Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany)
Recently exposed loess–palaeosol sequences in the northern Alpine foreland close to Bobingen (southern Germany) were investigated with a multi-proxy approach combining isotopic, geochemical, lithological, and micropalaeontological methods. Luminescence ages date the sections into the Middle and Uppe...
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Copernicus Publications
2017
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00007713 2023-05-15T16:29:09+02:00 Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany) Mayr, Christoph Matzke-Karasz, Renate Stojakowits, Philipp Lowick, Sally E. Zolitschka, Bernd Heigl, Tanja Mollath, Richard Theuerkauf, Marian Weckend, Marc-Oliver Bäumler, Rupert Gregor, Hans-Joachim 2017-12 electronic https://doi.org/10.5194/egqsj-66-73-2017 https://noa.gwlb.de/receive/cop_mods_00007713 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007670/egqsj-66-73-2017.pdf https://egqsj.copernicus.org/articles/66/73/2017/egqsj-66-73-2017.pdf eng eng Copernicus Publications E&G Quaternary Science Journal -- Quaternary science journal -- http://www.bibliothek.uni-regensburg.de/ezeit/?2572732 -- https://www.eg-quaternary-sci-j.net/volumes.html -- 2199-9090 https://doi.org/10.5194/egqsj-66-73-2017 https://noa.gwlb.de/receive/cop_mods_00007713 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007670/egqsj-66-73-2017.pdf https://egqsj.copernicus.org/articles/66/73/2017/egqsj-66-73-2017.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2017 ftnonlinearchiv https://doi.org/10.5194/egqsj-66-73-2017 2022-02-08T22:58:22Z Recently exposed loess–palaeosol sequences in the northern Alpine foreland close to Bobingen (southern Germany) were investigated with a multi-proxy approach combining isotopic, geochemical, lithological, and micropalaeontological methods. Luminescence ages date the sections into the Middle and Upper Würmian periods corresponding to Marine Isotope Stages 3 and 2. A gleyic soil horizon at the base was dated to 45 ka and provided a palynoflora dominated by Poaceae, Cyperaceae, and Pinus, as well as frequent aquatic taxa. Lacustrine conditions prevailed after the gley formation until 30 ka, providing a comparatively diverse lacustrine fauna dominated by aquatic gastropods and the ostracod species Candona candida. At the transition to the Upper Würm, climatic conditions became harsh, indicated by accelerated deposition of more coarse-grained loess, organic geochemical indicators, and scarceness of biotic remains. Two tundra-gley horizons in the Upper Würm point to short phases of climatic amelioration with higher humidity also evidenced by reoccurrence of ostracod and aquatic gastropod remains. We propose that these climatic ameliorations were coincident with the Greenland interstadials 4 and 2. Article in Journal/Newspaper Greenland Tundra Niedersächsisches Online-Archiv NOA Greenland E&G Quaternary Science Journal 66 2 73 89 |
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Niedersächsisches Online-Archiv NOA |
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ftnonlinearchiv |
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English |
topic |
article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Mayr, Christoph Matzke-Karasz, Renate Stojakowits, Philipp Lowick, Sally E. Zolitschka, Bernd Heigl, Tanja Mollath, Richard Theuerkauf, Marian Weckend, Marc-Oliver Bäumler, Rupert Gregor, Hans-Joachim Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany) |
topic_facet |
article Verlagsveröffentlichung |
description |
Recently exposed loess–palaeosol sequences in the northern Alpine foreland close to Bobingen (southern Germany) were investigated with a multi-proxy approach combining isotopic, geochemical, lithological, and micropalaeontological methods. Luminescence ages date the sections into the Middle and Upper Würmian periods corresponding to Marine Isotope Stages 3 and 2. A gleyic soil horizon at the base was dated to 45 ka and provided a palynoflora dominated by Poaceae, Cyperaceae, and Pinus, as well as frequent aquatic taxa. Lacustrine conditions prevailed after the gley formation until 30 ka, providing a comparatively diverse lacustrine fauna dominated by aquatic gastropods and the ostracod species Candona candida. At the transition to the Upper Würm, climatic conditions became harsh, indicated by accelerated deposition of more coarse-grained loess, organic geochemical indicators, and scarceness of biotic remains. Two tundra-gley horizons in the Upper Würm point to short phases of climatic amelioration with higher humidity also evidenced by reoccurrence of ostracod and aquatic gastropod remains. We propose that these climatic ameliorations were coincident with the Greenland interstadials 4 and 2. |
format |
Article in Journal/Newspaper |
author |
Mayr, Christoph Matzke-Karasz, Renate Stojakowits, Philipp Lowick, Sally E. Zolitschka, Bernd Heigl, Tanja Mollath, Richard Theuerkauf, Marian Weckend, Marc-Oliver Bäumler, Rupert Gregor, Hans-Joachim |
author_facet |
Mayr, Christoph Matzke-Karasz, Renate Stojakowits, Philipp Lowick, Sally E. Zolitschka, Bernd Heigl, Tanja Mollath, Richard Theuerkauf, Marian Weckend, Marc-Oliver Bäumler, Rupert Gregor, Hans-Joachim |
author_sort |
Mayr, Christoph |
title |
Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany) |
title_short |
Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany) |
title_full |
Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany) |
title_fullStr |
Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany) |
title_full_unstemmed |
Palaeoenvironments during MIS 3 and MIS 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at Bobingen (southern Germany) |
title_sort |
palaeoenvironments during mis 3 and mis 2 inferred from lacustrine intercalations in the loess–palaeosol sequence at bobingen (southern germany) |
publisher |
Copernicus Publications |
publishDate |
2017 |
url |
https://doi.org/10.5194/egqsj-66-73-2017 https://noa.gwlb.de/receive/cop_mods_00007713 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007670/egqsj-66-73-2017.pdf https://egqsj.copernicus.org/articles/66/73/2017/egqsj-66-73-2017.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Tundra |
genre_facet |
Greenland Tundra |
op_relation |
E&G Quaternary Science Journal -- Quaternary science journal -- http://www.bibliothek.uni-regensburg.de/ezeit/?2572732 -- https://www.eg-quaternary-sci-j.net/volumes.html -- 2199-9090 https://doi.org/10.5194/egqsj-66-73-2017 https://noa.gwlb.de/receive/cop_mods_00007713 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007670/egqsj-66-73-2017.pdf https://egqsj.copernicus.org/articles/66/73/2017/egqsj-66-73-2017.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/egqsj-66-73-2017 |
container_title |
E&G Quaternary Science Journal |
container_volume |
66 |
container_issue |
2 |
container_start_page |
73 |
op_container_end_page |
89 |
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1766018848278970368 |