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Abstract
This study reconstructs temperatures in the Swiss Alps during the Last Interglacial period (LIG, ~129,000–116,000 years ago) using hydrogen isotopes from fluid inclusions in precisely dated speleothems. The findings reveal temperatures up to 4.3 °C warmer than the 1971–1990 reference period, with climate instability, including an abrupt cooling event around 125,500 years ago. Higher-elevation areas show greater susceptibility to warming, suggesting potential implications for future climate scenarios.
Publisher
Communications Earth & Environment
Published On
Dec 08, 2020
Authors
Paul S. Wilcox, Charlotte Honiat, Martin Trüssel, R. Lawrence Edwards, Christoph Spötl
Tags
Swiss Alps
Last Interglacial
climate change
speleoethms
hydrogen isotopes
temperature reconstruction
climate instability
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