Sedimentology of a Late Quaternary lacustrine record from the south-eastern Carpathian Basin
| Autor: | Andreas Vött, Ulrich Hambach, Nicole Klasen, Slobodan B. Marković, Philipp Schulte, Janina J. Nett, Frank Lehmkuhl, Igor Obreht, Milivoj B. Gavrilov, Finn Viehberg, Wei Chu, Maria Papadopoulou, Peter Fischer, Daniel Veres, Frank Schäbitz, Christian Zeeden |
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| Přispěvatelé: | Hambach, Ulrich, 3 BayCEER & Chair of Geomorphology University of Bayreuth Germany, Klasen, Nicole, 4 Institute of Geography University of Cologne Germany, Fischer, Peter, 5 Institute for Geography Johannes Gutenberg‐Universität Mainz Germany, Schulte, Philipp, 1 Department of Geography RWTH Aachen University Germany, Nett, Janina J., Veres, Daniel, 6 Institute of Speleology Romanian Academy Cluj‐Napoca Romania, Obreht, Igor, Chu, Wei, 8 Institute of Prehistoric Archaeology University of Cologne Germany, Papadopoulou, Maria, 9 Institute of Geography Education University of Cologne Cologne Germany, Viehberg, Finn, 10 Institute for Geography and Geology Universität Greifswald Germany, Schäbitz, Frank, Gavrilov, Milivoj B., 11 Chair of Physical Geography, Faculty of Sciences University of Novi Sad Serbia, MarkoviĆ, Slobodan B., Vött, Andreas, Lehmkuhl, Frank |
| Jazyk: | angličtina |
| Rok vydání: | 2021 |
| Předmět: |
Carpathian Basin
Environmental dynamics Thermoluminescence dating Pannonian basin lacustrine sediment grain‐size analysis Paleontology Late Quaternary Arts and Humanities (miscellaneous) luminescence dating environmental dynamics Earth and Planetary Sciences (miscellaneous) geoelectric analyses Sedimentology Quaternary South eastern Geology |
| Zdroj: | Journal of Quaternary Science. 36(8):1414-1425 |
| ISSN: | 0267-8179 |
| DOI: | 10.1002/jqs.3297 |
| Popis: | The Upper Pleistocene geoarchives in the south‐eastern Carpathian Basin are represented predominantly by loess–palaeosol records. In 2015, a 10 m sediment core composed of clay‐rich lacustrine sediments was recovered by vibracoring a dry lake basin located between the Vršac Mountains (Serbia) and the Banat Sands in the south‐eastern Carpathian Basin; a location relevant for placing regional archaeological results in a palaeoenvironmental context. Here, we present results from geoelectrical prospection and a lithostratigraphic interpretation of this sequence supported by a detailed granulometric study supplemented by ostracod analysis. An age model based on luminescence dating is discussed against sedimentological proxy data and its implication for palaeoenvironmental change. The cores show a stratigraphy of lighter ochre‐coloured and darker greyish sediment, related to the deposition of clay and silt trapped in an aquatic environment. Geophysical measurements show ~20 m thick lacustrine sediments. The grain‐size distributions including the variability in fine clay are indicative of a lacustrine environment. Fine particles were brought into the depositional environments by aquatic input and settled from suspension; also, direct dust input is constrained by grain‐size results. Riverine input and aeolian dust input interplayed at the locality. Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659 Program IDEI_Proiecte de Cercetare Exploratorie Serbian Ministry of Education, Science and Technological Development |
| Databáze: | OpenAIRE |
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