Institut für Biologie der Martin-Luther-Universität Halle-Wittenberg
Date of this Version
2010
Document Type
Article
Citation
Erforschung biologischer Ressourcen der Mongolei (2010) band 11: 267-279.
Abstract
Geomorphological, geochemical, sedimentological and palynological results are presented against the background of palaeoclimatic changes during the past 15,000 years, yielding a chrono-, bio- and morphostratigraphical model of landscape evolution in the region of northern Central Asia. Holocene and Late-Glacial climatic fluctuations there are shown to correlate well with conditions in central Europe. Particular attention is given to the importance of the palaeoclimatic interpretation of lake Basin sediments when reconstructing the palaeoenvironment.
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Comments
Copyright 2010, Martin-Luther-Universität Halle Wittenberg, Halle (Saale). Used by permission.