Central European warm phases recorded by episodic speleothem growth during MIS 3
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....
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Format: | Article in Journal/Newspaper |
Language: | English |
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Johannes Gutenberg-Universität Mainz
2024
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Online Access: | https://openscience.ub.uni-mainz.de/handle/20.500.12030/12030 https://hdl.handle.net/20.500.12030/12030 https://doi.org/10.25358/openscience-12009 |
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author | Klose, Jennifer Weber, Michael Scholz, Denis |
author_facet | Klose, Jennifer Weber, Michael Scholz, Denis |
author_sort | Klose, Jennifer |
collection | Gutenberg Open Science (Open-Science-Repository of the Johannes Gutenberg-University Mainz) |
description | 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 230Th/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. |
format | Article in Journal/Newspaper |
genre | Greenland |
genre_facet | Greenland |
geographic | Greenland |
geographic_facet | Greenland |
id | ftunivmainzpubl:oai:openscience.ub.uni-mainz.de:20.500.12030/12030 |
institution | Open Polar |
language | English |
op_collection_id | ftunivmainzpubl |
op_doi | https://doi.org/20.500.12030/1203010.25358/openscience-12009 |
op_rights | CC BY https://creativecommons.org/licenses/by/4.0/ openAccess |
op_source | Communications Earth & Environment. 5. -. 2024. -. -. 719 |
publishDate | 2024 |
publisher | Johannes Gutenberg-Universität Mainz |
record_format | openpolar |
spelling | ftunivmainzpubl:oai:openscience.ub.uni-mainz.de:20.500.12030/12030 2025-05-11T14:20:12+00:00 Central European warm phases recorded by episodic speleothem growth during MIS 3 Klose, Jennifer Weber, Michael Scholz, Denis 2024 https://openscience.ub.uni-mainz.de/handle/20.500.12030/12030 https://hdl.handle.net/20.500.12030/12030 https://doi.org/10.25358/openscience-12009 eng eng Johannes Gutenberg-Universität Mainz CC BY https://creativecommons.org/licenses/by/4.0/ openAccess Communications Earth & Environment. 5. -. 2024. -. -. 719 ddc:333.7 ddc:550 Zeitschriftenaufsatz publishedVersion Text doc-type:Article 2024 ftunivmainzpubl https://doi.org/20.500.12030/1203010.25358/openscience-12009 2025-04-14T23:38:55Z 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 230Th/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. Article in Journal/Newspaper Greenland Gutenberg Open Science (Open-Science-Repository of the Johannes Gutenberg-University Mainz) Greenland |
spellingShingle | ddc:333.7 ddc:550 Klose, Jennifer Weber, Michael Scholz, Denis Central European warm phases recorded by episodic speleothem growth during MIS 3 |
title | Central European warm phases recorded by episodic speleothem growth during MIS 3 |
title_full | Central European warm phases recorded by episodic speleothem growth during MIS 3 |
title_fullStr | Central European warm phases recorded by episodic speleothem growth during MIS 3 |
title_full_unstemmed | Central European warm phases recorded by episodic speleothem growth during MIS 3 |
title_short | Central European warm phases recorded by episodic speleothem growth during MIS 3 |
title_sort | central european warm phases recorded by episodic speleothem growth during mis 3 |
topic | ddc:333.7 ddc:550 |
topic_facet | ddc:333.7 ddc:550 |
url | https://openscience.ub.uni-mainz.de/handle/20.500.12030/12030 https://hdl.handle.net/20.500.12030/12030 https://doi.org/10.25358/openscience-12009 |