The main object to be considered is sediments of the Eemian (Mginsk) or Boreal, transgression. Some general trends of their distribution and biostratigraphic evidence are presented. These sediments have been long studied by many researchers, and the aim of this chapter is to summarize the results.
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© 2009 Springer-Verlag Berlin Heidelberg
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Levitan, M.A., Lavrushin, Y.A. (2009). Late Pleistocene Geologic-Paleoecological Events in the North of European Russia. In: Sedimentation History in the Arctic Ocean and Subarctic Seas for the Last 130 kyr. Lecture Notes in Earth Sciences, vol 118. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-00288-5_2
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DOI: https://doi.org/10.1007/978-3-642-00288-5_2
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