Version history for vyDhoIMb8k0yw0TdJdlJ - CO01TUNG

Version: 1.0.8

lastVersion: 1.0.7
curator: nicholas
timestamp: 2025-05-20 18:27:36.390993 UTC
changes:
- Paleo Interpretation metadata:
  - year (LPD5024de7f_iso2k): interpretation5_scope: NULL has been replaced by ‘climate’
  - year (LPDdcf3abca_iso2k): interpretation5_scope: NULL has been replaced by ‘climate’

Version: 1.0.7

lastVersion: 1.0.6
curator: nicholas
timestamp: 2025-05-20 16:18:31.472443 UTC
changes:
- Paleo Interpretation metadata:
  - year (LPD5024de7f): interpretation4_scope: NULL has been replaced by ‘climate’
  - year (LPDdcf3abca): interpretation4_scope: NULL has been replaced by ‘climate’
- ChronData table:
  - 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

Version: 1.0.6

lastVersion: 1.0.5
curator: nicholas
timestamp: 2025-04-17 20:03:55.245742 UTC
changes:
- Paleo Column metadata:
  - year (LPD5024de7f): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - year (LPD5024de7f): paleoData_primaryAgeColumn: NULL has been replaced by ‘TRUE’
  - year (LPDdcf3abca): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - year (LPDdcf3abca): paleoData_primaryAgeColumn: NULL has been replaced by ‘TRUE’
  - d18O (Ocean2kHR_140): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - d18O (Ocean2kHR_140): paleoData_primaryAgeColumn: NULL has been replaced by ‘FALSE’
  - d18O (Ocean2kHR_141): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - d18O (Ocean2kHR_141): paleoData_primaryAgeColumn: NULL has been replaced by ‘FALSE’
- ChronData table:
  - 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

