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Spatial and temporal regularities in the evolution of vegetation and climate of North Eurasia in the Neopleistocene

Spatial and temporal regularities in the evolution of vegetation and climate of North Eurasia in... PALEOENVIRONMENT. THE STONE AGE DOI: 10.1134/S1563011007040019 N.S. Bolikhovskaya Moscow State University, Moscow, GSP-1, 119991, Russia E-mail: nbolikh@geogr.msu.ru 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 http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Archaeology, Ethnology and Anthropology of Eurasia Springer Journals

Spatial and temporal regularities in the evolution of vegetation and climate of North Eurasia in the Neopleistocene

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Publisher
Springer Journals
Copyright
Copyright © 2007 by N.S. Bolikhovskaya
Subject
Social Sciences, general; Archaeology; Regional and Cultural Studies; Anthropology
ISSN
1563-0110
eISSN
1531-832X
DOI
10.1134/S1563011007040019
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Abstract

PALEOENVIRONMENT. THE STONE AGE DOI: 10.1134/S1563011007040019 N.S. Bolikhovskaya Moscow State University, Moscow, GSP-1, 119991, Russia E-mail: nbolikh@geogr.msu.ru 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

Journal

Archaeology, Ethnology and Anthropology of Eurasia – Springer Journals

Published: Feb 18, 2007

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