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Archaeology, Ethnology & Anthropology of Eurasia
51 (2) 2023
doi:10.17746/1563-0110.2023.51.2.027-037
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Annotation:
The Kushevat Site and the Paleogeographic Context
of the Initial Peopling of Northern Urals
I.D. Zolnikov1, 2, A.A. Anoikin3, 4, R.N. Kurbanov5, 6, E.A. Filatov1, 3, L.V. Zotkina3, A.V. Vybornov1, 3, A.V. Postnov3, E.V. Parkhomchuk2, 3, and M.O. Filatova3
1Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
2Novosibirsk State University, Pirogova 2, Novosibirsk, 630090, Russia
3Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, Pr. Akademika Lavrentieva 17, Novosibirsk, 630090, Russia
4Altai State University, Pr. Lenina 61, Barnaul, 656049, Russia
5Institute of Geography, Russian Academy of Sciences, Staromonetny per. 29, Moscow, 119017, Russia
6Lomonosov Moscow State University, Leninskie Gory 1, Moscow, 119991, Russia
On the basis of new materials excavated in 2019-2021 from the Upper Paleolithic site of Kushevat, this study addresses the problem of initial human occupation of the Subpolar Urals. Geological and geomorphological findings are presented along with new chronological and paleogeographical data. Archaeological and faunal materials are described, and results of the traceological analysis of reindeer antlers with cut and chop marks are presented. The findings suggest that Kushevat was a pioneer settlement of the northern Ob region. The obtained luminescence and radiocarbon ages suggest that the peopling of the Lower Ob region occurred prior to 30 ka BP. Climatic conditions during the first half of the Upper Paleolithic (55-25 ka BP) were favorable for humans in the subpolar zone. Geological and geomorphological situation at the Upper Paleolithic sites of northwestern Urals (the Pechora and Kama basins) can be used as a paleogeographic analogue of the conditions in the Lower Ob region during the Pleistocene. The principal Upper Paleolithic sites in the region are associated with accumulations of megafaunal remains in the mouths of ancient gullies. Archaeological sites apparently consisted of two areas differing in location, economic specialization, and toolkit. Areas of the first type include residential zones on leveled areas of the second river terraces adjacent to the ravines. Those of the second type are estuarine zones of modern valleys of streams and rivers, where huge accumulations of megafaunal remains are preserved at the bottoms of ancient ravines.
Keywords: Northern Urals, Upper Paleolithic, Terminal Late Pleistocene, paleontology, paleogeography, traceology