Articles | Volume 72, issue 2
https://doi.org/10.5194/egqsj-72-163-2023
© 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-72-163-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Aug 2023
Research article |
| 04 Aug 2023
| 04 Aug 2023
What do dust sinks tell us about their sources and past environmental dynamics? A case study for oxygen isotope stages 3–2 in the Middle Rhine Valley, Germany
Mathias Vinnepand
CORRESPONDING AUTHOR
Natural Hazard Research and Geoarchaeology, Institute for Geography, Johannes Gutenberg-Universität Mainz, 55099 Mainz, Germany
Natural Hazard Research and Geoarchaeology, Institute for Geography, Johannes Gutenberg-Universität Mainz, 55099 Mainz, Germany
Ulrich Hambach
BayCEER and Chair of Geomorphology, University of Bayreuth, 95440 Bayreuth, Germany
Emil Racovita Institute of Speleology (ERIS), Romanian Academy, Cluj-Napoca branch, Clinicilor 5, 400006 Cluj-Napoca, Romania
Olaf Jöris
MONREPOS Archaeological Research Centre and Museum for Human Behavioural Evolution, Leibniz-Zentrum für Archäologie, 56567 Neuwied, Germany
Carol-Ann Craig
Environmental and Biogeochemical Sciences Group, The James Hutton Institute, Aberdeen, AB15 8QH, Scotland, UK
Christian Zeeden
Rock Physics and Borehole Geophysics, LIAG – Leibniz Institute for Applied Geophysics, 30655 Hanover, Germany
Barry Thornton
Environmental and Biogeochemical Sciences Group, The James Hutton Institute, Aberdeen, AB15 8QH, Scotland, UK
Thomas Tütken
Applied and Analytical Paleontology, Institute of Geosciences, Johannes Gutenberg-Universität Mainz, 55099 Mainz, Germany
Charlotte Prud'homme
Institute of Earth Surface Dynamics, University of Lausanne, 1015 Lausanne, Switzerland
Philipp Schulte
Chair in Physical Geography and Geoecology, Department of Geography, RWTH Aachen, 52056 Aachen, Germany
Olivier Moine
Laboratoire de Géographie Physique, UMR 8591 CNRS Université Paris 1 UPEC, Thiais 94320, France
Kathryn E. Fitzsimmons
Department of Geosciences, University of Tübingen, 72076 Tübingen, Germany
Christian Laag
Department of Research and Development, Nolte Geoservices GmbH, 48301 Nottuln, Germany
Institut de Physique du Globe de Paris, CNRS, Université Paris Cité, 75238 Paris, France
Frank Lehmkuhl
Chair in Physical Geography and Geoecology, Department of Geography, RWTH Aachen, 52056 Aachen, Germany
Wolfgang Schirmer
independent researcher: Wolkenstein 24, 91320 Wolkenstein, Germany
Andreas Vött
Natural Hazard Research and Geoarchaeology, Institute for Geography, Johannes Gutenberg-Universität Mainz, 55099 Mainz, Germany
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E&G Quaternary Sci. J., 70, 191–195, https://doi.org/10.5194/egqsj-70-191-2021, https://doi.org/10.5194/egqsj-70-191-2021, 2021
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D. Hoffmeister, M. Herbrecht, T. Kramm, and P. Schulte
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C. Hatté, C. Gauthier, D.-D. Rousseau, P. Antoine, M. Fuchs, F. Lagroix, S. B. Marković, O. Moine, and A. Sima
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Related subject area
Geomorphology
Millennial-scale erosion rates in the Harz Mountains (Germany) from cosmogenic 10Be: implications for landscape evolution of basement highs in Central Europe
Pleniglacial dynamics in an oceanic central European loess landscape
On the expression and distribution of glacial trimlines: a case study of Little Ice Age trimlines on Svalbard
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
Proposing a new conceptual model for the reconstruction of ice dynamics in the SW sector of the Scandinavian Ice Sheet (SIS) based on the reinterpretation of published data and new evidence from optically stimulated luminescence (OSL) dating
Revisiting Late Pleistocene glacier dynamics north-west of the Feldberg, southern Black Forest, Germany
Disestablishing “Glacial Lake Speight”, New Zealand? An example for the validity of detailed geomorphological assessment with the study of mountain glaciations
Reconsidering the origin of the Sedrun fans (Graubünden, Switzerland)
Ralf Hetzel, Henrik Rother, Reinhard Wolff, and Kyra Hölzer
E&G Quaternary Sci. J., 73, 161–178, https://doi.org/10.5194/egqsj-73-161-2024, https://doi.org/10.5194/egqsj-73-161-2024, 2024
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We present 10Be-based erosion rates for the Harz Mountains. Erosion is slope-dependent, and the Harz topography evolves at rates of a few tens of meters per million years. The 300 m difference in elevation between a planation surface in the Harz and its lower surroundings results from rock uplift, erosion of sediments in adjacent areas, and migration and dissolution of Permian salt. Active reverse faulting along the northern Harz is inconsistent with geological, geophysical, and geodetic data.
Stephan Pötter, Katharina Seeger, Christiane Richter, Dominik Brill, Mathias Knaak, Frank Lehmkuhl, and Philipp Schulte
E&G Quaternary Sci. J., 72, 77–94, https://doi.org/10.5194/egqsj-72-77-2023, https://doi.org/10.5194/egqsj-72-77-2023, 2023
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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.
Camilla M. Rootes and Christopher D. Clark
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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Glacial trimlines are visible breaks in vegetation or landforms that mark the former extent of glaciers. They are often observed as faint lines running across valley sides and are useful for mapping the three-dimensional shape of former glaciers or for assessing by how much present-day glaciers have thinned and retreated. Here we present the first application of a new trimline classification scheme to a case study location in central western Spitsbergen, Svalbard.
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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A main element in Büdel's concept is his quite provocative link between climate zones and geomorphological processes, a strong relation which was frequently contested later. Büdel's contribution is still relevant in modern times as the present-day climatic change will probably also invoke a poleward shift of climatic zones, accompanied by associated shifts in geomorphological environments and ecosystems.
Pierre G. Valla
E&G Quaternary Sci. J., 70, 209–212, https://doi.org/10.5194/egqsj-70-209-2021, https://doi.org/10.5194/egqsj-70-209-2021, 2021
James Rose, David R. Bridgland, and Rob Westaway
E&G Quaternary Sci. J., 70, 217–220, https://doi.org/10.5194/egqsj-70-217-2021, https://doi.org/10.5194/egqsj-70-217-2021, 2021
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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This article discusses the first basic framework of Quaternary landscape evolution in a main large river valley of the drylands of northeastern Iran and the first geomorphic frame for human migrations in the important migration corridor of central Asia.
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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Our new concept of the Weichselian ice dynamics in the south-western sector of the Baltic Sea depression is based on existing geochronological data from Germany, Denmark and southernmost Sweden, as well as new data from north-east Germany. Previous models are mainly based on the reconstruction of morphologically continuous ice-marginal positions, whereas our model shows a strong lobate and variable character of ice advances. We strongly suggest an age- and process-based approach in the future.
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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Geomorphological mapping and analysis conducted as an initial step towards a future sediment budget study of the middle Waimakariri River (Southern Alps, New Zealand) reveals that the traditional concept of the temporary palaeolake
glacial Lake Speightis conflicting with our conclusions of realistic chronosequences and timescales of para- and postglacial landform development. Especially the temporal and causal relation to the last deglaciation needs to be questioned and will be discussed.
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
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.
Loess–palaeosol sequences (LPSs) represent continental and non-aquatic archives providing...
