d13C (LPDe86e42a4d13c): interpretation1_scope: 'isotope' has been replaced by 'climate'
d13C (LPDe86e42a4d13c): interpretation1_variable: 'C3C4Ratio' has been replaced by ''
d13C (LPDe86e42a4d13c): interpretation1_variableGroup: 'composition C3-C4 plants' has been replaced by ''
d13C (LPDe86e42a4d13c): interpretation2_scope: 'isotope' has been replaced by 'climate'
d13C (LPDe86e42a4d13c): interpretation3_scope: 'isotope' has been replaced by 'climate'
d13C (LPDe86e42a4d13c): interpretation4_scope: '' has been replaced by 'isotope'
d13C (LPDe86e42a4d13c): interpretation4_variable: '' has been replaced by 'C3C4Ratio'
d13C (LPDe86e42a4d13c): interpretation4_variableGroup: '' has been replaced by 'composition C3-C4 plants'
d13C (LPDe86e42a4d13c): interpretation5_scope: '' has been replaced by 'isotope'
d13C (LPDe86e42a4d13c): interpretation6_scope: '' has been replaced by 'isotope'
d18O (SP08SPUS01A): interpretation2_basis: 'Sr/Ca ratios can be used to reconstruct relative rates of epikarstic moisture transport because low moisture levels can cause 1) increased drip water residence times, leading to 2) Ca drawdown via calcite precipitation in the overlying epikarst, which increases Sr/Ca ratios in the residual drip waters and their dependent speleothems' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_equilibriumEvidence: 'deep cave location' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_rank: '1' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP08SPUS01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP08SPUS01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP08SPUS01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP08SPUS01A): interpretation4_rank: '' has been replaced by '1'
d18O (SP08SPUS01A): interpretation4_basis: '' has been replaced by 'Sr/Ca ratios can be used to reconstruct relative rates of epikarstic moisture transport because low moisture levels can cause 1) increased drip water residence times, leading to 2) Ca drawdown via calcite precipitation in the overlying epikarst, which increases Sr/Ca ratios in the residual drip waters and their dependent speleothems'
d18O (SP08SPUS01A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP08SPUS01A): interpretation4_equilibriumEvidence: '' has been replaced by 'deep cave location'
d18O (SP08SPUS01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d18O (SP08SPUS01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d18O (SP08SPUS01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP08SPUS01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP08SPUS01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP08SPUS01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP08SPUS01A): interpretation6_scope: '' has been replaced by 'isotope'