d2H (LS06SHBE01A): interpretation2_basis: 'match with pollen based January temperature, C16 n-acids are produced by aquatic plants, and ponds in this region are recharged mainly by winter precipitation' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_direction: 'negative' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_integrationTime: '1 to 2' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_integrationTimeBasis: 'lake equilibrium with the mean annual balance of precipitation and evaporation across the watershed' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS06SHBE01A): interpretation2_seasonality: 'Winter' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS06SHBE01A): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d2H (LS06SHBE01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS06SHBE01A): interpretation4_basis: '' has been replaced by 'match with pollen based January temperature, C16 n-acids are produced by aquatic plants, and ponds in this region are recharged mainly by winter precipitation'
d2H (LS06SHBE01A): interpretation4_direction: '' has been replaced by 'negative'
d2H (LS06SHBE01A): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d2H (LS06SHBE01A): interpretation4_integrationTime: '' has been replaced by '1 to 2'
d2H (LS06SHBE01A): interpretation4_integrationTimeBasis: '' has been replaced by 'lake equilibrium with the mean annual balance of precipitation and evaporation across the watershed'
d2H (LS06SHBE01A): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d2H (LS06SHBE01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d2H (LS06SHBE01A): interpretation4_seasonality: '' has been replaced by 'Winter'
d2H (LS06SHBE01A): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d2H (LS06SHBE01A): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS06SHBE01A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS06SHBE01A): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d2H (LS06SHBE01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS06SHBE01A): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS06SHBE01B): interpretation2_basis: 'Given the lack of correlation between dDlw and pollen- inferred mean July temperatures (Fig. 6), the downcore dDlw changes likely represent either a change in the ratio of soil water and precipitation utilized by the vegetation and/ or a change in source and pathway of regional precipita- tion. The dDlw data may indicate a heavy reliance of terrestrial plants on cool-season derived soil moisture from 11,000?8000 cal yr BP when conditions were dry. Growing- season precipitation may have been too low to provide sufficient water to the plants. An alternative and not mutually exclusive interpretation is that growing-season precipitation was not enriched in deuterium from 11,000?8000 cal yr BP because the presence of high pressure over the Laurentide ice sheet prevented the northward advection of humid, sub-tropical airmasses that are important for summer precipitation today. Both interpre- tations are consistent with Shuman and Donnelly?s (2006) interpretation that low lake levels prior to ca 8200 cal yr BP resulted from low summer precipitation rates and a high ratio of winter to summer precipitation.' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_mathematicalRelation: 'depends on the source area and transport path to the study site' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS06SHBE01B): interpretation2_seasonality: 'Summer' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_seasonalityOriginal: 'summer' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS06SHBE01B): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS06SHBE01B): interpretation3_basis: 'Given the lack of correlation between dDlw and pollen- inferred mean July temperatures (Fig. 6), the downcore dDlw changes likely represent either a change in the ratio of soil water and precipitation utilized by the vegetation and/ or a change in source and pathway of regional precipita- tion. The dDlw data may indicate a heavy reliance of terrestrial plants on cool-season derived soil moisture from 11,000?8000 cal yr BP when conditions were dry. Growing- season precipitation may have been too low to provide sufficient water to the plants. An alternative and not mutually exclusive interpretation is that growing-season precipitation was not enriched in deuterium from 11,000?8000 cal yr BP because the presence of high pressure over the Laurentide ice sheet prevented the northward advection of humid, sub-tropical airmasses that are important for summer precipitation today. Both interpre- tations are consistent with Shuman and Donnelly?s (2006) interpretation that low lake levels prior to ca 8200 cal yr BP resulted from low summer precipitation rates and a high ratio of winter to summer precipitation.' has been replaced by ''
d2H (LS06SHBE01B): interpretation3_direction: 'depends on which season provides source moisture for plants' has been replaced by ''
d2H (LS06SHBE01B): interpretation3_mathematicalRelation: 'depends on which season provides source moisture for plants' has been replaced by ''
d2H (LS06SHBE01B): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS06SHBE01B): interpretation3_seasonality: 'deleteMe' has been replaced by ''
d2H (LS06SHBE01B): interpretation3_variable: 'seasonality' has been replaced by ''
d2H (LS06SHBE01B): interpretation3_variableGroup: 'precipitation seasonality' has been replaced by ''
d2H (LS06SHBE01B): interpretation4_basis: '' has been replaced by 'Given the lack of correlation between dDlw and pollen- inferred mean July temperatures (Fig. 6), the downcore dDlw changes likely represent either a change in the ratio of soil water and precipitation utilized by the vegetation and/ or a change in source and pathway of regional precipita- tion. The dDlw data may indicate a heavy reliance of terrestrial plants on cool-season derived soil moisture from 11,000?8000 cal yr BP when conditions were dry. Growing- season precipitation may have been too low to provide sufficient water to the plants. An alternative and not mutually exclusive interpretation is that growing-season precipitation was not enriched in deuterium from 11,000?8000 cal yr BP because the presence of high pressure over the Laurentide ice sheet prevented the northward advection of humid, sub-tropical airmasses that are important for summer precipitation today. Both interpre- tations are consistent with Shuman and Donnelly?s (2006) interpretation that low lake levels prior to ca 8200 cal yr BP resulted from low summer precipitation rates and a high ratio of winter to summer precipitation.'
d2H (LS06SHBE01B): interpretation4_direction: '' has been replaced by 'positive'
d2H (LS06SHBE01B): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS06SHBE01B): interpretation4_mathematicalRelation: '' has been replaced by 'depends on the source area and transport path to the study site'
d2H (LS06SHBE01B): interpretation4_seasonality: '' has been replaced by 'Summer'
d2H (LS06SHBE01B): interpretation4_seasonalityOriginal: '' has been replaced by 'summer'
d2H (LS06SHBE01B): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS06SHBE01B): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS06SHBE01B): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS06SHBE01B): interpretation5_basis: '' has been replaced by 'Given the lack of correlation between dDlw and pollen- inferred mean July temperatures (Fig. 6), the downcore dDlw changes likely represent either a change in the ratio of soil water and precipitation utilized by the vegetation and/ or a change in source and pathway of regional precipita- tion. The dDlw data may indicate a heavy reliance of terrestrial plants on cool-season derived soil moisture from 11,000?8000 cal yr BP when conditions were dry. Growing- season precipitation may have been too low to provide sufficient water to the plants. An alternative and not mutually exclusive interpretation is that growing-season precipitation was not enriched in deuterium from 11,000?8000 cal yr BP because the presence of high pressure over the Laurentide ice sheet prevented the northward advection of humid, sub-tropical airmasses that are important for summer precipitation today. Both interpre- tations are consistent with Shuman and Donnelly?s (2006) interpretation that low lake levels prior to ca 8200 cal yr BP resulted from low summer precipitation rates and a high ratio of winter to summer precipitation.'
d2H (LS06SHBE01B): interpretation5_direction: '' has been replaced by 'depends on which season provides source moisture for plants'
d2H (LS06SHBE01B): interpretation5_mathematicalRelation: '' has been replaced by 'depends on which season provides source moisture for plants'
d2H (LS06SHBE01B): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS06SHBE01B): interpretation5_seasonality: '' has been replaced by 'deleteMe'
d2H (LS06SHBE01B): interpretation5_variable: '' has been replaced by 'seasonality'
d2H (LS06SHBE01B): interpretation5_variableGroup: '' has been replaced by 'precipitation seasonality'
d2H (LS06SHBE01B): interpretation6_scope: '' has been replaced by 'isotope'