Articles | Volume 72, issue 1
https://doi.org/10.5194/egqsj-72-77-2023
© Author(s) 2023. 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-72-77-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Pleniglacial dynamics in an oceanic central European loess landscape
Stephan Pötter
CORRESPONDING AUTHOR
Department of Geography, RWTH Aachen University, 52062 Aachen, Germany
Chair of Geography, University of Koblenz-Landau, 56070 Koblenz, Germany
Katharina Seeger
Institute of Geography, University of Cologne, 50923 Cologne, Germany
Christiane Richter
Institute of Geography, Technical University Dresden, 01069 Dresden, Germany
Dominik Brill
Institute of Geography, University of Cologne, 50923 Cologne, Germany
Mathias Knaak
Division Applied Geosciences, Geological Survey of North Rhine-Westphalia, 47803 Krefeld, Germany
Frank Lehmkuhl
Department of Geography, RWTH Aachen University, 52062 Aachen, Germany
Philipp Schulte
Department of Geography, RWTH Aachen University, 52062 Aachen, Germany
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Martin Kehl, Katharina Seeger, Stephan Pötter, Philipp Schulte, Nicole Klasen, Mirijam Zickel, Andreas Pastoors, and Erich Claßen
E&G Quaternary Sci. J., 73, 41–67, https://doi.org/10.5194/egqsj-73-41-2024, https://doi.org/10.5194/egqsj-73-41-2024, 2024
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The loess–palaeosol sequence (LPS) at Rheindahlen provides a detailed sedimentary archive of past climate change. Furthermore, it contains Palaeolithic find horizons indicating repeated occupations by Neanderthals. The age of loess layers and the timing of human occupation are a matter of strong scientific debate. We present new data to shed light on formation processes and deposition ages. Previous chronostratigraphic estimates are revised providing a reliable chronostratigraphic framework .
Frank Lehmkuhl, Philipp Schulte, Wolfgang Römer, and Stephan Pötter
E&G Quaternary Sci. J., 72, 203–218, https://doi.org/10.5194/egqsj-72-203-2023, https://doi.org/10.5194/egqsj-72-203-2023, 2023
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Research in loess landscapes provides evidence for the paleoenvironmental settings for past human societies and for the paleoclimate evolution of the past. Archeological and geoscientific investigations must consider different relief settings due to erosion, slope wash, accumulation of sediments and relocation of artifacts. The Lower Rhine Embayment can serve as a blueprint for such research as a typical loess landscape of Central Europe.
Martin Kehl, Katharina Seeger, Stephan Pötter, Philipp Schulte, Nicole Klasen, Mirijam Zickel, Andreas Pastoors, and Erich Claßen
E&G Quaternary Sci. J., 73, 41–67, https://doi.org/10.5194/egqsj-73-41-2024, https://doi.org/10.5194/egqsj-73-41-2024, 2024
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The loess–palaeosol sequence (LPS) at Rheindahlen provides a detailed sedimentary archive of past climate change. Furthermore, it contains Palaeolithic find horizons indicating repeated occupations by Neanderthals. The age of loess layers and the timing of human occupation are a matter of strong scientific debate. We present new data to shed light on formation processes and deposition ages. Previous chronostratigraphic estimates are revised providing a reliable chronostratigraphic framework .
Frank Lehmkuhl, Philipp Schulte, Wolfgang Römer, and Stephan Pötter
E&G Quaternary Sci. J., 72, 203–218, https://doi.org/10.5194/egqsj-72-203-2023, https://doi.org/10.5194/egqsj-72-203-2023, 2023
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Research in loess landscapes provides evidence for the paleoenvironmental settings for past human societies and for the paleoclimate evolution of the past. Archeological and geoscientific investigations must consider different relief settings due to erosion, slope wash, accumulation of sediments and relocation of artifacts. The Lower Rhine Embayment can serve as a blueprint for such research as a typical loess landscape of Central Europe.
Mathias Vinnepand, Peter Fischer, Ulrich Hambach, Olaf Jöris, Carol-Ann Craig, Christian Zeeden, Barry Thornton, Thomas Tütken, Charlotte Prud'homme, Philipp Schulte, Olivier Moine, Kathryn E. Fitzsimmons, Christian Laag, Frank Lehmkuhl, Wolfgang Schirmer, and Andreas Vött
E&G Quaternary Sci. J., 72, 163–184, https://doi.org/10.5194/egqsj-72-163-2023, https://doi.org/10.5194/egqsj-72-163-2023, 2023
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Loess–palaeosol sequences (LPSs) represent continental and non-aquatic archives providing detailed information on Quaternary environmental and climate changes. We present an integrative approach combining sedimentological, rock magnetic, and bulk geochemical data, as well as information on Sr and Nd isotope composition. The approach adds to a comprehensive understanding of LPS formation including changes in dust composition and associated circulation patterns during Quaternary climate changes.
