The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997
Multiprep carbonate inlet system and the resulting CO gas was analyzed with a Micromass Optima triple-collecting mass spectro- meter
; archiveType changed - was originally Coral (CO)
Diploastrea heliopora specie; test regarding Diploasrea sampling strategy over the first 50 mm
Composite of CO04BAFI01A and CO04BAFI02A
mid-point depth of the sub-sample drilled for U-Th age
[230Th/238U] activity measured in the sub-sample
Analytical uncertainty of 230Th-238U activity
Analytical uncertainty of 230Th-232Th ratio
Analytical uncertainty of Uncorrected Age
Uncertainty of Corrected Age (includes Th correction)
Calculated initial d234U in the sub-sample
Analytical uncertainty of calculated d234U initial
Depth at the top of the sub-sample for 210Pb analysis
Depth at the bottom of the sub-sample for 210Pb analysis
Lead-210 excess measured in the sub-sample
Depth at the top of the sub-sample for 137Cs analysis
Depth at the bottom of the sub-sample for 137Cs analysis
Cesium-137 g-activity measured in the sub-sample
Analytical uncertainty of 137Cs g-activity
Sample description. E.g., round plug, annual density band
year (MAT034aca7b9b): interpretation4_scope: '' has been replaced by 'climate'
year (MAT2ce6761c47): interpretation4_scope: '' has been replaced by 'climate'
year (MAT3d77acceab): interpretation4_scope: '' has been replaced by 'climate'
depth (MAT3e7e72dbc4): interpretation4_scope: '' has been replaced by 'climate'
depth (MAT41704fb11c): interpretation4_scope: '' has been replaced by 'climate'
ChronData: Duplicated TSids names in original dataset, couldn't log column-level changes.
d18O (CO04BAFI00A): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (CO04BAFI00A): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (CO04BAFI01A): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (CO04BAFI01A): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (CO04BAFI02A): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (CO04BAFI02A): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
year (MAT034aca7b9b): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (MAT034aca7b9b): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
year (MAT2ce6761c47): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (MAT2ce6761c47): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
year (MAT3d77acceab): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (MAT3d77acceab): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
depth (MAT3e7e72dbc4): paleoData_isPrimary: '' has been replaced by 'FALSE'
depth (MAT3e7e72dbc4): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
depth (MAT41704fb11c): paleoData_isPrimary: '' has been replaced by 'FALSE'
depth (MAT41704fb11c): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (CO04BAFI00A): interpretation2_direction: 'negative' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_integrationTimeBasis: 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_rank: '1' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (CO04BAFI00A): interpretation2_seasonality: 'Annual' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_variable: 'temperature' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO04BAFI00A): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_direction: 'positive' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_integrationTimeBasis: 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_rank: '2' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (CO04BAFI00A): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO04BAFI00A): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (CO04BAFI00A): interpretation4_direction: '' has been replaced by 'negative'
d18O (CO04BAFI00A): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO04BAFI00A): interpretation4_integrationTimeBasis: '' has been replaced by 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997'
d18O (CO04BAFI00A): interpretation4_rank: '' has been replaced by '1'
d18O (CO04BAFI00A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI00A): interpretation4_seasonality: '' has been replaced by 'Annual'
d18O (CO04BAFI00A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d18O (CO04BAFI00A): interpretation4_variable: '' has been replaced by 'temperature'
d18O (CO04BAFI00A): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (CO04BAFI00A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO04BAFI00A): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (CO04BAFI00A): interpretation5_direction: '' has been replaced by 'positive'
d18O (CO04BAFI00A): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO04BAFI00A): interpretation5_integrationTimeBasis: '' has been replaced by 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997'
d18O (CO04BAFI00A): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (CO04BAFI00A): interpretation5_rank: '' has been replaced by '2'
