Abstract
During the last decades a considerable amount of data on mammals from Mikulino (=Eemian) deposits of the central and southern parts of the Russian Plain has been produced. Mammuthus primigenius (the early type), Palaeoloxodon antiquus (the advanced form), Arvicola ex gr. terrestris, Eolagurus cf. luteus and Lagurus cf. lagurus characterize this period. The so-called 'Shkurlatian mammal assemblage' was distinguished on the basis of a number of Eemian faunas. The age of the mammal localities was established by using various geological and palaeontological evidence, together with the results of palaeomagnatic studies and absolute dating. The evolutionary level of the diagnostic species allows correlations between localities from different parts of the Russian Plain that have varying taphonomical conditions. The mammal- and malacofauna of the Mikulino Interglacial can also be used as a basis for correlations between the Karangat marine strata of the Black Sea and the continental deposits (alluvial sediments of the second terrace of the Sudost' River and the Salyn phase of the Mezin fossil pedocomplex (see Dodonov et al., this volume). Forest, forest-steppe and steppe zone landscapes have been reconstructed for the central and southern parts of the Russian Plain on the basis of the Eemian faunas.
Author supplied keywords
Cite
CITATION STYLE
Markova, A. K. (2000). The Mikulino (= Eemian) mammal faunas of the Russian Plain and Crimea. Geologie En Mijnbouw/Netherlands Journal of Geosciences, 79(2–3), 293–301. https://doi.org/10.1017/s0016774600021776
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.