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DOI10.1016/j.palaeo.2019.05.024
Stratigraphy and chronology of the periphery of the Scandinavian ice sheet at the foot of the Ukrainian Carpathians
Łanczont M.; Bogucki A.; Yatsyshyn A.; Terpiłowski S.; Mroczek P.; Orłowska A.; Hołub B.; Zieliński P.; Komar M.; Woronko B.; Kulesza P.; Dmytruk R.; Tomeniuk O.
发表日期2019
ISSN0031-0182
起始页码59
结束页码77
卷号530
英文摘要The article presents the results of research on the formation conditions and the age of glaciogenic deposits left by the Scandinavian ice sheet in the Eastern Carpathian Foreland, in its part drained by the Dniester River and its tributaries (Black Sea basin). These deposits (till, erratics, glaciolacustrine and glaciofluvial sediments), preserved only in some places and occurring in the range of altitudes defined by terrace VI (Early Pleistocene) and terrace V (Middle Pleistocene), are the southernmost traces of the ice sheet in Europe. They are underlain by fluvial deposits and overlain by loess deposits, and locally occur as intraloess layers. The following research methods were used: geomorphological mapping, sedimentological, lithological, micromorphological, palaeopedological, and palaeontological analyses, as well as luminescence dating. The obtained results allowed a reconstruction to be made of the main stages of morphogenesis and the style of the ice-sheet advance at its maximum extent, defined as the Sambor Phase. The area was glaciated during MIS 12 (Elsterian II = Sanian 2 = Okanian), as indicated by the occurrence of a complete Middle/Upper Pleistocene loess–palaeosol sequence. The oldest palaeosol (S4), i.e. Sokal (=Mazovian = Zavadivka) soil that developed directly on the glaciogenic deposits or loess L5 is correlated with the Holsteinian (=Likhvinian) Interglacial (MIS 11). © 2019 Elsevier B.V.
英文关键词Dniester River valley; Elsterian glaciation; Fluvial and glaciogenic deposits; Loess–palaeosol sequences; Palaeoreconstructions; Pleistocene
语种英语
scopus关键词chronology; glaciation; glaciofluvial deposit; Holsteinian; interglacial; loess; luminescence dating; paleoenvironment; paleosol; Pleistocene; reconstruction; Scandinavian Ice Sheet; scandium; stratigraphy; tributary; Black Sea Coast [Ukraine]; Carpathians; Dniester River; Scandinavia; Ukraine
来源期刊Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/150910
作者单位Faculty of Earth Sciences and Spatial Management, Maria Curie-Skłodowska University, Al. Kraśnicka 2d, Lublin, 20-718, Poland; Faculty of Geography, Ivan Franko National University, Doroshenka Str. 41, Lviv, 79000, Ukraine; National Museum of Natural History, National Academy of Sciences of Ukraine, B. Khmelnitsky 15 Str., Kiev, 01601, Ukraine; Institute of Geological Sciences, National Academy of Sciences of Ukraine, O. Gonchar Str. 55b, Kiev, 01054, Ukraine; Faculty of Geology, University of Warsaw, ul. Żwirki i Wigury 93, Warszawa, 02-089, Poland
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GB/T 7714
Łanczont M.,Bogucki A.,Yatsyshyn A.,et al. Stratigraphy and chronology of the periphery of the Scandinavian ice sheet at the foot of the Ukrainian Carpathians[J],2019,530.
APA Łanczont M..,Bogucki A..,Yatsyshyn A..,Terpiłowski S..,Mroczek P..,...&Tomeniuk O..(2019).Stratigraphy and chronology of the periphery of the Scandinavian ice sheet at the foot of the Ukrainian Carpathians.Palaeogeography, Palaeoclimatology, Palaeoecology,530.
MLA Łanczont M.,et al."Stratigraphy and chronology of the periphery of the Scandinavian ice sheet at the foot of the Ukrainian Carpathians".Palaeogeography, Palaeoclimatology, Palaeoecology 530(2019).
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