Palaeosols and their cover sediments of a glacial landscape in northern central Europe: Spatial distribution, pedostratigraphy and evidence on landscape evolution
•The largest local record of palaeosols in northern central Europe is presented.•Most palaeosols are Cambisols, Arenosols and Gleysols.•A share of 9% of the study area has buried land surfaces, totalling 5.7 km2.•They were dominantly buried in the late Holocene by anthropogenic soil erosion.•Implica...
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Published in | Catena (Giessen) Vol. 193; p. 104647 |
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Main Authors | , , , , , , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
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Elsevier B.V
01.10.2020
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Abstract | •The largest local record of palaeosols in northern central Europe is presented.•Most palaeosols are Cambisols, Arenosols and Gleysols.•A share of 9% of the study area has buried land surfaces, totalling 5.7 km2.•They were dominantly buried in the late Holocene by anthropogenic soil erosion.•Implications on aeolian, colluvial, lacustrine, and telmatic dynamics were drawn.
Knowledge of the distribution, types and properties of buried soils, i.e. palaeosols, is essential in understanding how lowlands in northern central Europe have changed over past millennia. This is an indispensable requirement for evaluating long-term human impact including soil erosion and land-cover dynamics. In the Serrahn area (62 km2), a young glacial landscape representative for northeastern Germany and part of the Müritz National Park, 26 pedosedimentary sections were documented and analysed. To this end, a multiproxy-approach was applied using pedology, micromorphology, geochronology, and palaeoecology. Statistical and spatial analyses of c. 5200 soil profiles, of which 10% contain palaeosols, show that buried soils cover an area of 5.7 km2, i.e. 9% of the area studied. Most palaeosols are Cambisols, Arenosols and Gleysols. Palaeosols are mainly covered by aeolian and colluvial sands, as well as by lacustrine sands and peat. Radiocarbon and luminescence dating together with palynological and anthracological data reveal that former land surfaces were dominantly buried through erosion triggered by human activity in the late Holocene. In addition, but to a clearly smaller extent, Lateglacial/early Holocene palaeosols and cover sediments occur. Following Medieval clear-cutting and intensive land use, the study area is today again widely forested. The high share of buried land surfaces detected here is expected to be representative for the hilly glacial landscapes even in the wider region, i.e. in northern central Europe, and should be considered in soil mapping, soil carbon budgeting and assessments of past human impact. |
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AbstractList | •The largest local record of palaeosols in northern central Europe is presented.•Most palaeosols are Cambisols, Arenosols and Gleysols.•A share of 9% of the study area has buried land surfaces, totalling 5.7 km2.•They were dominantly buried in the late Holocene by anthropogenic soil erosion.•Implications on aeolian, colluvial, lacustrine, and telmatic dynamics were drawn.
Knowledge of the distribution, types and properties of buried soils, i.e. palaeosols, is essential in understanding how lowlands in northern central Europe have changed over past millennia. This is an indispensable requirement for evaluating long-term human impact including soil erosion and land-cover dynamics. In the Serrahn area (62 km2), a young glacial landscape representative for northeastern Germany and part of the Müritz National Park, 26 pedosedimentary sections were documented and analysed. To this end, a multiproxy-approach was applied using pedology, micromorphology, geochronology, and palaeoecology. Statistical and spatial analyses of c. 5200 soil profiles, of which 10% contain palaeosols, show that buried soils cover an area of 5.7 km2, i.e. 9% of the area studied. Most palaeosols are Cambisols, Arenosols and Gleysols. Palaeosols are mainly covered by aeolian and colluvial sands, as well as by lacustrine sands and peat. Radiocarbon and luminescence dating together with palynological and anthracological data reveal that former land surfaces were dominantly buried through erosion triggered by human activity in the late Holocene. In addition, but to a clearly smaller extent, Lateglacial/early Holocene palaeosols and cover sediments occur. Following Medieval clear-cutting and intensive land use, the study area is today again widely forested. The high share of buried land surfaces detected here is expected to be representative for the hilly glacial landscapes even in the wider region, i.e. in northern central Europe, and should be considered in soil mapping, soil carbon budgeting and assessments of past human impact. |
