Central European warm phases recorded by episodic speleothem growth during MIS 3

Abstract Speleothems provide exceptional age control and are a valuable archive for the identification of warm phases in temperate climates. Here we present a speleothem composite record from Germany, which shows episodic growth during the last glacial period, coinciding with several Greenland Interstadials. Using a combined approach of high-resolution solution and in-situ laser ablation 230 Th/U-dating, we were able to precisely constrain the timing and duration of several particularly warm phases during Marine Isotope Stage 3. Climatic conditions favourable for speleothem growth occurred episodically until 32,000 years ago, much longer than reported from existing speleothem records. The inception of speleothem growth lags the onset of Greenland Interstadials and covers approximately 88% of their total duration during early, and approximately 25% during middle and late Marine Isotope Stage 3. This indicates progressive climatic cooling during Marine Isotope Stage 3, with the speleothem growth phases representing persistent Central European warm phases.

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Publication Details

Journal
Communications Earth & Environment
Published
2024-11-20
DOI
https://doi.org/10.1038/s43247-024-01863-0
Citations
5
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
1.88

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article

Central European warm phases recorded by episodic speleothem growth during MIS 3

Denis Scholz, Michael Weber, Jennifer Klose
5 citations
Communications Earth & Environment
Geology and Paleoclimatology Research
1.88
article

Central European warm phases recorded by episodic speleothem growth during MIS 3

Denis Scholz, Michael Weber, Jennifer Klose
article en
5 citations

Abstract

Abstract Speleothems provide exceptional age control and are a valuable archive for the identification of warm phases in temperate climates. Here we present a speleothem composite record from Germany, which shows episodic growth during the last glacial period, coinciding with several Greenland Interstadials. Using a combined approach of high-resolution solution and in-situ laser ablation 230 Th/U-dating, we were able to precisely constrain the timing and duration of several particularly warm phases during Marine Isotope Stage 3. Climatic conditions favourable for speleothem growth occurred episodically until 32,000 years ago, much longer than reported from existing speleothem records. The inception of speleothem growth lags the onset of Greenland Interstadials and covers approximately 88% of their total duration during early, and approximately 25% during middle and late Marine Isotope Stage 3. This indicates progressive climatic cooling during Marine Isotope Stage 3, with the speleothem growth phases representing persistent Central European warm phases.

Communications Earth & EnvironmentVol. 5(1)
Johannes Gutenberg University Mainz (DE)
Deutsche Forschungsgemeinschaft
Life below water
Openalex Percentile: Top 15%
Geology and Paleoclimatology Research
1.88
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