APPLICATION OF MODERN CAVE DRIPWATER GEOCHEMISTRY TO UNDERSTANDING SEASONAL CHANGES IN MINERAL-SOLUTION REACTIONS: IMPLICATIONS FOR RECONSTRUCTING PALEOCLIMATE FROM SPELEOTHEMS
Geochemical modeling indicates that drip-water geochemical evolution is controlled by a combination of PCP and water-rock interaction (WRI), with PCP dominating during the summer. 87Sr/86Sr values for all sites range from 0.70846-0.70856, which is similar to values for soils and higher than values for the host Cretaceous limestones. The largest range of 87Sr/86Sr at any of the sites is 0.000035, which is similar to the analytical uncertainty. Sr isotopes will undergo negligible fractionation during mineral precipitation from solution, whereas mineral dissolution during WRI will evolve solution 87Sr/86Sr values. Therefore, the essentially invariant Sr isotope variability at each drip site is consistent with PCP as the primary control. Drip-site location also appears to play a role in drip-water geochemistry, as 87Sr/86Sr values vary between sites. This may be due to either the heterogeneity of soil above the cave, or varying flow paths of the water feeding the sites. Further studies of the host limestone and soils may constrain the origin of the local differences. Co- variations of trace elements and Sr isotope compositions may be applicable to speleothems as proxies for seasonal changes in temperature, the extent of different mineral-solution reactions, and the sources of dissolved ions.