d18O (SP08HUCN01A): interpretation1_seasonality: 'mostly summer' has been replaced by 'Summer'
d18O (SP08HUCN01A): interpretation1_variable: 'P' has been replaced by 'precipitation'
d18O (SP08HUCN01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'
d13C (SP08HUCN01A_d13C): interpretation1_variable: 'composition C3-C4 plants' has been replaced by 'C3C4Ratio'

d18O (SP08HUCN01A): interpretation1_seasonality: 'mostly summer' has been replaced by 'Summer'
d18O (SP08HUCN01A): interpretation1_variable: 'P' has been replaced by 'precipitation'
d18O (SP08HUCN01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'
d13C (SP08HUCN01A_d13C): interpretation1_variable: 'composition C3-C4 plants' has been replaced by 'C3C4Ratio'

year (MAT7a842ea1ae): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT7a842ea1ae): paleoData_longName: '' has been replaced by 'AD'
depth (MATb424a884a8): paleoData_longName: '' has been replaced by 'AD'
d18O (SP08HUCN01A): paleoData_longName: '' has been replaced by 'AD'
d13C (SP08HUCN01A_d13C): paleoData_longName: '' has been replaced by 'AD'

d18O (SP08HUCN01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP08HUCN01A): interpretation4_scope: '' has been replaced by 'isotope'
d13C (SP08HUCN01A_d13C): interpretation2_scope: '' has been replaced by 'isotope'
d13C (SP08HUCN01A_d13C): interpretation3_scope: '' has been replaced by 'isotope'

Hu, C., Henderson, G. M., Huang, J., Xie, S., Sun, Y. and Johnson, K. R.: Quantification of Holocene Asian monsoon rainfall from spatially separated cave records, Earth and Planetary Science Letters, 266(3-4), 221–232, doi:10.1016/j.epsl.2007.10.015, 2008.

GasBench II coupled to a ThermoFinnigan DeltaPlusXP isotope ratio mass spectrometer

Both Sr/Ca and d13C show correlated values

Lower precipitation produces higher d13C and Sr/Ca values

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