d2H (LS14ATJU01A): interpretation1_basis: 'In closed (endorheic) lakes, lake water dD is driven by the ratio of precipitation to evaporation and the isotopic value of the precipitation which, in the tropics, is strongly negatively correlated with the amount of precipitation on monthly and longer timescales. The combination of these processes amplifies the response of lake water dD to changes in rainfall with lower (higher) dD values occurring during periods of wetter (drier) conditions. Changes in rainfall patterns can therefore be reconstructed from dD values of sedimentary algal lipids, due to the near perfect correlation between water dD and algal lipid dD values.' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_direction: 'negative' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_rank: '1' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_scope: 'isotope' has been replaced by 'climate'
d2H (LS14ATJU01A): interpretation1_seasonality: 'Annual' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_variable: 'effectivePrecipitation' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS14ATJU01A): interpretation1_variableGroupOriginal: 'P_E' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_basis: '"In closed (endorheic) lakes, lake water dD is driven by the ratio of precipitation to evaporation and the isotopic value of the precipitation which, in the tropics, is strongly negatively correlated with the amount of precipitation on monthly and longer timescales. The combination of these processes amplifies the response of lake water dD to changes in rainfall with lower (higher) dD values occurring during periods of wetter (drier) conditions. Changes in rainfall patterns can therefore be reconstructed from dD values of sedimentary algal lipids, due to the near perfect correlation between water dD and algal lipid dD values."' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_rank: '2' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS14ATJU01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS14ATJU01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS14ATJU01A): interpretation3_scope: '' has been replaced by 'climate'
d2H (LS14ATJU01A): interpretation4_basis: '' has been replaced by 'In closed (endorheic) lakes, lake water dD is driven by the ratio of precipitation to evaporation and the isotopic value of the precipitation which, in the tropics, is strongly negatively correlated with the amount of precipitation on monthly and longer timescales. The combination of these processes amplifies the response of lake water dD to changes in rainfall with lower (higher) dD values occurring during periods of wetter (drier) conditions. Changes in rainfall patterns can therefore be reconstructed from dD values of sedimentary algal lipids, due to the near perfect correlation between water dD and algal lipid dD values.'
d2H (LS14ATJU01A): interpretation4_direction: '' has been replaced by 'negative'
d2H (LS14ATJU01A): interpretation4_rank: '' has been replaced by '1'
d2H (LS14ATJU01A): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS14ATJU01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS14ATJU01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS14ATJU01A): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d2H (LS14ATJU01A): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS14ATJU01A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS14ATJU01A): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d2H (LS14ATJU01A): interpretation5_basis: '' has been replaced by '"In closed (endorheic) lakes, lake water dD is driven by the ratio of precipitation to evaporation and the isotopic value of the precipitation which, in the tropics, is strongly negatively correlated with the amount of precipitation on monthly and longer timescales. The combination of these processes amplifies the response of lake water dD to changes in rainfall with lower (higher) dD values occurring during periods of wetter (drier) conditions. Changes in rainfall patterns can therefore be reconstructed from dD values of sedimentary algal lipids, due to the near perfect correlation between water dD and algal lipid dD values."'
