Access the full text.
Sign up today, get DeepDyve free for 14 days.
PALEOENVIRONMENT. THE STONE AGE DOI: 10.1134/S1563011007040019 N.S. Bolikhovskaya Moscow State University, Moscow, GSP-1, 119991, Russia E-mail: email@example.com SPATIAL AND TEMPORAL REGULARITIES IN THE EVOLUTION OF VEGETATION AND CLIMATE OF NORTH EURASIA IN THE NEOPLEISTOCENE* Introduction southeastern Massif Central in France (Reille, Beaulieu de, 1995; Reille et al., 1998), Castiglione in Central In view of the incompleteness of the Pleistocene geological Italy (Follieri, Magri, Sadori, 1988), Tenagi Philippon record in most parts of North Eurasia, the subdivision of (Wijmstra, 1969; Hammen, Wijmstra, Zagwijn, 1971; the most recent deposits and the correlation of glacial and Wijmstra, Smit, 1976; Wijmstra, Groenhart, 1983) and interglacial horizons with climatic and geographic events Ioannina (Tzedakis, 1993; Tzedakis et al., 2001) in must be primarily derived from spatial and temporal Greece, as well as from proﬁ les in central and southern regularities in the evolution of vegetation and climate, parts of Eastern Europe – Likhvin on the upper Oka established on the basis of geographic criteria for the best (Bolikhovskaya, 1974, 1976, 1995b), Odintsovo in the known stratigraphic sequences of a region. Moscow area (Maudina, Pisareva, Velichkevich, 1985), The pioneering studies in the evolution of Pleistocene Strelitsa on the upper Don (Bolikhovskaya, 1976, environments were those
Archaeology, Ethnology and Anthropology of Eurasia – Springer Journals
Published: Feb 18, 2007
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.