Paper No. 10
Presentation Time: 10:30 AM


BOOP, Liana M.1, ONAC, Bogdan P.1, WYNN, Jonathan G.2, FORNÓS, Joan J.3, MERINO, Antoni4 and RODRÍGUEZ-HOMAR, Marta3, (1)Geology, University of South Florida, 4202 E. Fowler Ave, SCA 528, Tampa, FL 33620, (2)School of Geosciences, University of South Florida, 4202 E. Fowler Ave, SCA 528, NES 107, Tampa, FL 33620, (3)Earth Sciences, Universitat de les Illes Balears, Cra. Valldemossa, km. 7.5, Palma de Mallorca, 07071, Spain, (4)Federació Balear d'Espeleologia, C/ Margarida Xirgú, 16, Palma de Mallorca, 07011, Spain,

Mallorca’s phreatic overgrowths on speleothems (POS) are an ideal paleo-sea level proxy because they precipitate from brackish water in littoral caves, where the water table is coincident with sea level. POS are documented above, below, and at the current Mediterranean sea level and can be accurately dated using U-series techniques, thus precisely constraining the elevation of each sea-level stand.

POS mineralogy alternates between calcite and aragonite; sometimes both minerals occur within the same cave, but at different sea level stands. To determine the controls of aragonite/calcite precipitation, this study monitored an aragonite- and a calcite-precipitating site in Vallgornera and Drac caves, respectively. In the continuous aquatic (temperature, pH, and specific conductivity) and cave atmospheric (temperature and CO2) records, higher variability was recorded in Vallgornera, whereas Drac was more stable. CO2 levels were higher in Vallgornera (2,493 ppm maximum) than Drac (1,110 ppm maximum). While cave ventilation is more efficient in the latter cave, water pCO2 calculations (using total alkalinity and pH) indicate a greater CO2 concentration gradient from the cave water to the cave atmosphere, documenting the role of CO2 degassing.

Salinity ranged from 6.2 - 8.6 PSU in Drac, higher than the 5.5 - 6.5 PSU range observed in Vallgornera; this indicates a greater marine influence over the calcite-precipitating POS in Drac. Monthly cave water samples and vertical profiles indicate higher δ18O values and higher salinity with increasing depth, with the surface influenced by meteoric water. δ18O and salinity both trend toward the Mediterranean Sea endmember with depth in the caves.

Water samples collected from 0.2 m and 1.0 m depths in Drac show more positive δ13C values at the surface. Vertical δ13C profiles collected every 0.5 m show more positive values in the surface layer in Drac. δ13C profiles collected in Vallgornera did not have a positive offset at the surface. Monthly vertical pH profiles record similar results, with positive offsets of 0.5 – 1 pH unit at the water surface in Drac and only intermittently in Vallgornera. Combined with considerations of CO2 gradient between the cave water and atmosphere, it is evident that degassing is episodic in Vallgornera Cave, and more consistent in Drac Cave.