d18O (CO04BAFI00A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI00A): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (CO04BAFI00A): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (CO04BAFI00A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO04BAFI00A): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (CO04BAFI00A): interpretation6_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI01A): interpretation2_direction: 'negative' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_integrationTime: '12-Jun' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_integrationTimeBasis: 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_integrationTimeUncertainty: '1/12 to 2/12' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_integrationTimeUncertaintyType: 'chronology' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_integrationTimeUnits: 'year' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_rank: '1' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (CO04BAFI01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_variable: 'temperature' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO04BAFI01A): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_direction: 'positive' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_integrationTime: '12-Jun' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_integrationTimeBasis: 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_integrationTimeUncertainty: '1/12 to 2/12' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_integrationTimeUncertaintyType: 'chronology' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_integrationTimeUnits: 'year' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_rank: '2' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (CO04BAFI01A): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO04BAFI01A): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (CO04BAFI01A): interpretation4_direction: '' has been replaced by 'negative'
d18O (CO04BAFI01A): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO04BAFI01A): interpretation4_integrationTime: '' has been replaced by '12-Jun'
d18O (CO04BAFI01A): interpretation4_integrationTimeBasis: '' has been replaced by 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997'
d18O (CO04BAFI01A): interpretation4_integrationTimeUncertainty: '' has been replaced by '1/12 to 2/12'
d18O (CO04BAFI01A): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronology'
d18O (CO04BAFI01A): interpretation4_integrationTimeUnits: '' has been replaced by 'year'
d18O (CO04BAFI01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (CO04BAFI01A): interpretation4_rank: '' has been replaced by '1'
d18O (CO04BAFI01A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d18O (CO04BAFI01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d18O (CO04BAFI01A): interpretation4_variable: '' has been replaced by 'temperature'
d18O (CO04BAFI01A): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (CO04BAFI01A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO04BAFI01A): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (CO04BAFI01A): interpretation5_direction: '' has been replaced by 'positive'
d18O (CO04BAFI01A): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO04BAFI01A): interpretation5_integrationTime: '' has been replaced by '12-Jun'
d18O (CO04BAFI01A): interpretation5_integrationTimeBasis: '' has been replaced by 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997'
d18O (CO04BAFI01A): interpretation5_integrationTimeUncertainty: '' has been replaced by '1/12 to 2/12'
d18O (CO04BAFI01A): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'chronology'
d18O (CO04BAFI01A): interpretation5_integrationTimeUnits: '' has been replaced by 'year'
d18O (CO04BAFI01A): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (CO04BAFI01A): interpretation5_rank: '' has been replaced by '2'
d18O (CO04BAFI01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI01A): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (CO04BAFI01A): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (CO04BAFI01A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO04BAFI01A): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (CO04BAFI01A): interpretation6_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI02A): interpretation2_direction: 'negative' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_integrationTime: '12-Jun' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_integrationTimeBasis: 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_integrationTimeUncertainty: '1/12 to 2/12' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_integrationTimeUncertaintyType: 'chronology' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_integrationTimeUnits: 'year' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_rank: '1' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (CO04BAFI02A): interpretation2_seasonality: 'Annual' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_variable: 'temperature' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO04BAFI02A): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_direction: 'positive' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_integrationTime: '12-Jun' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_integrationTimeBasis: 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_integrationTimeUncertainty: '1/12 to 2/12' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_integrationTimeUncertaintyType: 'chronology' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_integrationTimeUnits: 'year' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_rank: '2' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (CO04BAFI02A): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO04BAFI02A): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (CO04BAFI02A): interpretation4_direction: '' has been replaced by 'negative'
d18O (CO04BAFI02A): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO04BAFI02A): interpretation4_integrationTime: '' has been replaced by '12-Jun'