Version: 1.0.5

lastVersion: 1.0.4
curator: nicholas
timestamp: 2025-04-11 16:10:24.607557 UTC
changes:
- Paleo Interpretation metadata:
  - year (LPD5024de7f): interpretation1_scope: NULL has been replaced by ‘climate’
  - year (LPD5024de7f): interpretation2_scope: NULL has been replaced by ‘climate’
  - year (LPD5024de7f): interpretation3_scope: NULL has been replaced by ‘climate’
  - year (LPDdcf3abca): interpretation1_scope: NULL has been replaced by ‘climate’
  - year (LPDdcf3abca): interpretation2_scope: NULL has been replaced by ‘climate’
  - year (LPDdcf3abca): interpretation3_scope: NULL 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 NULL
  - d18O (Ocean2kHR_140): interpretation2_direction: ‘negative’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_inferredMaterial: ‘seawater’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_integrationTime: ‘3’ has been replaced by NULL
  - 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 NULL
  - d18O (Ocean2kHR_140): interpretation2_integrationTimeUnits: ‘months’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_mathematicalRelation: ‘linear’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_rank: ‘1’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_scope: ‘isotope’ has been replaced by ‘climate’
  - d18O (Ocean2kHR_140): interpretation2_seasonality: ‘subannual’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_variable: ‘temperature’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_variableGroup: ‘Temperature’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_variableGroupDirection: ‘negative’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation2_variableGroupOriginal: ‘T_water’ has been replaced by NULL
  - 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 NULL
  - d18O (Ocean2kHR_140): interpretation3_direction: ‘positive’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_inferredMaterial: ‘seawater’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_integrationTime: ‘3’ has been replaced by NULL
  - 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 NULL
  - d18O (Ocean2kHR_140): interpretation3_integrationTimeUnits: ‘months’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_mathematicalRelation: ‘linear’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_rank: ‘2’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_scope: ‘isotope’ has been replaced by ‘climate’
  - d18O (Ocean2kHR_140): interpretation3_variable: ‘seawaterIsotope’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_variableGroup: ‘EffectiveMoisture’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_variableGroupDirection: ‘negative’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation3_variableGroupOriginal: ‘d18O_seawater’ has been replaced by NULL
  - d18O (Ocean2kHR_140): interpretation4_basis: NULL 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: NULL has been replaced by ‘negative’
  - d18O (Ocean2kHR_140): interpretation4_inferredMaterial: NULL has been replaced by ‘seawater’
  - d18O (Ocean2kHR_140): interpretation4_integrationTime: NULL has been replaced by ‘3’
  - d18O (Ocean2kHR_140): interpretation4_integrationTimeBasis: NULL 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: NULL has been replaced by ‘months’
  - d18O (Ocean2kHR_140): interpretation4_mathematicalRelation: NULL has been replaced by ‘linear’
  - d18O (Ocean2kHR_140): interpretation4_rank: NULL has been replaced by ‘1’
  - d18O (Ocean2kHR_140): interpretation4_scope: NULL has been replaced by ‘isotope’
  - d18O (Ocean2kHR_140): interpretation4_seasonality: NULL has been replaced by ‘subannual’
  - d18O (Ocean2kHR_140): interpretation4_variable: NULL has been replaced by ‘temperature’
  - d18O (Ocean2kHR_140): interpretation4_variableGroup: NULL has been replaced by ‘Temperature’
  - d18O (Ocean2kHR_140): interpretation4_variableGroupDirection: NULL has been replaced by ‘negative’
  - d18O (Ocean2kHR_140): interpretation4_variableGroupOriginal: NULL has been replaced by ‘T_water’
  - d18O (Ocean2kHR_140): interpretation5_basis: NULL 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: NULL has been replaced by ‘positive’
  - d18O (Ocean2kHR_140): interpretation5_inferredMaterial: NULL has been replaced by ‘seawater’
  - d18O (Ocean2kHR_140): interpretation5_integrationTime: NULL has been replaced by ‘3’
  - d18O (Ocean2kHR_140): interpretation5_integrationTimeBasis: NULL 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: NULL has been replaced by ‘months’
  - d18O (Ocean2kHR_140): interpretation5_mathematicalRelation: NULL has been replaced by ‘linear’
  - d18O (Ocean2kHR_140): interpretation5_rank: NULL has been replaced by ‘2’
  - d18O (Ocean2kHR_140): interpretation5_scope: NULL has been replaced by ‘isotope’
  - d18O (Ocean2kHR_140): interpretation5_variable: NULL has been replaced by ‘seawaterIsotope’
  - d18O (Ocean2kHR_140): interpretation5_variableGroup: NULL has been replaced by ‘EffectiveMoisture’
  - d18O (Ocean2kHR_140): interpretation5_variableGroupDirection: NULL has been replaced by ‘negative’
  - d18O (Ocean2kHR_140): interpretation5_variableGroupOriginal: NULL has been replaced by ‘d18O_seawater’
  - d18O (Ocean2kHR_140): interpretation6_scope: NULL 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 NULL
  - d18O (Ocean2kHR_141): interpretation2_direction: ‘negative’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_inferredMaterial: ‘seawater’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_integrationTime: ‘1 to 3 years’ has been replaced by NULL
  - 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 NULL
  - d18O (Ocean2kHR_141): interpretation2_integrationTimeUnits: ‘months’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_mathematicalRelation: ‘linear’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_rank: ‘1’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_scope: ‘isotope’ has been replaced by ‘climate’
  - d18O (Ocean2kHR_141): interpretation2_seasonality: ‘subannual’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_variable: ‘temperature’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_variableGroup: ‘Temperature’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_variableGroupDirection: ‘negative’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation2_variableGroupOriginal: ‘T_water’ has been replaced by NULL
  - 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 NULL
  - d18O (Ocean2kHR_141): interpretation3_direction: ‘positive’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_inferredMaterial: ‘seawater’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_integrationTime: ‘3’ has been replaced by NULL
  - 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 NULL
  - d18O (Ocean2kHR_141): interpretation3_integrationTimeUnits: ‘months’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_mathematicalRelation: ‘linear’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_rank: ‘2’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_scope: ‘isotope’ has been replaced by ‘climate’
  - d18O (Ocean2kHR_141): interpretation3_variable: ‘seawaterIsotope’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_variableGroup: ‘EffectiveMoisture’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_variableGroupDirection: ‘negative’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation3_variableGroupOriginal: ‘d18O_seawater’ has been replaced by NULL
  - d18O (Ocean2kHR_141): interpretation4_basis: NULL 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: NULL has been replaced by ‘negative’
  - d18O (Ocean2kHR_141): interpretation4_inferredMaterial: NULL has been replaced by ‘seawater’
  - d18O (Ocean2kHR_141): interpretation4_integrationTime: NULL has been replaced by ‘1 to 3 years’
  - d18O (Ocean2kHR_141): interpretation4_integrationTimeBasis: NULL 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: NULL has been replaced by ‘months’
  - d18O (Ocean2kHR_141): interpretation4_mathematicalRelation: NULL has been replaced by ‘linear’
  - d18O (Ocean2kHR_141): interpretation4_rank: NULL has been replaced by ‘1’
  - d18O (Ocean2kHR_141): interpretation4_scope: NULL has been replaced by ‘isotope’
  - d18O (Ocean2kHR_141): interpretation4_seasonality: NULL has been replaced by ‘subannual’
  - d18O (Ocean2kHR_141): interpretation4_variable: NULL has been replaced by ‘temperature’
  - d18O (Ocean2kHR_141): interpretation4_variableGroup: NULL has been replaced by ‘Temperature’
  - d18O (Ocean2kHR_141): interpretation4_variableGroupDirection: NULL has been replaced by ‘negative’
  - d18O (Ocean2kHR_141): interpretation4_variableGroupOriginal: NULL has been replaced by ‘T_water’
  - d18O (Ocean2kHR_141): interpretation5_basis: NULL 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: NULL has been replaced by ‘positive’
  - d18O (Ocean2kHR_141): interpretation5_inferredMaterial: NULL has been replaced by ‘seawater’
  - d18O (Ocean2kHR_141): interpretation5_integrationTime: NULL has been replaced by ‘3’
  - d18O (Ocean2kHR_141): interpretation5_integrationTimeBasis: NULL 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: NULL has been replaced by ‘months’
  - d18O (Ocean2kHR_141): interpretation5_mathematicalRelation: NULL has been replaced by ‘linear’
  - d18O (Ocean2kHR_141): interpretation5_rank: NULL has been replaced by ‘2’
  - d18O (Ocean2kHR_141): interpretation5_scope: NULL has been replaced by ‘isotope’
  - d18O (Ocean2kHR_141): interpretation5_variable: NULL has been replaced by ‘seawaterIsotope’
  - d18O (Ocean2kHR_141): interpretation5_variableGroup: NULL has been replaced by ‘EffectiveMoisture’
  - d18O (Ocean2kHR_141): interpretation5_variableGroupDirection: NULL has been replaced by ‘negative’
  - d18O (Ocean2kHR_141): interpretation5_variableGroupOriginal: NULL has been replaced by ‘d18O_seawater’
  - d18O (Ocean2kHR_141): interpretation6_scope: NULL has been replaced by ‘isotope’
- ChronData table:
  - 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

