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 has been replaced by ''
d18O (LS97HOKA1a): interpretation1_direction: 'negative' has been replaced by ''
d18O (LS97HOKA1a): interpretation1_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS97HOKA1a): interpretation1_rank: '1' has been replaced by ''
d18O (LS97HOKA1a): interpretation1_scope: 'isotope' has been replaced by 'climate'
d18O (LS97HOKA1a): interpretation1_variable: 'hydrologicBalance' has been replaced by ''
d18O (LS97HOKA1a): interpretation1_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (LS97HOKA1a): interpretation1_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS97HOKA1a): interpretation1_variableGroupOriginal: 'I_E' has been replaced by ''
d18O (LS97HOKA1a): interpretation2_direction: 'negative' has been replaced by ''
d18O (LS97HOKA1a): interpretation2_inferredMaterial: 'Lake water' has been replaced by ''
d18O (LS97HOKA1a): interpretation2_rank: '2' has been replaced by ''
d18O (LS97HOKA1a): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (LS97HOKA1a): interpretation2_variable: 'temperature' has been replaced by ''
d18O (LS97HOKA1a): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (LS97HOKA1a): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS97HOKA1a): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
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 has been replaced by ''
d18O (LS97HOKA1a): interpretation3_inferredMaterial: 'Lake water' has been replaced by ''
d18O (LS97HOKA1a): interpretation3_rank: '3' has been replaced by ''
d18O (LS97HOKA1a): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (LS97HOKA1a): interpretation3_variable: 'precipitationIsotope' has been replaced by ''
d18O (LS97HOKA1a): interpretation3_variableGroup: 'P_isotope' has been replaced by ''
d18O (LS97HOKA1a): interpretation3_variableGroupDirection: 'positive' has been replaced by ''
d18O (LS97HOKA1a): interpretation4_basis: '' 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: '' has been replaced by 'negative'
d18O (LS97HOKA1a): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS97HOKA1a): interpretation4_rank: '' has been replaced by '1'
d18O (LS97HOKA1a): interpretation4_scope: '' has been replaced by 'isotope'
d18O (LS97HOKA1a): interpretation4_variable: '' has been replaced by 'hydrologicBalance'
d18O (LS97HOKA1a): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (LS97HOKA1a): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS97HOKA1a): interpretation4_variableGroupOriginal: '' has been replaced by 'I_E'
d18O (LS97HOKA1a): interpretation5_direction: '' has been replaced by 'negative'
d18O (LS97HOKA1a): interpretation5_inferredMaterial: '' has been replaced by 'Lake water'
d18O (LS97HOKA1a): interpretation5_rank: '' has been replaced by '2'
d18O (LS97HOKA1a): interpretation5_scope: '' has been replaced by 'isotope'
d18O (LS97HOKA1a): interpretation5_variable: '' has been replaced by 'temperature'
d18O (LS97HOKA1a): interpretation5_variableGroup: '' has been replaced by 'Temperature'
d18O (LS97HOKA1a): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS97HOKA1a): interpretation5_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (LS97HOKA1a): interpretation6_basis: '' 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: '' has been replaced by 'Lake water'
d18O (LS97HOKA1a): interpretation6_rank: '' has been replaced by '3'
d18O (LS97HOKA1a): interpretation6_scope: '' has been replaced by 'isotope'
d18O (LS97HOKA1a): interpretation6_variable: '' has been replaced by 'precipitationIsotope'
d18O (LS97HOKA1a): interpretation6_variableGroup: '' has been replaced by 'P_isotope'
d18O (LS97HOKA1a): interpretation6_variableGroupDirection: '' has been replaced by 'positive'
year (MAT5a83d3ba3b): interpretation1_scope: '' has been replaced by 'climate'
year (MAT5a83d3ba3b): interpretation2_scope: '' has been replaced by 'climate'
year (MAT5a83d3ba3b): interpretation3_scope: '' has been replaced by 'climate'
depth (MATeb6bfe7013): interpretation1_scope: '' has been replaced by 'climate'
depth (MATeb6bfe7013): interpretation2_scope: '' has been replaced by 'climate'
depth (MATeb6bfe7013): interpretation3_scope: '' has been replaced by 'climate'