d2H (LPD292174f8): interpretation1_direction: 'negative' has been replaced by ''
d2H (LPD292174f8): interpretation1_mathematicalRelation: 'linear' has been replaced by ''
d2H (LPD292174f8): interpretation1_scope: 'isotope' has been replaced by 'climate'
d2H (LPD292174f8): interpretation1_variable: 'hydrologicBalance' has been replaced by ''
d2H (LPD292174f8): interpretation1_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LPD292174f8): interpretation1_variableGroupDirection: 'negative' has been replaced by ''
d2H (LPD292174f8): interpretation1_variableGroupOriginal: 'I_E' has been replaced by ''
d2H (LPD292174f8): interpretation2_scope: '' has been replaced by 'climate'
d2H (LPD292174f8): interpretation3_scope: '' has been replaced by 'climate'
d2H (LPD292174f8): interpretation4_direction: '' has been replaced by 'negative'
d2H (LPD292174f8): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LPD292174f8): interpretation4_variable: '' has been replaced by 'hydrologicBalance'
d2H (LPD292174f8): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LPD292174f8): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d2H (LPD292174f8): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d2H (LPD292174f8): interpretation4_variableGroupOriginal: '' has been replaced by 'I_E'
d2H (LPD292174f8): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LPD292174f8): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS09SASP01A): interpretation2_basis: 'Permanent anoxia in the subsurface water confines phytoplankton, dominated by dinoflagellates and diatoms24, to the oxygenated, brackish and deuterium-depleted surface water where their lipid ?D values can be expected to closely co-vary with the surface water ?Dvalues25,26. ?D values of that water are controlled by the amount of rainfall, its isotopic composition and the amount of mixing with the underlying sea water. As rain also increases the density stratification in the lakes, decreasing mixing, surface water ?D values are expected to be significantly lower during wet periods compared with dry periods.  Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.' has been replaced by ''
d2H (LS09SASP01A): interpretation2_direction: 'negative' has been replaced by ''
d2H (LS09SASP01A): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d2H (LS09SASP01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS09SASP01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS09SASP01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS09SASP01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS09SASP01A): interpretation2_variable: 'precipitation' has been replaced by ''
d2H (LS09SASP01A): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS09SASP01A): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS09SASP01A): interpretation2_variableGroupOriginal: 'P_amount' has been replaced by ''
d2H (LS09SASP01A): interpretation3_basis: 'Permanent anoxia in the subsurface water confines phytoplankton, dominated by dinoflagellates and diatoms24, to the oxygenated, brackish and deuterium-depleted surface water where their lipid ?D values can be expected to closely co-vary with the surface water ?Dvalues25,26. ?D values of that water are controlled by the amount of rainfall, its isotopic composition and the amount of mixing with the underlying sea water. As rain also increases the density stratification in the lakes, decreasing mixing, surface water ?D values are expected to be significantly lower during wet periods compared with dry periods.  Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.' has been replaced by ''
d2H (LS09SASP01A): interpretation3_direction: 'depends on source, transport history, etc' has been replaced by ''
d2H (LS09SASP01A): interpretation3_inferredMaterial: 'lake water' has been replaced by ''
d2H (LS09SASP01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS09SASP01A): interpretation3_seasonality: 'Annual' has been replaced by ''
d2H (LS09SASP01A): interpretation3_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS09SASP01A): interpretation3_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS09SASP01A): interpretation3_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS09SASP01A): interpretation3_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS09SASP01A): interpretation3_variableGroupOriginal: 'rainfall d2H' has been replaced by ''
d2H (LS09SASP01A): interpretation4_basis: 'Permanent anoxia in the subsurface water confines phytoplankton, dominated by dinoflagellates and diatoms24, to the oxygenated, brackish and deuterium-depleted surface water where their lipid dD values can be expected to closely co-vary with the surface water dDvalues25,26. dD values of that water are controlled by the amount of rainfall, its isotopic composition and the amount of mixing with the underlying sea water. As rain also increases the density stratification in the lakes, decreasing mixing, surface water dD values are expected to be significantly lower during wet periods compared with dry periods.  Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.' has been replaced by 'Permanent anoxia in the subsurface water confines phytoplankton, dominated by dinoflagellates and diatoms24, to the oxygenated, brackish and deuterium-depleted surface water where their lipid ?D values can be expected to closely co-vary with the surface water ?Dvalues25,26. ?D values of that water are controlled by the amount of rainfall, its isotopic composition and the amount of mixing with the underlying sea water. As rain also increases the density stratification in the lakes, decreasing mixing, surface water ?D values are expected to be significantly lower during wet periods compared with dry periods.  Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.'
d2H (LS09SASP01A): interpretation4_direction: 'positive (more mixing, higher d2H in surface waters)' has been replaced by 'negative'
d2H (LS09SASP01A): interpretation4_variable: 'lakeWaterIsotope' has been replaced by 'precipitation'
d2H (LS09SASP01A): interpretation4_variableGroup: 'mixing with sea water which is in bottom of meromictic lake' has been replaced by 'EffectiveMoisture'
d2H (LS09SASP01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d2H (LS09SASP01A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS09SASP01A): interpretation4_variableGroupOriginal: '' has been replaced by 'P_amount'
d2H (LS09SASP01A): interpretation5_basis: '' has been replaced by 'Permanent anoxia in the subsurface water confines phytoplankton, dominated by dinoflagellates and diatoms24, to the oxygenated, brackish and deuterium-depleted surface water where their lipid ?D values can be expected to closely co-vary with the surface water ?Dvalues25,26. ?D values of that water are controlled by the amount of rainfall, its isotopic composition and the amount of mixing with the underlying sea water. As rain also increases the density stratification in the lakes, decreasing mixing, surface water ?D values are expected to be significantly lower during wet periods compared with dry periods.  Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.'
d2H (LS09SASP01A): interpretation5_direction: '' has been replaced by 'depends on source, transport history, etc'
d2H (LS09SASP01A): interpretation5_inferredMaterial: '' has been replaced by 'lake water'
d2H (LS09SASP01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS09SASP01A): interpretation5_seasonality: '' has been replaced by 'Annual'
d2H (LS09SASP01A): interpretation5_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS09SASP01A): interpretation5_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS09SASP01A): interpretation5_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS09SASP01A): interpretation5_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS09SASP01A): interpretation5_variableGroupOriginal: '' has been replaced by 'rainfall d2H'
d2H (LS09SASP01A): interpretation6_basis: '' has been replaced by 'Permanent anoxia in the subsurface water confines phytoplankton, dominated by dinoflagellates and diatoms24, to the oxygenated, brackish and deuterium-depleted surface water where their lipid dD values can be expected to closely co-vary with the surface water dDvalues25,26. dD values of that water are controlled by the amount of rainfall, its isotopic composition and the amount of mixing with the underlying sea water. As rain also increases the density stratification in the lakes, decreasing mixing, surface water dD values are expected to be significantly lower during wet periods compared with dry periods.  Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.'
d2H (LS09SASP01A): interpretation6_direction: '' has been replaced by 'positive (more mixing, higher d2H in surface waters)'
d2H (LS09SASP01A): interpretation6_inferredMaterial: '' has been replaced by 'lake water'
d2H (LS09SASP01A): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS09SASP01A): interpretation6_seasonality: '' has been replaced by 'Annual'
d2H (LS09SASP01A): interpretation6_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS09SASP01A): interpretation6_variable: '' has been replaced by 'lakeWaterIsotope'
d2H (LS09SASP01A): interpretation6_variableGroup: '' has been replaced by 'mixing with sea water which is in bottom of meromictic lake'