d18O (CO04BAFI02A): interpretation4_integrationTimeBasis: '' has been replaced by 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997'
d18O (CO04BAFI02A): interpretation4_integrationTimeUncertainty: '' has been replaced by '1/12 to 2/12'
d18O (CO04BAFI02A): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronology'
d18O (CO04BAFI02A): interpretation4_integrationTimeUnits: '' has been replaced by 'year'
d18O (CO04BAFI02A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (CO04BAFI02A): interpretation4_rank: '' has been replaced by '1'
d18O (CO04BAFI02A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI02A): interpretation4_seasonality: '' has been replaced by 'Annual'
d18O (CO04BAFI02A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d18O (CO04BAFI02A): interpretation4_variable: '' has been replaced by 'temperature'
d18O (CO04BAFI02A): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (CO04BAFI02A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO04BAFI02A): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (CO04BAFI02A): interpretation5_direction: '' has been replaced by 'positive'
d18O (CO04BAFI02A): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO04BAFI02A): interpretation5_integrationTime: '' has been replaced by '12-Jun'
d18O (CO04BAFI02A): interpretation5_integrationTimeBasis: '' has been replaced by 'The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997'
d18O (CO04BAFI02A): interpretation5_integrationTimeUncertainty: '' has been replaced by '1/12 to 2/12'
d18O (CO04BAFI02A): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'chronology'
d18O (CO04BAFI02A): interpretation5_integrationTimeUnits: '' has been replaced by 'year'
d18O (CO04BAFI02A): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (CO04BAFI02A): interpretation5_rank: '' has been replaced by '2'
d18O (CO04BAFI02A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (CO04BAFI02A): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (CO04BAFI02A): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (CO04BAFI02A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO04BAFI02A): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (CO04BAFI02A): interpretation6_scope: '' has been replaced by 'isotope'
year (MAT034aca7b9b): interpretation1_scope: '' has been replaced by 'climate'
year (MAT034aca7b9b): interpretation2_scope: '' has been replaced by 'climate'
year (MAT034aca7b9b): interpretation3_scope: '' has been replaced by 'climate'
year (MAT2ce6761c47): interpretation1_scope: '' has been replaced by 'climate'
year (MAT2ce6761c47): interpretation2_scope: '' has been replaced by 'climate'
year (MAT2ce6761c47): interpretation3_scope: '' has been replaced by 'climate'
year (MAT3d77acceab): interpretation1_scope: '' has been replaced by 'climate'
year (MAT3d77acceab): interpretation2_scope: '' has been replaced by 'climate'
year (MAT3d77acceab): interpretation3_scope: '' has been replaced by 'climate'
depth (MAT3e7e72dbc4): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT3e7e72dbc4): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT3e7e72dbc4): interpretation3_scope: '' has been replaced by 'climate'
depth (MAT41704fb11c): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT41704fb11c): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT41704fb11c): interpretation3_scope: '' has been replaced by 'climate'
Updated lipdverse database entry with a changed file.
d18O (CO04BAFI00A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO04BAFI00A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (CO04BAFI00A): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (CO04BAFI00A): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (CO04BAFI01A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO04BAFI01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (CO04BAFI01A): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (CO04BAFI01A): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
d18O (CO04BAFI02A): interpretation1_variable: 'temperature and salinity' has been replaced by 'temperature'
d18O (CO04BAFI02A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (CO04BAFI02A): interpretation2_variable: 'T_water' has been replaced by 'temperature'
d18O (CO04BAFI02A): interpretation3_variable: 'd18O_seawater' has been replaced by 'seawaterIsotope'
Changes made as part of LiPDverse vocabulary standardization process
d18O (CO04BAFI00A): paleoData_longName: '' has been replaced by 'AD'
d18O (CO04BAFI01A): paleoData_longName: '' has been replaced by 'AD'
d18O (CO04BAFI02A): paleoData_longName: '' has been replaced by 'AD'
year (MAT034aca7b9b): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT034aca7b9b): paleoData_longName: '' has been replaced by 'AD'
year (MAT2ce6761c47): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT2ce6761c47): paleoData_longName: '' has been replaced by 'AD'
year (MAT3d77acceab): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT3d77acceab): paleoData_longName: '' has been replaced by 'AD'
depth (MAT3e7e72dbc4): paleoData_longName: '' has been replaced by 'AD'
depth (MAT41704fb11c): paleoData_longName: '' has been replaced by 'AD'
Bagnato, S., B.K. Linsley, S.S. Howe, G.M. Wellington, J. Salinger
Bagnato, S., Linsley, B. K., Howe, S. S., Wellington, G. M. and Salinger, J.: Evaluating the use of the massive coralDiploastrea helioporafor paleoclimate reconstruction, Paleoceanography, 19(1), n/a–n/a, doi:10.1029/2003pa000935, 2004.