Katharina Seeger, Philip S. J. Minderhoud, Andreas Peffeköver, Anissa Vogel, Helmut Brückner, Frauke Kraas, Nay Win Oo, and Dominik Brill
Hydrol. Earth Syst. Sci., 27, 2257–2281, https://doi.org/10.5194/hess-27-2257-2023, https://doi.org/10.5194/hess-27-2257-2023, 2023
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Accurate elevation data is essential for flood risk assessment. We assess land elevation to local mean sea level of the Ayeyarwady Delta with a new, local DEM based on geodetic data and evaluate the performance of 10 global DEMs in an SLR impact assessment. Our study reveals major differences in performance between global DEMs and consequentially introduced uncertainty in SLR impact assessments, indicating potential similar uncertainties for other data-poor coastal lowlands around the world.
Stephanie Scheidt, Matthias Lenz, Ramon Egli, Dominik Brill, Martin Klug, Karl Fabian, Marlene M. Lenz, Raphael Gromig, Janet Rethemeyer, Bernd Wagner, Grigory Federov, and Martin Melles
Geochronology, 4, 87–107, https://doi.org/10.5194/gchron-4-87-2022, https://doi.org/10.5194/gchron-4-87-2022, 2022
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Levinson-Lessing Lake in northern central Siberia provides an exceptional opportunity to study the evolution of the Earth's magnetic field in the Arctic. This is the first study carried out at the lake that focus on the palaeomagnetic record. It presents the relative palaeointensity and palaeosecular variation of the upper 38 m of sediment core Co1401, spanning ~62 kyr. A comparable high-resolution record of this time does not exist in the Eurasian Arctic.
P. Oyunbat, O. Batkhishig, B. Batsaikhan, F. Lehmkuhl, M. Knippertz, and V. Nottebaum
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLIII-B4-2021, 123–133, https://doi.org/10.5194/isprs-archives-XLIII-B4-2021-123-2021, https://doi.org/10.5194/isprs-archives-XLIII-B4-2021-123-2021, 2021
Dominik Brill, Simon Matthias May, Nadia Mhammdi, Georgina King, Benjamin Lehmann, Christoph Burow, Dennis Wolf, Anja Zander, and Helmut Brückner
Earth Surf. Dynam., 9, 205–234, https://doi.org/10.5194/esurf-9-205-2021, https://doi.org/10.5194/esurf-9-205-2021, 2021
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Wave-transported boulders are important records for storm and tsunami impact over geological timescales. Their use for hazard assessment requires chronological information. We investigated the potential of a new dating technique, luminescence rock surface exposure dating, for estimating transport ages of wave-emplaced boulders. Our results indicate that the new approach may provide chronological information on decadal to millennial timescales for boulders not datable by any other method so far.
Hans von Suchodoletz, Christiane Richter, Frank Walther, Marcel Bliedtner, Mariam Eloshvili, Levan Losaberidze, and Bernhard Hausdorf
E&G Quaternary Sci. J., 69, 247–260, https://doi.org/10.5194/egqsj-69-247-2020, https://doi.org/10.5194/egqsj-69-247-2020, 2020
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We studied snails from Holocene river sediments of the upper Alazani River in the southeastern Caucasus. Since no natural floodplain forests existed in the river valley until ca. 4500 years ago, our snail data confirm a formerly suggested regional settlement center from the ca. 8000 years unknown thus far. Furthermore, increasing proportions of water-related snails for ca. 4000 years indicate a shift of the river course possibly linked with the formation of the Greater Caucasus.
