Version history for xfDZQAuBvICCPhTZHPrL - LS97HOKA

Version: 1.0.7

• lastVersion: 1.0.6
• curator: nicholas
• timestamp: 2025-05-22 04:33:58.746978 UTC
• changes:
  • Paleo Interpretation metadata:
    • age (MAT5a83d3ba3b): interpretation4_scope: NULL has been replaced by ‘climate’
    • age (MAT5a83d3ba3b): interpretation5_scope: NULL has been replaced by ‘climate’
    • age (MAT5a83d3ba3b): interpretation6_scope: NULL has been replaced by ‘climate’
    • depth (MATeb6bfe7013): interpretation4_scope: NULL has been replaced by ‘climate’
    • depth (MATeb6bfe7013): interpretation5_scope: NULL has been replaced by ‘climate’
    • depth (MATeb6bfe7013): interpretation6_scope: NULL has been replaced by ‘climate’

Version: 1.0.6

• lastVersion: 1.0.5
• curator: nicholas
• timestamp: 2025-05-22 00:50:32.615602 UTC
• notes: Updated lipdverse database entry with a changed file.
• changes:
  • Paleo Column metadata:
    • age (MAT5a83d3ba3b): paleoData_units: ‘yr AD’ has been replaced by ‘yr BP’
    • age (MAT5a83d3ba3b): paleoData_variableName: ‘year’ has been replaced by ‘age’

Version: 1.0.5

• lastVersion: 1.0.4
• curator: nicholas
• timestamp: 2025-04-17 20:04:43.418964 UTC
• changes:
  • Paleo Column metadata:
    • d18O (LS97HOKA1a): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • d18O (LS97HOKA1a): paleoData_primaryAgeColumn: NULL has been replaced by ‘FALSE’
    • year (MAT5a83d3ba3b): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • year (MAT5a83d3ba3b): paleoData_primaryAgeColumn: NULL has been replaced by ‘TRUE’
    • depth (MATeb6bfe7013): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • depth (MATeb6bfe7013): paleoData_primaryAgeColumn: NULL has been replaced by ‘FALSE’

