New evidence of the late neopleistocene peoplingof the lower ob valley

I. D. Zolnikov, A. A. Anoikin, E. A. Filatov, A. V. Vybornov, A. V. Vasiliev, A. V. Postnov, L. V. Zotkina

Результат исследования: Научные публикации в периодических изданияхстатьярецензирование


This study focuses on the early human occupation of the arctic part of the West Siberian Plain and introduces the fi nds at the Paleolithic site Kushevat (Shuryshkarsky District, Yamal-Nenets Autonomous Okrug), discovered in 2020. Geological and geomorphological characteristics of the Lower Ob region are provided, the chronology of the key Middle and Late Neopleistocene sequences is assessed, and criteria underlying the search for Paleolithic sites in the area are outlined. We describe the discovery and excavations at Kushevat, its stratigraphy and its faunal remains. On the basis of correlation with neighboring key Late Neopleistocene sections with a representative series of absolute dates, the age of the site is estimated at cal 50-35 ka BP. Results of a traceological study of a possibly human-modifi ed reindeer antler are provided. Findings at Kushevat and the available information on the early peopling of northern Eurasia suggest that the boundary of the inhabited part of that region must be shifted -200 km to the north. The Ob, therefore, is one of the last major Siberian rivers where traces of the Early Upper Paleolithic culture have been found. The discovery of a stratifi ed site in its lower stretch is a milestone in the Paleolithic studies in the region. A large area over which faunal remains are distributed, and the presence of lithics among the surface fi nds, suggest that Kushevat is a highly prospective site for future archaeological studies of the early stages in the human peopling of the region.

Язык оригиналаанглийский
Страницы (с-по)9-20
Число страниц12
ЖурналArchaeology, Ethnology and Anthropology of Eurasia
Номер выпуска1
СостояниеОпубликовано - 2021

Предметные области OECD FOS+WOS



Подробные сведения о темах исследования «New evidence of the late neopleistocene peoplingof the lower ob valley». Вместе они формируют уникальный семантический отпечаток (fingerprint).