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Aeolian dynamics at...
Aeolian dynamics at the northern edge of Deliblato (Banat) Sand Sea, Vojvodina, Serbia, at the time of the last deglaciation
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- Marković, Rastko S. (författare)
- University of Niš
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- Perić, Zoran M. (författare)
- Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science
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- Gavrilov, Milivoj B. (författare)
- University of Novi Sad
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- Marković, Slobodan B. (författare)
- University of Novi Sad,University of Montenegro
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- Vandenberghe, Jef (författare)
- Vrije Universiteit Amsterdam
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- Schaetzl, Randall J. (författare)
- Michigan State University
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- Obreht, Igor (författare)
- University of Bremen
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- Bartyik, Tamás (författare)
- University of Szeged
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- Radaković, Milica G. (författare)
- University of Novi Sad
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- Radivojević, Aleksandar (författare)
- University of Niš
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- Marjanović, Miloš (författare)
- University of Novi Sad
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- Lukić, Tin (författare)
- University of Novi Sad
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- Sipos, György (författare)
- University of Bremen
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(creator_code:org_t)
- 2024
- 2024
- Engelska.
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Ingår i: Quaternary Research (United States). - 0033-5894.
- Relaterad länk:
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http://dx.doi.org/10...
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https://lup.lub.lu.s...
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https://doi.org/10.1...
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Abstract
Ämnesord
Stäng
- The Deliblato (Banat) Sand Sea, which is one of the largest areas of aeolian sand in Europe, is located near the Iron Gate, which marks the crossing of the Danube River through the biggest gorge of this river. Here, Danubian alluvium has served as the sand source for the Banat Sand Sea, which was formed primarily through southeasterly (Košava) winds. Utilizing a multi-proxy approach, the objective of this study is to gain a better understanding of the environmental dynamics of the Banat Sand Sea. To achieve this goal, we conducted an analysis of an archive representing an approximately 20-m-thick dune formation on the northern edge of this dune field. Using optically stimulated luminescence (OSL) dating, we calculated aeolian sedimentation rates and dune ages. Sand was deposited here approximately between 17 ka and 13 ka. Magnetic susceptibility, grain size, and colorimetric analyses were interpreted in terms of local paleoenvironmental conditions. Calculated sedimentation rates (SR) indicate intensive aeolian deposition during the study period that range from 483 cm/ka to 502 cm/ka. We compared our data with regional and other European archives, as well as with climatic variations recorded in the Greenland ice core North Greenland Ice Core Project (NGRIP).
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
Nyckelord
- Aeolian sand
- Aeolian sedimentation rates
- Carpathian basin
- Climate
- Danube River
- Dunes
Publikations- och innehållstyp
- art (ämneskategori)
- ref (ämneskategori)
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Till lärosätets databas
- Av författaren/redakt...
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Marković, Rastko ...
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Perić, Zoran M.
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Gavrilov, Milivo ...
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Marković, Slobod ...
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Vandenberghe, Je ...
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Schaetzl, Randal ...
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visa fler...
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Obreht, Igor
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Bartyik, Tamás
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Radaković, Milic ...
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Radivojević, Ale ...
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Marjanović, Milo ...
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Lukić, Tin
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Sipos, György
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visa färre...
- Om ämnet
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- NATURVETENSKAP
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NATURVETENSKAP
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och Geovetenskap och ...
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och Geologi
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Quaternary Resea ...
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Lunds universitet