d18O (SP12CACN01A): interpretation2_basis: 'A low correlation between δ13C and δ18O values (r2=0.133) argues against kinetically driven fractionation during speleothem growth according to traditional Hendy criteria. This suggests that the speleothem most likely grew under isotopic equilibrium conditions. Fluctuations in δ18O values result mainly from changes in δ18O value of the drip water. In low latitude areas, the “amount effect”, i.e. a relationship where the δ18O of meteoric precipitation is negatively correlated with precipitation amount, is the major controlling factor of precipitation δ18O (Dansgaard, 1964; Rozanski et al., 1993) and often overshadows the dependence of δ18O on temperature in Asian monsoon regions (Araguas-Araguas et al., 1998, Wei and Gasse, 1999).' has been replaced by ''
d18O (SP12CACN01A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP12CACN01A): interpretation2_equilibriumEvidence: 'equilibrium is evidenced by (1) the lack of correlation among d18O and d13C, (2) the application of fractionation equation with current d18O values in dripwaters and cave temperature and (3) replication with other caves' has been replaced by ''
d18O (SP12CACN01A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''
d18O (SP12CACN01A): interpretation2_integrationTime: 'from 3 to 7' has been replaced by ''
d18O (SP12CACN01A): interpretation2_integrationTimeBasis: 'age model' has been replaced by ''
d18O (SP12CACN01A): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (SP12CACN01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP12CACN01A): interpretation2_seasonality: 'Jun-Sep' has been replaced by ''
d18O (SP12CACN01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP12CACN01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP12CACN01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP12CACN01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP12CACN01A): interpretation4_basis: '' has been replaced by 'A low correlation between δ13C and δ18O values (r2=0.133) argues against kinetically driven fractionation during speleothem growth according to traditional Hendy criteria. This suggests that the speleothem most likely grew under isotopic equilibrium conditions. Fluctuations in δ18O values result mainly from changes in δ18O value of the drip water. In low latitude areas, the “amount effect”, i.e. a relationship where the δ18O of meteoric precipitation is negatively correlated with precipitation amount, is the major controlling factor of precipitation δ18O (Dansgaard, 1964; Rozanski et al., 1993) and often overshadows the dependence of δ18O on temperature in Asian monsoon regions (Araguas-Araguas et al., 1998, Wei and Gasse, 1999).'
d18O (SP12CACN01A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP12CACN01A): interpretation4_equilibriumEvidence: '' has been replaced by 'equilibrium is evidenced by (1) the lack of correlation among d18O and d13C, (2) the application of fractionation equation with current d18O values in dripwaters and cave temperature and (3) replication with other caves'
d18O (SP12CACN01A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'
d18O (SP12CACN01A): interpretation4_integrationTime: '' has been replaced by 'from 3 to 7'
d18O (SP12CACN01A): interpretation4_integrationTimeBasis: '' has been replaced by 'age model'
d18O (SP12CACN01A): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (SP12CACN01A): interpretation4_seasonality: '' has been replaced by 'Jun-Sep'
d18O (SP12CACN01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP12CACN01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP12CACN01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP12CACN01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP12CACN01A): interpretation6_scope: '' has been replaced by 'isotope'