Articles | Volume 72, issue 1
https://doi.org/10.5194/egqsj-72-77-2023
https://doi.org/10.5194/egqsj-72-77-2023
Research article
 | 
24 Apr 2023
Research article |  | 24 Apr 2023

Pleniglacial dynamics in an oceanic central European loess landscape

Stephan Pötter, Katharina Seeger, Christiane Richter, Dominik Brill, Mathias Knaak, Frank Lehmkuhl, and Philipp Schulte

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Cited articles

Allen, J. R. L. and Thornley, D. M.: Laser granulometry of Holocene estuarine silts: effects of hydrogen peroxide treatment, Holocene, 14, 290–295, https://doi.org/10.1191/0959683604hl681rr, 2004. 
Antoine, P., Rousseau, D.-D., Zöller, L., Lang, A., Munaut, A.-V., Hatté, C., and Fontugne, M.: High-resolution record of the last Interglacial–glacial cycle in the Nussloch loess–palaeosol sequences, Upper Rhine Area, Germany, Quatern. Int., 76–77, 211–229, https://doi.org/10.1016/S1040-6182(00)00104-X, 2001. 
Antoine, P., Catt, J., Lautridou, J.-P., and Sommé, J.: The loess and coversands of northern France and southern England, J. Quaternary Sci., 18, 309–318, https://doi.org/10.1002/jqs.750, 2003. 
Antoine, P., Rousseau, D.-D., Moine, O., Kunesch, S., Hatté, C., Lang, A., Tissoux, H., and Zöller, L.: Rapid and cyclic aeolian deposition during the Last Glacial in European loess: a high-resolution record from Nussloch, Germany, Quaternary Sci. Rev., 28, 2955–2973, https://doi.org/10.1016/j.quascirev.2009.08.001, 2009. 
Antoine, P., Rousseau, D.-D., Degeai, J.-P., Moine, O., Lagroix, F., Kreutzer, S., Fuchs, M., Hatté, C., Gauthier, C., Svoboda, J., and Lisá, L.: High-resolution record of the environmental response to climatic variations during the Last Interglacial–Glacial cycle in Central Europe: the loess-palaeosol sequence of Dolní Věstonice (Czech Republic), Quaternary Sci. Rev., 67, 17–38, https://doi.org/10.1016/j.quascirev.2013.01.014, 2013. 
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Short summary
We reconstructed a wetland environment for a late Middle to Upper Pleniglacial (approx. 30–20 ka) loess sequence in western Germany. Typically, these sequences reveal terrestrial conditions with soil formation processes during this time frame. The here-investigated section, however, was influenced by periodical flooding, leading to marshy conditions and a stressed ecosystem. Our results show that the landscape of the study area was much more fragmented during this time than previously thought.
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