Aeolian dynamics at the northern edge of Deliblato (Banat) Sand Sea, Vojvodina, Serbia, at the time of the last deglaciation
The Deliblato (Banat) Sand Sea, which is one of the largest areas of аeolian 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 fo...
Elmentve itt :
| Szerzők: | |
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| Dokumentumtípus: | Cikk |
| Megjelent: |
2024
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| Sorozat: | QUATERNARY RESEARCH
121 |
| Tárgyszavak: | |
| doi: | 10.1017/qua.2024.13 |
| mtmt: | 34851610 |
| Online Access: | http://publicatio.bibl.u-szeged.hu/34711 |
| LEADER | 02636nab a2200361 i 4500 | ||
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| 008 | 240925s2024 hu o 000 eng d | ||
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| 024 | 7 | |a 10.1017/qua.2024.13 |2 doi | |
| 024 | 7 | |a 34851610 |2 mtmt | |
| 040 | |a SZTE Publicatio Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Marković Rastko S. | |
| 245 | 1 | 0 | |a Aeolian dynamics at the northern edge of Deliblato (Banat) Sand Sea, Vojvodina, Serbia, at the time of the last deglaciation |h [elektronikus dokumentum] / |c Marković Rastko S. |
| 260 | |c 2024 | ||
| 300 | |a 59-72 | ||
| 490 | 0 | |a QUATERNARY RESEARCH |v 121 | |
| 520 | 3 | |a The Deliblato (Banat) Sand Sea, which is one of the largest areas of аeolian 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). | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 700 | 0 | 1 | |a Perić Zoran M. |e aut |
| 700 | 0 | 1 | |a Gavrilov Milivoj B. |e aut |
| 700 | 0 | 1 | |a Marković Slobodan B |e aut |
| 700 | 0 | 1 | |a Vandenberghe Jef |e aut |
| 700 | 0 | 1 | |a Schaetzl Randall J. |e aut |
| 700 | 0 | 1 | |a Obreht Igor |e aut |
| 700 | 0 | 1 | |a Bartyik Tamás |e aut |
| 700 | 0 | 1 | |a Radaković Milica G. |e aut |
| 700 | 0 | 1 | |a Radivojević Aleksandar |e aut |
| 700 | 0 | 1 | |a Marjanović Miloš |e aut |
| 700 | 0 | 1 | |a Lukić Tin |e aut |
| 700 | 0 | 1 | |a Sipos György |e aut |
| 856 | 4 | 0 | |u http://publicatio.bibl.u-szeged.hu/34711/1/aeolian-dynamics-at-the-northern-edge-of-deliblato-banat-sand-sea-vojvodina-serbia-at-the-time-of-the-last-deglaciation.pdf |z Dokumentum-elérés |