Enviar artigo por via de e-mail A Polychronous Locality of Megafauna on the Northwestern Coast of Lake Baikal
- Autores: Kalmykov N.P.1, Budaev R.T.2
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Afiliações:
- Institute of Arid Zones, Southern Science Center, Russian Academy of Sciences
- Geological Institute, Siberian Branch, Russian Academy of Sciences
- Edição: Volume 483, Nº 2 (2018)
- Páginas: 1487-1490
- Seção: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/194398
- DOI: https://doi.org/10.1134/S1028334X18120036
- ID: 194398
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Resumo
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.
Sobre autores
N. Kalmykov
Institute of Arid Zones, Southern Science Center,Russian Academy of Sciences
Autor responsável pela correspondência
Email: kalm@ssc-ras.ru
Rússia, Rostov-on-Don, 344006
R. Budaev
Geological Institute, Siberian Branch, Russian Academyof Sciences
Email: kalm@ssc-ras.ru
Rússia, Ulan-Ude, 670047
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