d2H (LS14ATJU01A): interpretation5_direction: '' has been replaced by 'positive'
d2H (LS14ATJU01A): interpretation5_rank: '' has been replaced by '2'
d2H (LS14ATJU01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14ATJU01A): interpretation5_seasonality: '' has been replaced by 'Annual'
d2H (LS14ATJU01A): interpretation5_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS14ATJU01A): interpretation5_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS14ATJU01A): interpretation5_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS14ATJU01A): interpretation5_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS14ATJU01A): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS14ATJU01B): interpretation2_basis: 'All botryococcene dD values were highly correlated with water dD values (R2>0.99). And, Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_integrationTime: '1 to 10' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_integrationTimeBasis: 'These lines of evidence strongly suggest that conditions favor- able for B. braunii growth occur during moderate-to-strong El Nin?o events and thus that C34 botryococcene ?D records the hydrologic conditions of the lake during these events. In contrast, the avail- able evidence suggests that the dinoflagellate population persists throughout the varying hydrologic conditions experienced by El Junco Lake and thus that sedimentary dinosterol ?D records the long-term (decadal-to-centennial) mean lake conditions.' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS14ATJU01B): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS14ATJU01B): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_basis: 'changes in rainfall amount are imprinted in the isotopic composition of botryococcenes, with negative (posi- tive) ?D values co-occurring with wetter (drier) periods.' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_direction: 'negative' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_inferredMaterial: 'lake water' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_integrationTime: '1 to 10' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_integrationTimeBasis: 'These lines of evidence strongly suggest that conditions favor- able for B. braunii growth occur during moderate-to-strong El Nin?o events and thus that C34 botryococcene ?D records the hydrologic conditions of the lake during these events. In contrast, the avail- able evidence suggests that the dinoflagellate population persists throughout the varying hydrologic conditions experienced by El Junco Lake and thus that sedimentary dinosterol ?D records the long-term (decadal-to-centennial) mean lake conditions.' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_integrationTimeUnits: 'years' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS14ATJU01B): interpretation3_seasonality: 'Annual' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_variable: 'effectivePrecipitation' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS14ATJU01B): interpretation3_variableGroupOriginal: 'P_E' has been replaced by ''
d2H (LS14ATJU01B): interpretation4_basis: '' has been replaced by 'All botryococcene dD values were highly correlated with water dD values (R2>0.99). And, Zhang and Sachs 2007, Organic Geochemistry, 38: 582-608.'
d2H (LS14ATJU01B): interpretation4_direction: '' has been replaced by 'positive'
d2H (LS14ATJU01B): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d2H (LS14ATJU01B): interpretation4_integrationTime: '' has been replaced by '1 to 10'
d2H (LS14ATJU01B): interpretation4_integrationTimeBasis: '' has been replaced by 'These lines of evidence strongly suggest that conditions favor- able for B. braunii growth occur during moderate-to-strong El Nin?o events and thus that C34 botryococcene ?D records the hydrologic conditions of the lake during these events. In contrast, the avail- able evidence suggests that the dinoflagellate population persists throughout the varying hydrologic conditions experienced by El Junco Lake and thus that sedimentary dinosterol ?D records the long-term (decadal-to-centennial) mean lake conditions.'
d2H (LS14ATJU01B): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d2H (LS14ATJU01B): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d2H (LS14ATJU01B): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS14ATJU01B): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS14ATJU01B): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS14ATJU01B): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS14ATJU01B): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS14ATJU01B): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS14ATJU01B): interpretation5_basis: '' has been replaced by 'changes in rainfall amount are imprinted in the isotopic composition of botryococcenes, with negative (posi- tive) ?D values co-occurring with wetter (drier) periods.'
d2H (LS14ATJU01B): interpretation5_direction: '' has been replaced by 'negative'
d2H (LS14ATJU01B): interpretation5_inferredMaterial: '' has been replaced by 'lake water'
d2H (LS14ATJU01B): interpretation5_integrationTime: '' has been replaced by '1 to 10'
d2H (LS14ATJU01B): interpretation5_integrationTimeBasis: '' has been replaced by 'These lines of evidence strongly suggest that conditions favor- able for B. braunii growth occur during moderate-to-strong El Nin?o events and thus that C34 botryococcene ?D records the hydrologic conditions of the lake during these events. In contrast, the avail- able evidence suggests that the dinoflagellate population persists throughout the varying hydrologic conditions experienced by El Junco Lake and thus that sedimentary dinosterol ?D records the long-term (decadal-to-centennial) mean lake conditions.'
d2H (LS14ATJU01B): interpretation5_integrationTimeUnits: '' has been replaced by 'years'
d2H (LS14ATJU01B): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d2H (LS14ATJU01B): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14ATJU01B): interpretation5_seasonality: '' has been replaced by 'Annual'
d2H (LS14ATJU01B): interpretation5_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS14ATJU01B): interpretation5_variable: '' has been replaced by 'effectivePrecipitation'
d2H (LS14ATJU01B): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS14ATJU01B): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS14ATJU01B): interpretation5_variableGroupOriginal: '' has been replaced by 'P_E'
d2H (LS14ATJU01B): interpretation6_scope: '' has been replaced by 'isotope'
depth (MAT6c43cd5d85): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT6c43cd5d85): interpretation2_scope: '' has been replaced by 'climate'
year (MAT795501f3aa): interpretation1_scope: '' has been replaced by 'climate'
year (MAT795501f3aa): interpretation2_scope: '' has been replaced by 'climate'