globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2017.08.014
Scopus记录号: 2-s2.0-85028357559
论文题名:
Middle to Late Pleistocene multi-proxy record of environmental response to climate change from the Vienna Basin, Central Europe (Austria)
作者: Salcher B.C.; Frank-Fellner C.; Lomax J.; Preusser F.; Ottner F.; Scholger R.; Wagreich M.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2017
卷: 173
起始页码: 193
结束页码: 210
语种: 英语
Scopus关键词: Deposits ; Geomagnetism ; Glacial geology ; Salinity measurement ; Stratigraphy ; Coarse-grained fluvial ; Environmental conditions ; Environmental history ; Environmental response ; Geomagnetic excursions ; Marine isotope stages ; Mediterranean climates ; Palaeoenvironmental reconstruction ; Climate change ; Mollusca
英文摘要: Tectonic basins can represent valuable archives of the environmental history. Presented here are the stratigraphy and multi-proxy analyses of two adjacent alluvial fans in the Quaternary active parts of the Vienna Basin, situated at the interface of the Atlantic, European continental and Mediterranean climate. Deposits comprise a sequence of coarse-grained fluvial deposits intercalated by laterally extensive horizons of pedogenically altered fine sediments. To establish palaeoenvironmental reconstructions, fine-grained sequences from a drill core and outcrop data were analysed according to its malacofauna, palaeopedology, susceptibility and sedimentology. The chronological framework is provided by 38 luminescence ages and supported by geomagnetic polarity investigations. Distinct warm periods each associated with a geomagnetic excursion, are recorded in three pedocomplexes formed during the Last Interglacial and two earlier interglacial periods, indicted to correlate with Marine Isotope Stage (MIS) 9 and MIS 11, respectively. Environmental conditions during the early last glacial period (MIS 5, c. 100–70 ka) are reconstructed from mollusc-shell rich overbank fines deposited along a former channel belt, covered by massive sheetflood deposits during MIS 2. Analysed warm phases suggest strong variations in humidity, ranging from steppe to forest dominated environments. The study presents one of the few numerically dated Middle Pleistocene multi-proxy records and one of the most comprehensive malacological datasets covering the early phases of last glacial period of continental Europe. © 2017 Elsevier Ltd
资助项目: This project was funded by the Vienna City Fund (Hochschuljubiläumsstiftung, H-2048/2010) and the Austrian Science Fund (FWF 18203). Digital elevation and drill log data was provided by the Government of Lower Austria and the Geological Survey of Austria. Ola Kwiecien's and Stephanie Neuhuber's thoughtful and thorough reading of the manuscript are highly appreciated. We are grateful to Matthias Marbach for help with water-saturation tests. Ylvie Aranmanoth is thanked for her patience with the artwork and manuscript writing. Four anonymous reviewers are highly acknowledged for their very constructive reviews and valuable suggestions.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59101
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作者单位: Department for Geography and Geology, University of Salzburg, Hellbrunnerstrasse 34, Salzburg, Austria; Department of Anthropology, University of Vienna, Althanstraße 14, Vienna, Austria; University of Natural Resources and Life Sciences, Peter-Jordan-Straße 70, Wien, Austria; Department of Physical Geography, Justus-Liebig-Universität Gießen, Senckenbergstraße 1, Gießen, Germany; Institute of Earth and Environmental Science, University of Freiburg, Albertstraße 23b, Freiburg, Germany; Chair of Applied Geophysics, Montanuniversität Leoben, Peter-Tunner-Straße 25, Leoben, Austria; Department for Geodynamics and Sedimentology, University of Vienna, Althanstrasse 14, Vienna, Austria

Recommended Citation:
Salcher B.C.,Frank-Fellner C.,Lomax J.,et al. Middle to Late Pleistocene multi-proxy record of environmental response to climate change from the Vienna Basin, Central Europe (Austria)[J]. Quaternary Science Reviews,2017-01-01,173
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