Abstract
Cave monitoring was conducted in the Béke and Baradla caves in the Aggtelek Karst, in the Ajándék-Ariadne cave system in the Pilis Mountain, as well as in the Szemlőhegy and Pálvölgy caves in the Buda Mountain. Climatological data outside of the cave (e.g., temperature, amount of precipitation), within the cave (temperature, humidity, CO2 concentration), as well as the geochemical data of drip water (chemical and isotopic compositions) and carbonates (stable isotope compositions) were compiled in order to constrain the processes that influence the cave air, drip waters, and the precipitated carbonates. The monitoring activities in the Béke and Baradla caves revealed that the speleothems formed in these caves are able to record temperature and hydrological changes, and hence the measured trace element and isotopic compositions together with petrographic characteristics can be used to reconstruct past climate and environmental fluctuations. In addition, the equations that best describe the carbonate-water oxygen isotope fractionation and best reflect the temperature dependence of the isotopic composition of precipitations were identified for paleotemperature reconstruction. The investigations conducted in the Ajándék-Ariadne cave system indicate that the isotope fractionation during carbonate formation in the Legény and Leány caves is kinetically altered. Most promising sites are assumed to be in the inner part of Vacska Cave within this system, where speleothems can be selected for future paleoclimate studies. The monitoring in the caves (Szemlőhegy and Pálvölgy caves) located under urban areas revealed a complex influence of both natural and anthropogenic factors on chemical and isotopic compositions of the drip water.
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Acknowledgements
The study was financially supported by the National Research, Development and Innovation Office, Hungary (OTKA 101664, OTKA 123871 and PD 121387), the Hungarian Academy of Sciences (NANOMIN project, KEP-8/2018), and the Eötvös Loránd Research Network (KEP-1/2020). We are also thankful for the support and permission to the Aggtelek National Park Directorate and Duna-Ipoly National Park Directorate. The János Bolyai Research Scholarship of the Hungarian Academy of Sciences financially supported György Czuppon’s work. The work was language-edited by Iain Coulthard.
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Czuppon, G. et al. (2022). Monitoring and Geochemical Investigations of Caves in Hungary: Implications for Climatological, Hydrological, and Speleothem Formation Processes. In: Veress, M., Leél-Őssy, S. (eds) Cave and Karst Systems of Hungary . Cave and Karst Systems of the World. Springer, Cham. https://doi.org/10.1007/978-3-030-92960-2_16
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