Email this article A Polychronous Locality of Megafauna on the Northwestern Coast of Lake Baikal
- Authors: Kalmykov N.P.1, Budaev R.T.2
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Affiliations:
- Institute of Arid Zones, Southern Science Center, Russian Academy of Sciences
- Geological Institute, Siberian Branch, Russian Academy of Sciences
- Issue: Vol 483, No 2 (2018)
- Pages: 1487-1490
- Section: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/194398
- DOI: https://doi.org/10.1134/S1028334X18120036
- ID: 194398
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Abstract
Based on geochronological data, it is shown that the formation of sediments of a 50–80 m terrace of Lake Baikal occurred during the Middle Pleistocene and its top part was formed in the Late Pleistocene. This conclusion is confirmed by polychronous burials of mammals related to the early and late mammoth faunal complexes: Canis, Mammuthus, Equus, Coelodonta, Cervus, Capreolus, and Bison.
About the authors
N. P. Kalmykov
Institute of Arid Zones, Southern Science Center,Russian Academy of Sciences
Author for correspondence.
Email: kalm@ssc-ras.ru
Russian Federation, Rostov-on-Don, 344006
R. Ts. Budaev
Geological Institute, Siberian Branch, Russian Academyof Sciences
Email: kalm@ssc-ras.ru
Russian Federation, Ulan-Ude, 670047
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