Hydroclimatic Inferences Using Speleothem Trace element, Stable Isotope, and U- Series Proxies from the SISALv3 Speleothem Database
Speleothems are calcium carbonate deposits formed by the degassing of high pCO2 groundwaters typically found in karstic caves. They are a globally distributed geological archive that store information of climate and environmental changes at the time of their formation in multiple proxies, and crucially, provide excellent age control through uranium- thorium dating methods going back to 500,000+ years at seasonal to multi-decadal resolutions.
Authors
- Sophie Warken (ORCID: https://orcid.org/0000-0003-3293-9074)
- Monika Markowska (ORCID: https://orcid.org/0000-0003-1455-1121)
- Zoltán Kern (ORCID: https://orcid.org/0000-0003-4900-2587)
- A. Martin (ORCID: https://orcid.org/0000-0002-0268-0471)
- Micheline Campbell (ORCID: https://orcid.org/0000-0002-9626-1189)
- Dániel Erdélyi (ORCID: https://orcid.org/0000-0002-3340-8403)
- Nikita Kaushal (ORCID: https://orcid.org/0000-0002-2220-9046)
- István Gábor Hatvani (ORCID: https://orcid.org/0000-0002-9262-7315)
- Pauline C. Treble (ORCID: https://orcid.org/0000-0002-1969-8555)
- Andrea Borsato (ORCID: https://orcid.org/0000-0003-3858-4462)
- Carol V. Tadros (ORCID: https://orcid.org/0000-0002-8286-4042)
- Andrea Columbu (ORCID: https://orcid.org/0000-0001-5410-062X)
- Jens Fohlmeister (ORCID: https://orcid.org/0009-0002-1654-3715)
- Nathalie F. Goodkin (ORCID: https://orcid.org/0000-0001-9697-5520)
- Ezgi Ünal‐İmer (ORCID: https://orcid.org/0000-0002-2387-4283)
Publication Details
- Journal
- Karst Science Day Symposium Proceedings.
- Published
- 2024-12-31
- DOI
- https://doi.org/10.70655/ksd.2024.12
- Primary Topic
- Geology and Paleoclimatology Research
- Type
- article
- Field-Weighted Citation Impact
- 0.00