d18O (LS09LAEL): interpretation2_basis: 'The oxygen isotope composition of ostracod carapaces depends primarily on the d18O composition of the water and the tempera- ture at which carbonates precipitate (Craig, 1965; Stuiver, 1970). In tropical, closed-basin lakes within seasonally dry climates, the d18O value of lake water is controlled primarily by the evaporation to precipitation ratio (E/P) of the lake (Fontes and Gonfiantini, 1967; Gasse et al., 1990). During periods of increased (decreased) E/P ratios, the d18O value of lake water will go up (down) as kinetic fractionation processes lead to an increase (decrease) in concen- trations of 18O relative to 16O. Assuming that long-term tempera- ture changes in the tropics are less likely to affect d18O values in the lake than are changes in the E/P ratio (Covich and Stuiver, 1974; Curtis and Hodell, 1993), the d18O value of ostracod carapaces should indicate variations in the E/P ratio of the lake.' has been replaced by ''
d18O (LS09LAEL): interpretation2_direction: 'negative' has been replaced by ''
d18O (LS09LAEL): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS09LAEL): interpretation2_integrationTimeUncertaintyType: 'chronology; hydrology; seasonality; habitat; vital effects' has been replaced by ''
d18O (LS09LAEL): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (LS09LAEL): interpretation2_rank: '1' has been replaced by ''
d18O (LS09LAEL): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (LS09LAEL): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (LS09LAEL): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (LS09LAEL): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS09LAEL): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (LS09LAEL): interpretation3_scope: '' has been replaced by 'climate'
d18O (LS09LAEL): interpretation4_basis: '' has been replaced by 'The oxygen isotope composition of ostracod carapaces depends primarily on the d18O composition of the water and the tempera- ture at which carbonates precipitate (Craig, 1965; Stuiver, 1970). In tropical, closed-basin lakes within seasonally dry climates, the d18O value of lake water is controlled primarily by the evaporation to precipitation ratio (E/P) of the lake (Fontes and Gonfiantini, 1967; Gasse et al., 1990). During periods of increased (decreased) E/P ratios, the d18O value of lake water will go up (down) as kinetic fractionation processes lead to an increase (decrease) in concen- trations of 18O relative to 16O. Assuming that long-term tempera- ture changes in the tropics are less likely to affect d18O values in the lake than are changes in the E/P ratio (Covich and Stuiver, 1974; Curtis and Hodell, 1993), the d18O value of ostracod carapaces should indicate variations in the E/P ratio of the lake.'
d18O (LS09LAEL): interpretation4_direction: '' has been replaced by 'negative'
d18O (LS09LAEL): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS09LAEL): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronology; hydrology; seasonality; habitat; vital effects'
d18O (LS09LAEL): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (LS09LAEL): interpretation4_rank: '' has been replaced by '1'
d18O (LS09LAEL): interpretation4_scope: '' has been replaced by 'isotope'
d18O (LS09LAEL): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (LS09LAEL): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (LS09LAEL): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS09LAEL): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (LS09LAEL): interpretation5_scope: '' has been replaced by 'isotope'
d18O (LS09LAEL): interpretation6_scope: '' has been replaced by 'isotope'
year (MAT47cd7c60d5): interpretation1_scope: '' has been replaced by 'climate'
year (MAT47cd7c60d5): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT6cf2a17f91): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT6cf2a17f91): interpretation2_scope: '' has been replaced by 'climate'