Search Results for: Temporal And Spatial Controls On Cave Water And Speleothem Calcite Isotopic And Elemental Chemistry Central Texas

The isotopic and elemental composition of speleothem calcite precipitated from dripwaters in caves have been used to elucidate changes in karst groundwater flow

There is the potential for bias in the speleothem paleoclimate record due to fluctuations in speleothem growth. A previous study in three central Texas tourist

Speleothem calcite growth rate is a commonly used paleoclimate proxy. Seasonal variations in cave CO2 concentration (P[subscript CO2]) are known to control spel