Version: 1.0.4

lastVersion: 1.0.3
curator: nicholas
timestamp: 2025-04-08 22:57:27.926946 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Paleo Interpretation metadata:
  - 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’
- ChronData table:
  - 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

Version: 1.0.3

lastVersion: 1.0.2
curator: nicholas
timestamp: 2025-04-08 22:57:23.729675 UTC
notes: Changes made as part of LiPDverse vocabulary standardization process
changes:
- Paleo Interpretation metadata:
  - 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’
- ChronData table:
  - 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

Version: 1.0.2

lastVersion: 1.0.1
curator: nicholas
timestamp: 2025-04-08 18:46:31.15538 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- ChronData table:
  - 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

Version: 1.0.1

lastVersion: 1.0.0
curator: nicholas
timestamp: 2025-04-08 17:30:20.646503 UTC
notes: Changes made as part of LiPDverse vocabulary standardization process
changes:
- Paleo Column metadata:
  - year (LPD5024de7f): paleoData_units: ‘AD’ has been replaced by ‘yr AD’
  - year (LPD5024de7f): paleoData_longName: NULL has been replaced by ‘AD’
  - year (LPDdcf3abca): paleoData_units: ‘AD’ has been replaced by ‘yr AD’
  - year (LPDdcf3abca): paleoData_longName: NULL has been replaced by ‘AD’
  - d18O (Ocean2kHR_140): paleoData_longName: NULL has been replaced by ‘AD’
  - d18O (Ocean2kHR_141): paleoData_longName: NULL has been replaced by ‘AD’