2019 Dubrivka Scandinavian I
Palaeogeography, Palaeoclimatology, Palaeoecology 530 (2019) 59–77 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Stratigraphy and chronology of the periphery of the Scandinavian ice sheet T at the foot of the Ukrainian Carpathians Maria Łanczonta, Andriy Boguckib, Andriy Yatsyshynb, Sławomir Terpiłowskia, ⁎ Przemysław Mroczeka, , Anna Orłowskaa, Beata Hołuba, Paweł Zielińskia, Maryna Komarc,d, Barbara Woronkoe, Piotr Kuleszaa, Roman Dmytrukb, Olena Tomeniukb a Faculty of Earth Sciences and Spatial Management, Maria Curie-Skłodowska University, Al. Kraśnicka 2d, 20-718 Lublin, Poland b Faculty of Geography, Ivan Franko National University, Doroshenka Str. 41, 79000 Lviv, Ukraine c National Museum of Natural History, National Academy of Sciences of Ukraine, B. Khmelnitsky 15 Str., 01601 Kiev, Ukraine d Institute of Geological Sciences, National Academy of Sciences of Ukraine, O. Gonchar Str. 55b, 01054 Kiev, Ukraine e Faculty of Geology, University of Warsaw, ul. Żwirki i Wigury 93, 02-089 Warszawa, Poland ARTICLE INFO ABSTRACT Keywords: The article presents the results of research on the formation conditions and the age of glaciogenic deposits left by Fluvial and glaciogenic deposits the Scandinavian ice sheet in the Eastern Carpathian Foreland, in its part drained by the Dniester River and its Loess–palaeosol sequences tributaries (Black Sea basin). These deposits (till, erratics, glaciolacustrine and glaciofluvial sediments), pre- Elsterian glaciation served only in some places and occurring in the range of altitudes defined by terrace VI (Early Pleistocene) and Palaeoreconstructions terrace V (Middle Pleistocene), are the southernmost traces of the ice sheet in Europe. They are underlain by Pleistocene fluvial deposits and overlain by loess deposits, and locally occur as intraloess layers.
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