d18O (SP08HUCN01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP08HUCN01A): interpretation4_scope: '' has been replaced by 'isotope'
d13C (SP08HUCN01A_d13C): interpretation2_scope: '' has been replaced by 'isotope'
d13C (SP08HUCN01A_d13C): interpretation3_scope: '' has been replaced by 'isotope'

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

Springer, G. S., Rowe, H. D., Hardt, B., Edwards, R. L. and Cheng, H.: Solar forcing of Holocene droughts in a stalagmite record from West Virginia in east-central North America, Geophysical Research Letters, 35(17), doi:10.1029/2008gl034971, 2008.

d13C (LPDe86e42a4d13c): interpretation2_scope: '' has been replaced by 'isotope'
d13C (LPDe86e42a4d13c): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP08SPUS01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP08SPUS01A): interpretation4_scope: '' has been replaced by 'isotope'

AA (2019-03-08): Data is wonky (e.g. age ranges from -8E9 to 8E9). LCB: Time should cover the last 14k. MJ (30/12/19) there are two speleothems in the paper, one covers the last c. 4k, one from c. 4 to c. 14ka.

AA (2019-03-08): Data is wonky (e.g. age ranges from -8E9 to 8E9)

Fossil dripwater in stalagmites reveals Holocene temperature and rainfall variation in Amazonia

Van Breukelen, M. R., Vonhof, H. B., Hellstrom, J. C., Wester, W. C. G. and Kroon, D.: Fossil dripwater in stalagmites reveals Holocene temperature and rainfall variation in Amazonia, Earth and Planetary Science Letters, 275(1-2), 54–60, doi:10.1016/j.epsl.2008.07.060, 2008.