Мақаланы E-mail арқылы жіберу A Polychronous Locality of Megafauna on the Northwestern Coast of Lake Baikal
- Авторлар: Kalmykov N.P.1, Budaev R.T.2
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Мекемелер:
- Institute of Arid Zones, Southern Science Center, Russian Academy of Sciences
- Geological Institute, Siberian Branch, Russian Academy of Sciences
- Шығарылым: Том 483, № 2 (2018)
- Беттер: 1487-1490
- Бөлім: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/194398
- DOI: https://doi.org/10.1134/S1028334X18120036
- ID: 194398
Дәйексөз келтіру
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Аннотация
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.
Авторлар туралы
N. Kalmykov
Institute of Arid Zones, Southern Science Center,Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: kalm@ssc-ras.ru
Ресей, Rostov-on-Don, 344006
R. Budaev
Geological Institute, Siberian Branch, Russian Academyof Sciences
Email: kalm@ssc-ras.ru
Ресей, Ulan-Ude, 670047
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