Version: 1.0.4

• lastVersion: 1.0.3
• curator: nicholas
• timestamp: 2025-04-11 16:27:01.973325 UTC
• changes:
  • Paleo Interpretation metadata:
    • d18O (LS97HOKA1a): interpretation1_basis: ‘In a closed, low-latitude lake basin, the d18O values of the lake water, which are the main control on the d18O values of carbonates, are influenced largely by the balance between inflow (mainly shallow groundwater, in the case of Kajemarum) and evaporation (Talbot 1990). Thus, the d18O record in endogenic carbonate should largely reflect salinity.’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation1_direction: ‘negative’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation1_inferredMaterial: ‘lake water’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation1_rank: ‘1’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation1_scope: ‘isotope’ has been replaced by ‘climate’
    • d18O (LS97HOKA1a): interpretation1_variable: ‘hydrologicBalance’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation1_variableGroup: ‘EffectiveMoisture’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation1_variableGroupDirection: ‘negative’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation1_variableGroupOriginal: ‘I_E’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation2_direction: ‘negative’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation2_inferredMaterial: ‘Lake water’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation2_rank: ‘2’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation2_scope: ‘isotope’ has been replaced by ‘climate’
    • d18O (LS97HOKA1a): interpretation2_variable: ‘temperature’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation2_variableGroup: ‘Temperature’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation2_variableGroupDirection: ‘negative’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation2_variableGroupOriginal: ‘T_water’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation3_basis: ‘Changes in d18O values that do not parallel those in Sr/Ca, however, are best explained by changes in water temperature, or in the 18O/16O ratio of precipitation. Changes in the isotopic composition of precipitation may be brought about by shifts in water-vapour source, air temperature (Andrews 1993) or cloud height. Variations in the intensity of monsoon convection may be important, since highly 18O-depleted rainfall is produced by the strong uplift that occurs in monsoon clouds with cold tops (Fontes et al. 1993).’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation3_inferredMaterial: ‘Lake water’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation3_rank: ‘3’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation3_scope: ‘isotope’ has been replaced by ‘climate’
    • d18O (LS97HOKA1a): interpretation3_variable: ‘precipitationIsotope’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation3_variableGroup: ‘P_isotope’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation3_variableGroupDirection: ‘positive’ has been replaced by NULL
    • d18O (LS97HOKA1a): interpretation4_basis: NULL has been replaced by ‘In a closed, low-latitude lake basin, the d18O values of the lake water, which are the main control on the d18O values of carbonates, are influenced largely by the balance between inflow (mainly shallow groundwater, in the case of Kajemarum) and evaporation (Talbot 1990). Thus, the d18O record in endogenic carbonate should largely reflect salinity.’
    • d18O (LS97HOKA1a): interpretation4_direction: NULL has been replaced by ‘negative’
    • d18O (LS97HOKA1a): interpretation4_inferredMaterial: NULL has been replaced by ‘lake water’
    • d18O (LS97HOKA1a): interpretation4_rank: NULL has been replaced by ‘1’
    • d18O (LS97HOKA1a): interpretation4_scope: NULL has been replaced by ‘isotope’
    • d18O (LS97HOKA1a): interpretation4_variable: NULL has been replaced by ‘hydrologicBalance’
    • d18O (LS97HOKA1a): interpretation4_variableGroup: NULL has been replaced by ‘EffectiveMoisture’
    • d18O (LS97HOKA1a): interpretation4_variableGroupDirection: NULL has been replaced by ‘negative’
    • d18O (LS97HOKA1a): interpretation4_variableGroupOriginal: NULL has been replaced by ‘I_E’
    • d18O (LS97HOKA1a): interpretation5_direction: NULL has been replaced by ‘negative’
    • d18O (LS97HOKA1a): interpretation5_inferredMaterial: NULL has been replaced by ‘Lake water’
    • d18O (LS97HOKA1a): interpretation5_rank: NULL has been replaced by ‘2’
    • d18O (LS97HOKA1a): interpretation5_scope: NULL has been replaced by ‘isotope’
    • d18O (LS97HOKA1a): interpretation5_variable: NULL has been replaced by ‘temperature’
    • d18O (LS97HOKA1a): interpretation5_variableGroup: NULL has been replaced by ‘Temperature’
    • d18O (LS97HOKA1a): interpretation5_variableGroupDirection: NULL has been replaced by ‘negative’
    • d18O (LS97HOKA1a): interpretation5_variableGroupOriginal: NULL has been replaced by ‘T_water’
    • d18O (LS97HOKA1a): interpretation6_basis: NULL has been replaced by ‘Changes in d18O values that do not parallel those in Sr/Ca, however, are best explained by changes in water temperature, or in the 18O/16O ratio of precipitation. Changes in the isotopic composition of precipitation may be brought about by shifts in water-vapour source, air temperature (Andrews 1993) or cloud height. Variations in the intensity of monsoon convection may be important, since highly 18O-depleted rainfall is produced by the strong uplift that occurs in monsoon clouds with cold tops (Fontes et al. 1993).’
    • d18O (LS97HOKA1a): interpretation6_inferredMaterial: NULL has been replaced by ‘Lake water’
    • d18O (LS97HOKA1a): interpretation6_rank: NULL has been replaced by ‘3’
    • d18O (LS97HOKA1a): interpretation6_scope: NULL has been replaced by ‘isotope’
    • d18O (LS97HOKA1a): interpretation6_variable: NULL has been replaced by ‘precipitationIsotope’
    • d18O (LS97HOKA1a): interpretation6_variableGroup: NULL has been replaced by ‘P_isotope’
    • d18O (LS97HOKA1a): interpretation6_variableGroupDirection: NULL has been replaced by ‘positive’
    • year (MAT5a83d3ba3b): interpretation1_scope: NULL has been replaced by ‘climate’
    • year (MAT5a83d3ba3b): interpretation2_scope: NULL has been replaced by ‘climate’
    • year (MAT5a83d3ba3b): interpretation3_scope: NULL has been replaced by ‘climate’
    • depth (MATeb6bfe7013): interpretation1_scope: NULL has been replaced by ‘climate’
    • depth (MATeb6bfe7013): interpretation2_scope: NULL has been replaced by ‘climate’
    • depth (MATeb6bfe7013): interpretation3_scope: NULL has been replaced by ‘climate’

Version: 1.0.3

• lastVersion: 1.0.2
• curator: nicholas
• timestamp: 2025-04-09 20:48:39.31506 UTC
• notes: Updated lipdverse database entry with a changed file.
• changes:
  • Paleo Interpretation metadata:
    • d18O (LS97HOKA1a): interpretation1_variable: ‘I_E’ has been replaced by ‘hydrologicBalance’
    • d18O (LS97HOKA1a): interpretation2_variable: ‘T_water’ has been replaced by ‘temperature’
    • d18O (LS97HOKA1a): interpretation3_variable: ‘P_isotope’ has been replaced by ‘precipitationIsotope’

Version: 1.0.2

• lastVersion: 1.0.1
• curator: nicholas
• timestamp: 2025-04-09 19:55:08.535133 UTC
• notes: Changes made as part of LiPDverse vocabulary standardization process
• changes:
  • Paleo Interpretation metadata:
    • d18O (LS97HOKA1a): interpretation1_variable: ‘I_E’ has been replaced by ‘hydrologicBalance’
    • d18O (LS97HOKA1a): interpretation2_variable: ‘T_water’ has been replaced by ‘temperature’
    • d18O (LS97HOKA1a): interpretation3_variable: ‘P_isotope’ has been replaced by ‘precipitationIsotope’

Version: 1.0.1

• lastVersion: 1.0.0
• curator: nicholas
• timestamp: 2025-04-08 17:33:02.982153 UTC
• notes: Changes made as part of LiPDverse vocabulary standardization process
• changes:
  • Paleo Column metadata:
    • d18O (LS97HOKA1a): paleoData_longName: NULL has been replaced by ‘AD’
    • year (MAT5a83d3ba3b): paleoData_units: ‘AD’ has been replaced by ‘yr AD’
    • year (MAT5a83d3ba3b): paleoData_longName: NULL has been replaced by ‘AD’
    • depth (MATeb6bfe7013): paleoData_longName: NULL has been replaced by ‘AD’