Abstract
Several small caves located in the southwestern part of the South Carpathians discharge steam or/and chloride-rich hot groundwater derived from a geothermal reservoir situated nearby. The monitoring of natural tracers (heat, certain solutes, stable isotopes) documented uncommon levels for the fluids discharged within the Băile Herculane caves, thus revealing flow processes that ordinary meteoric-derived groundwater would be unable to depict. Furthermore, the exotic cave minerals and their isotopic composition suggest that the caves are the result of combination of hypogene and epigene processes. A rich and peculiar endemic troglobite fauna was identified in the Adam’s Shaft, in which a guano accumulation dated to ~8425 cal yrs BP suggests it is one of Europe’s oldest permanent bat colonies. The unusual warm/wet microclimate of the cave favored both an ideal roosting site for bats and a “tropical” biospeleological oasis.
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Acknowledgements
Parts of this work were supported by grants from the Romanian National Authority for Scientific Research, CNDI-UEFISCDI; PN-II-PT-PCCA-2011-3.1-1619 to MC and ID_544 to BPO). For their dedicated assistance provided during the field operations, Elisabeta Primejdie and Socrate Bucur are gratefully acknowledged. We also thank Floarea Răducă for her continuing support in the laboratory work and Dr. Victor Polyak for providing the U-series ages on gypsum speleothems.
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Povară, I. et al. (2019). Cernei Mountains: Caves Conveying Geothermal Fluids at Băile Herculane. In: Ponta, G., Onac, B. (eds) Cave and Karst Systems of Romania. Cave and Karst Systems of the World. Springer, Cham. https://doi.org/10.1007/978-3-319-90747-5_25
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