Articles | Volume 75, issue 1
https://doi.org/10.5194/egqsj-75-85-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/egqsj-75-85-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
An MIS 8 terrestrial record retrieved from a glacially overdeepened basin in the northern foreland of the European Alps
Institute of Applied Geology, University of Natural Resources and Life Sciences Vienna (BOKU), Vienna, 1190, Austria
Christopher Lüthgens
Institute of Applied Geology, University of Natural Resources and Life Sciences Vienna (BOKU), Vienna, 1190, Austria
Thomas Burschil
Federal Institute for Geosciences and Resources (BGR), Hanover, 30655, Germany
Stephanie Neuhuber
Institute of Applied Geology, University of Natural Resources and Life Sciences Vienna (BOKU), Vienna, 1190, Austria
Roberta Pini
CNR IGAG, Laboratory of Palynology and Palaeoecology, Milano, 20126, Italy
Oscar Marchhart
Isotope Physics, University of Vienna, Vienna, 1090, Austria
Alexander Wieser
Isotope Physics, University of Vienna, Vienna, 1090, Austria
Clemens Schmalfuss
Institute of Applied Geology, University of Natural Resources and Life Sciences Vienna (BOKU), Vienna, 1190, Austria
Ernst Kroemer
Bavarian Environment Agency (LfU), Hof/Saale, 95030, Germany
Markus Fiebig
Institute of Applied Geology, University of Natural Resources and Life Sciences Vienna (BOKU), Vienna, 1190, Austria
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The Last Glacial Maximum (LGM) about 21 kyr ago is known to have been global in extent. Nonetheless, we have limited knowledge during the pre-LGM time in the southern middle latitudes. If we want to understand the causes of the ice ages, the complete glacial period must be addressed. In this paper, we show that the Patagonian Ice Sheet in southern South America reached its full glacial extent also by 57 kyr ago and defies a climate explanation.
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Short summary
Depositional single-grain feldspar luminescence ages reveal the filling of a glacially overdeepened basin during Marine Isotope Stage 8, representing rare evidence of this time frame in the northern Alpine foreland. Reflection seismic surveys revealed two cross-cutting glacial basins. The dated sediments reveal significantly younger ages than previously assumed. This represents a first step in a re-evaluation of the established Quaternary depositional chronology of the Bavarian Alpine foreland.
Depositional single-grain feldspar luminescence ages reveal the filling of a glacially...