Abstract
The geological structure and faunal content of one of the principal localities for Quaternary mammal remains in Western Siberia, Krasniy Yar (Tomsk region, Russia) are considered. This locality contains 3 layers of bone remains: lower (Middle Neopleistocene), middle (the end of Late Neopleistocene) and upper (end of Neopleistocene—beginning of Holocene). The richest horizon in number of species and the quantity of remains is the middle horizon, which contains the mammoth fauna.
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