New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2

The study of two cliff outcrops from the Jasmund Peninsula provides new information on the ice‐sheet dynamics and palaeo‐environmental conditions during MIS 3 and the ensuing transition to MIS 2 in the southwestern Baltic Sea region. We identified interstadial fluvial sediments, with mollusc and ver...

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Published in:Boreas
Main Authors: Kenzler, Michael, Tsukamoto, Sumiko, Meng, Stefan, Frechen, Manfred, Hüneke, Heiko
Other Authors: Deutsche Forschungsgemeinschaft
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
Subjects:
Online Access:http://dx.doi.org/10.1111/bor.12206
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12206
https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12206
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author Kenzler, Michael
Tsukamoto, Sumiko
Meng, Stefan
Frechen, Manfred
Hüneke, Heiko
author2 Deutsche Forschungsgemeinschaft
author_facet Kenzler, Michael
Tsukamoto, Sumiko
Meng, Stefan
Frechen, Manfred
Hüneke, Heiko
author_sort Kenzler, Michael
collection Wiley Online Library
container_issue 1
container_start_page 34
container_title Boreas
container_volume 46
description The study of two cliff outcrops from the Jasmund Peninsula provides new information on the ice‐sheet dynamics and palaeo‐environmental conditions during MIS 3 and the ensuing transition to MIS 2 in the southwestern Baltic Sea region. We identified interstadial fluvial sediments, with mollusc and vertebrate fauna, which were deposited between 47 and 42 ka in a steppe‐like landscape. A subsequent cooling phase led to the formation of a proglacial lake, between 30 and 22 ka, indicated by varve‐like, rhythmically bedded silty clay. This proglacial lake formation can be correlated to the blocking of the Baltic Basin by the Kattegat ice advance, previously dated to c . 29–26 ka. The transition from proglacial to terminoglacial lacustrine deposits reflects the immediate advance of the Scandinavian Ice Sheet ( SIS ) into the study area after the transition from MIS 3 to early MIS 2. The SIS finally reached the area at 23±2 ka (Brandenburgian phase; advance from the northeast). A subsequent ice retreat accompanied by the deposition of meltwater sediments was followed by a re‐advance of the SIS , resulting in a glaciotectonic deformation event across the study area. The age control for our study is based on optically stimulated luminescence ( OSL ). The investigated Pleistocene sediments show ice‐free conditions during MIS 3 and early MIS 2, indicating that neither the Ristinge nor the Klintholm advance reached the SW Baltic Sea coast of Jasmund.
format Article in Journal/Newspaper
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op_doi https://doi.org/10.1111/bor.12206
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_source Boreas
volume 46, issue 1, page 34-52
ISSN 0300-9483 1502-3885
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spelling crwiley:10.1111/bor.12206 2025-01-16T22:25:46+00:00 New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2 Kenzler, Michael Tsukamoto, Sumiko Meng, Stefan Frechen, Manfred Hüneke, Heiko Deutsche Forschungsgemeinschaft 2016 http://dx.doi.org/10.1111/bor.12206 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12206 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12206 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 46, issue 1, page 34-52 ISSN 0300-9483 1502-3885 journal-article 2016 crwiley https://doi.org/10.1111/bor.12206 2024-06-18T04:12:41Z The study of two cliff outcrops from the Jasmund Peninsula provides new information on the ice‐sheet dynamics and palaeo‐environmental conditions during MIS 3 and the ensuing transition to MIS 2 in the southwestern Baltic Sea region. We identified interstadial fluvial sediments, with mollusc and vertebrate fauna, which were deposited between 47 and 42 ka in a steppe‐like landscape. A subsequent cooling phase led to the formation of a proglacial lake, between 30 and 22 ka, indicated by varve‐like, rhythmically bedded silty clay. This proglacial lake formation can be correlated to the blocking of the Baltic Basin by the Kattegat ice advance, previously dated to c . 29–26 ka. The transition from proglacial to terminoglacial lacustrine deposits reflects the immediate advance of the Scandinavian Ice Sheet ( SIS ) into the study area after the transition from MIS 3 to early MIS 2. The SIS finally reached the area at 23±2 ka (Brandenburgian phase; advance from the northeast). A subsequent ice retreat accompanied by the deposition of meltwater sediments was followed by a re‐advance of the SIS , resulting in a glaciotectonic deformation event across the study area. The age control for our study is based on optically stimulated luminescence ( OSL ). The investigated Pleistocene sediments show ice‐free conditions during MIS 3 and early MIS 2, indicating that neither the Ristinge nor the Klintholm advance reached the SW Baltic Sea coast of Jasmund. Article in Journal/Newspaper Ice Sheet Wiley Online Library Kattegat ENVELOPE(9.692,9.692,63.563,63.563) Boreas 46 1 34 52
spellingShingle Kenzler, Michael
Tsukamoto, Sumiko
Meng, Stefan
Frechen, Manfred
Hüneke, Heiko
New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2
title New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2
title_full New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2
title_fullStr New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2
title_full_unstemmed New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2
title_short New age constraints from the SW Baltic Sea area – implications for Scandinavian Ice Sheet dynamics and palaeo‐environmental conditions during MIS 3 and early MIS 2
title_sort new age constraints from the sw baltic sea area – implications for scandinavian ice sheet dynamics and palaeo‐environmental conditions during mis 3 and early mis 2
url http://dx.doi.org/10.1111/bor.12206
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12206
https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12206