ArticleNumber | 104647 |
Author | Vogel, Sebastian Schwabe, Matthias Küster, Mathias Wirner, Michael de Boer, Anna Maartje Kaiser, Knut Preusser, Frank Schneider, Thomas Schult, Manuela Theuerkauf, Martin Fülling, Alexander Bens, Oliver Ulrich, Jens Kappler, Christoph Dietze, Elisabeth Börner, Andreas Heinrich, Susann Nelle, Oliver |
Author_xml | – sequence: 1 givenname: Knut surname: Kaiser fullname: Kaiser, Knut email: kaiserk@gfz-potsdam.de organization: GFZ German Research Centre for Geosciences, Telegrafenberg, D-14473 Potsdam, Germany – sequence: 2 givenname: Thomas surname: Schneider fullname: Schneider, Thomas organization: Institute of Earth- and Environmental Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, D-14476 Potsdam, Germany – sequence: 3 givenname: Mathias surname: Küster fullname: Küster, Mathias organization: Müritzeum, Zur Steinmole 1, D-17192 Waren (Müritz), Germany – sequence: 4 givenname: Elisabeth orcidid: 0000-0003-4817-8441 surname: Dietze fullname: Dietze, Elisabeth organization: GFZ German Research Centre for Geosciences, Telegrafenberg, D-14473 Potsdam, Germany – sequence: 5 givenname: Alexander surname: Fülling fullname: Fülling, Alexander organization: Institute of Earth and Environmental Sciences, University of Freiburg, Albertstraße 23b, D-79104 Freiburg, Germany – sequence: 6 givenname: Susann surname: Heinrich fullname: Heinrich, Susann organization: Max Planck Institute for Evolutionary Anthropology, Department of Human Evolution, Deutscher Platz 6, D-04103 Leipzig, Germany – sequence: 7 givenname: Christoph orcidid: 0000-0001-9099-1546 surname: Kappler fullname: Kappler, Christoph organization: GFZ German Research Centre for Geosciences, Telegrafenberg, D-14473 Potsdam, Germany – sequence: 8 givenname: Oliver surname: Nelle fullname: Nelle, Oliver organization: Dendrochronologisches Labor, Landesamt für Denkmalpflege Baden-Württemberg, Regierungspräsidium Stuttgart, Fischersteig 9, D-78343 Hemmenhofen, Germany – sequence: 9 givenname: Manuela surname: Schult fullname: Schult, Manuela organization: Institute of Geography and Geology, University of Greifswald, Friedrich-Ludwig-Jahn-Strasse 16, D-17487Greifswald, Germany – sequence: 10 givenname: Martin surname: Theuerkauf fullname: Theuerkauf, Martin organization: Institute of Geography and Geology, University of Greifswald, Friedrich-Ludwig-Jahn-Strasse 16, D-17487Greifswald, Germany – sequence: 11 givenname: Sebastian orcidid: 0000-0002-9625-8510 surname: Vogel fullname: Vogel, Sebastian organization: Leibniz Institute for Agricultural Engineering and Bioeconomy (ATB), Max-Eyth-Allee 100, D-14469 Potsdam, Germany – sequence: 12 givenname: Anna Maartje surname: de Boer fullname: de Boer, Anna Maartje organization: Wageningen University, Soil Geography and Landscape Group, P.O. Box 476700 AA, Wageningen, The Netherlands – sequence: 13 givenname: Andreas surname: Börner fullname: Börner, Andreas organization: Landesamt für Umwelt, Naturschutz und Geologie (LUNG) Mecklenburg-Vorpommern, Goldberger Straße 12, D-18263 Güstrow, Germany – sequence: 14 givenname: Frank surname: Preusser fullname: Preusser, Frank organization: Institute of Earth and Environmental Sciences, University of Freiburg, Albertstraße 23b, D-79104 Freiburg, Germany – sequence: 15 givenname: Matthias surname: Schwabe fullname: Schwabe, Matthias organization: Müritz National Park Authority, Schlossplatz 3, D-17237 Hohenzieritz, Germany – sequence: 16 givenname: Jens surname: Ulrich fullname: Ulrich, Jens organization: State Archaeological Survey of Mecklenburg-Vorpommern, Domhof 4-5, D-19055 Schwerin, Germany – sequence: 17 givenname: Michael surname: Wirner fullname: Wirner, Michael organization: Landesforst Mecklenburg-Vorpommern, Fachgebiet Standortskartierung, Hauptstraße 11, D-19306 Klein Laasch, Germany – sequence: 18 givenname: Oliver surname: Bens fullname: Bens, Oliver organization: GFZ German Research Centre for Geosciences, Telegrafenberg, D-14473 Potsdam, Germany |
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Snippet | •The largest local record of palaeosols in northern central Europe is presented.•Most palaeosols are Cambisols, Arenosols and Gleysols.•A share of 9% of the... |
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SubjectTerms | Buried soil Holocene Human impact Land-cover change Landscape dynamics Soil erosion |
Title | Palaeosols and their cover sediments of a glacial landscape in northern central Europe: Spatial distribution, pedostratigraphy and evidence on landscape evolution |
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