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....

Full description

Bibliographic Details
Main Authors: Klose, Jennifer, Weber, Michael, Scholz, Denis
Format: Article in Journal/Newspaper
Language:English
Published: Johannes Gutenberg-Universität Mainz 2024
Subjects:
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
_version_ 1831845225692135424
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