year (MAT36170f341f): interpretation1_scope: '' has been replaced by 'climate'
year (MAT36170f341f): interpretation2_scope: '' has been replaced by 'climate'
year (MAT36170f341f): interpretation3_scope: '' has been replaced by 'climate'
depth (MATade0778ee9): interpretation1_scope: '' has been replaced by 'climate'
depth (MATade0778ee9): interpretation2_scope: '' has been replaced by 'climate'
depth (MATade0778ee9): interpretation3_scope: '' has been replaced by 'climate'
d18O (SP13LAMX01A): interpretation2_basis: 'The stalagmite ?18O values also contain a temperature imprint: a decrease in LST of ?3?4 i¿½C is responsible for making the stalagmite ?18O values higher by ?0.6?0.8% due to the water?carbonate precipitation temperature' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_equilibriumEvidence: 'The stalagmite ?18O values for the Mexican samples replicate very well over the common time intervals (Fig. S2), suggesting the values have not been significantly affected by kinetic effects, a conclusion that is further supported by an observation of apparent equilibrium isotopic relationships between drip-water samples and modern aragonite precipitating in the cave.' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_integrationTimeBasis: 'U/Th dating' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_integrationTimeUncertainty: 'A 0.5-or 1.0-mm sampling interval corresponds to a temporal resolution of ?2 y for the last 2 ka, 10?12 y for the LGM, HS1, and YD, and ?60 y for the Holocene.' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_rank: '1' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP13LAMX01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP13LAMX01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP13LAMX01A): interpretation3_direction: 'negative' has been replaced by ''
d18O (SP13LAMX01A): interpretation3_rank: '2' has been replaced by ''
d18O (SP13LAMX01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP13LAMX01A): interpretation3_variable: 'temperature' has been replaced by ''
d18O (SP13LAMX01A): interpretation3_variableGroup: 'Temperature' has been replaced by ''
d18O (SP13LAMX01A): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (SP13LAMX01A): interpretation3_variableGroupOriginal: 'Temperature_air' has been replaced by ''
d18O (SP13LAMX01A): interpretation4_rank: '' has been replaced by '1'
d18O (SP13LAMX01A): interpretation4_basis: '' has been replaced by 'The stalagmite ?18O values also contain a temperature imprint: a decrease in LST of ?3?4 i¿½C is responsible for making the stalagmite ?18O values higher by ?0.6?0.8% due to the water?carbonate precipitation temperature'
d18O (SP13LAMX01A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP13LAMX01A): interpretation4_equilibriumEvidence: '' has been replaced by 'The stalagmite ?18O values for the Mexican samples replicate very well over the common time intervals (Fig. S2), suggesting the values have not been significantly affected by kinetic effects, a conclusion that is further supported by an observation of apparent equilibrium isotopic relationships between drip-water samples and modern aragonite precipitating in the cave.'
d18O (SP13LAMX01A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'
d18O (SP13LAMX01A): interpretation4_integrationTimeBasis: '' has been replaced by 'U/Th dating'
d18O (SP13LAMX01A): interpretation4_integrationTimeUncertainty: '' has been replaced by 'A 0.5-or 1.0-mm sampling interval corresponds to a temporal resolution of ?2 y for the last 2 ka, 10?12 y for the LGM, HS1, and YD, and ?60 y for the Holocene.'
d18O (SP13LAMX01A): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (SP13LAMX01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (SP13LAMX01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d18O (SP13LAMX01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d18O (SP13LAMX01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP13LAMX01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP13LAMX01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP13LAMX01A): interpretation5_direction: '' has been replaced by 'negative'
d18O (SP13LAMX01A): interpretation5_rank: '' has been replaced by '2'
d18O (SP13LAMX01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP13LAMX01A): interpretation5_variable: '' has been replaced by 'temperature'
d18O (SP13LAMX01A): interpretation5_variableGroup: '' has been replaced by 'Temperature'
d18O (SP13LAMX01A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (SP13LAMX01A): interpretation5_variableGroupOriginal: '' has been replaced by 'Temperature_air'
d18O (SP13LAMX01A): interpretation6_scope: '' has been replaced by 'isotope'