EGU22-6748
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under the Creative Commons Attribution 4.0 License.
A massive ancient flowstone deposit in a high-Alpine cave (Dolomites, N Italy): clues for regional paleovegetation and paleoclimate prior to the Quaternary glaciations
- 1Institute of Geology, University of Innsbruck, Innsbruck, Austria (gabriella.koltai@uibk.ac.at; christoph.spoetl@uibk.ac.at)
- 2Department of Applied Geological Sciences and Geophysics, Montanuniversität Leoben, Leoben, Austria (robert.scholger@unileoben.ac.at)
- 3Climate Risk Analysis, Bad Gandersheim, Germany (mudelsee@climate-risk-analysis.com)
- 4Institute of Botany, University of Hohenheim, Stuttgart, Germany (maria.knipping@uni-hohenheim.de)
- 5School of Environmental and Life Sciences, The University of Newcastle, Callaghan, Australia (andrea.borsato@newcastle.edu)
- 6Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an, China (cheng021@mail.xjtu.edu.cn)
- 7School of Earth Sciences, The University of Melbourne, Melbourne, Australia (j.hellstrom@unimelb.edu.au)
How to cite: Koltai, G., Scholger, R., Mudelsee, M., Knipping, M., Borsato, A., Cheng, H., Hellstrom, J., and Spötl, C.: A massive ancient flowstone deposit in a high-Alpine cave (Dolomites, N Italy): clues for regional paleovegetation and paleoclimate prior to the Quaternary glaciations, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-6748, 2022.