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DOI | 10.1016/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 |
ISSN | 0031-0182 |
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
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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 |
推荐引用方式 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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