D. Hoffmeister, M. Herbrecht, T. Kramm, and P. Schulte
ISPRS Ann. Photogramm. Remote Sens. Spatial Inf. Sci., IV-3-W2-2020, 25–28, https://doi.org/10.5194/isprs-annals-IV-3-W2-2020-25-2020, https://doi.org/10.5194/isprs-annals-IV-3-W2-2020-25-2020, 2020
Max Engel, Stefanie Rückmann, Philipp Drechsler, Dominik Brill, Stephan Opitz, Jörg W. Fassbinder, Anna Pint, Kim Peis, Dennis Wolf, Christoph Gerber, Kristina Pfeiffer, Ricardo Eichmann, and Helmut Brückner
E&G Quaternary Sci. J., 68, 215–236, https://doi.org/10.5194/egqsj-68-215-2020, https://doi.org/10.5194/egqsj-68-215-2020, 2020
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Late Quaternary landform evolution and sedimentary successions in the Miaoli Tableland, northwestern Taiwan
A tribute to Büdel (1951): The climatic zones of the ice age
A tribute to Louis (1952): On the theory of glacial erosion in valleys
A tribute to Woldstedt (1952): Problems of terrace formation
A tribute to Rohdenburg (1970): Morphodynamic activity and stability phases instead of pluvial and interpluvial times
A first outline of the Quaternary landscape evolution of the Kashaf Rud River basin in the drylands of northeastern Iran
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Revisiting Late Pleistocene glacier dynamics north-west of the Feldberg, southern Black Forest, Germany
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Mathias Vinnepand, Peter Fischer, Ulrich Hambach, Olaf Jöris, Carol-Ann Craig, Christian Zeeden, Barry Thornton, Thomas Tütken, Charlotte Prud'homme, Philipp Schulte, Olivier Moine, Kathryn E. Fitzsimmons, Christian Laag, Frank Lehmkuhl, Wolfgang Schirmer, and Andreas Vött
E&G Quaternary Sci. J., 72, 163–184, https://doi.org/10.5194/egqsj-72-163-2023, https://doi.org/10.5194/egqsj-72-163-2023, 2023
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E&G Quaternary Sci. J., 71, 111–122, https://doi.org/10.5194/egqsj-71-111-2022, https://doi.org/10.5194/egqsj-71-111-2022, 2022
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Shih-Hung Liu, Robert Hebenstreit, and Margot Böse
E&G Quaternary Sci. J., 71, 1–22, https://doi.org/10.5194/egqsj-71-1-2022, https://doi.org/10.5194/egqsj-71-1-2022, 2022
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The Miaoli Tableland (northwestern Taiwan) consists of a sequence of fine-grained tidal to coarse fluvial late Quaternary sediments which underwent a spatially differentiated uplift and fluvial dissection. They reveal repeated rework processes of fluvial cobbles from the highlands to the coast. A new landform classification based on high-resolution 3D terrain analysis results in a new interpretation of the landform evolution. The results favour a local rarely used Quaternary stratigraphic code.
Jef Vandenberghe
E&G Quaternary Sci. J., 70, 205–207, https://doi.org/10.5194/egqsj-70-205-2021, https://doi.org/10.5194/egqsj-70-205-2021, 2021
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Pierre G. Valla
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Dominik Faust and Markus Fuchs
E&G Quaternary Sci. J., 70, 243–246, https://doi.org/10.5194/egqsj-70-243-2021, https://doi.org/10.5194/egqsj-70-243-2021, 2021
Azra Khosravichenar, Morteza Fattahi, Alireza Karimi, Hassan Fazeli Nashli, and Hans von Suchodoletz
E&G Quaternary Sci. J., 70, 145–150, https://doi.org/10.5194/egqsj-70-145-2021, https://doi.org/10.5194/egqsj-70-145-2021, 2021
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Christopher Lüthgens, Jacob Hardt, and Margot Böse
E&G Quaternary Sci. J., 69, 201–223, https://doi.org/10.5194/egqsj-69-201-2020, https://doi.org/10.5194/egqsj-69-201-2020, 2020
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Felix Martin Hofmann, Florian Rauscher, William McCreary, Jan-Paul Bischoff, and Frank Preusser
E&G Quaternary Sci. J., 69, 61–87, https://doi.org/10.5194/egqsj-69-61-2020, https://doi.org/10.5194/egqsj-69-61-2020, 2020
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The Black Forest was covered by a 1000 km2 large ice cap during the last glaciation. Glacial landforms in the area north-west of the highest summit of the Black Forest, the Feldberg (1493 m above sea level), were investigated to select suitable sampling sites for dating glacial landforms in future studies. Some of the terminal moraines described in this study are mapped for the first time. The application of dating methods will provide insights into the chronology of the last glaciation.
Stefan Winkler, David Bell, Maree Hemmingsen, Kate Pedley, and Anna Schoch
E&G Quaternary Sci. J., 67, 25–31, https://doi.org/10.5194/egqsj-67-25-2018, https://doi.org/10.5194/egqsj-67-25-2018, 2018
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Catharina Dieleman, Susan Ivy-Ochs, Kristina Hippe, Olivia Kronig, Florian Kober, and Marcus Christl
E&G Quaternary Sci. J., 67, 17–23, https://doi.org/10.5194/egqsj-67-17-2018, https://doi.org/10.5194/egqsj-67-17-2018, 2018
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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.
We reconstructed a wetland environment for a late Middle to Upper Pleniglacial (approx....