation2_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_direction: 'negative' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_integrationTime: '1 to 3 years' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_rank: '1' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_141): interpretation2_seasonality: 'subannual' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variable: 'temperature' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_direction: 'positive' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_integrationTime: '3' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_rank: '2' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_141): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (Ocean2kHR_141): interpretation4_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_141): interpretation4_direction: '' has been replaced by 'negative'
d18O (Ocean2kHR_141): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_141): interpretation4_integrationTime: '' has been replaced by '1 to 3 years'
d18O (Ocean2kHR_141): interpretation4_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_141): interpretation4_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_141): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_141): interpretation4_rank: '' has been replaced by '1'
d18O (Ocean2kHR_141): interpretation4_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_141): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (Ocean2kHR_141): interpretation4_variable: '' has been replaced by 'temperature'
d18O (Ocean2kHR_141): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (Ocean2kHR_141): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_141): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (Ocean2kHR_141): interpretation5_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_141): interpretation5_direction: '' has been replaced by 'positive'
d18O (Ocean2kHR_141): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_141): interpretation5_integrationTime: '' has been replaced by '3'
d18O (Ocean2kHR_141): interpretation5_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_141): interpretation5_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_141): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_141): interpretation5_rank: '' has been replaced by '2'
d18O (Ocean2kHR_141): interpretation5_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_141): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (Ocean2kHR_141): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (Ocean2kHR_141): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_141): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (Ocean2kHR_141): interpretation6_scope: '' has been replaced by 'isotope'
Updated lipdverse database entry with a changed file.
d18O (Ocean2kHR_140): interpretation1_seasonality: 'not applicable (subannually resolved)' has been replaced by 'subannual'
d18O (Ocean2kHR_140): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (Ocean2kHR_140): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (Ocean2kHR_140): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (Ocean2kHR_141): interpretation1_seasonality: 'not applicable (subannually resolved)' has been replaced by 'subannual'
d18O (Ocean2kHR_141): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (Ocean2kHR_141): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (Ocean2kHR_141): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
Changes made as part of LiPDverse vocabulary standardization process
year (LPD5024de7f): paleoData_units: 'AD' has been replaced by 'yr AD'
year (LPD5024de7f): paleoData_longName: '' has been replaced by 'AD'
year (LPDdcf3abca): paleoData_units: 'AD' has been replaced by 'yr AD'
year (LPDdcf3abca): paleoData_longName: '' has been replaced by 'AD'
d18O (Ocean2kHR_140): paleoData_longName: '' has been replaced by 'AD'
d18O (Ocean2kHR_141): paleoData_longName: '' has been replaced by 'AD'
Tudhope, A.W.; Chilcott, C.P.; McCulloch, M.T.; Cook, E.R.; Chappell, J.; Ellam, R.M.; Lea, D.W.; Lough, J.M.; Shimmield, G.B.
Tudhope, A. W.: Variability in the El Nino-Southern Oscillation Through a Glacial-Interglacial Cycle, Science, 291(5508), 1511–1517, doi:10.1126/science.1057969, 2001.
American Association for the Advancement of Science (AAAS)
Variability in the El Nino-Southern Oscillation Through a Glacial-Interglacial Cycle
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
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.