Kosinsky Mesolithic sites in the context of the history of the natural environment of the upper Kama region in the Late Glacial and early Holocene

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Abstract

The article presents the results of interdisciplinary (archaeological and palaeoecological) studies conducted in 2018–2021 in the northern part of the Perm Territory at the confluence of the Kosa and Lolog rivers. The main objects of research were the sites of the Mesolithic period and the natural environment of the Late Glacial and Early Holocene. To identify the confinement of archaeological sites to certain landforms within the river valley, the paleochannel method was used. As a result, 2 terraces and a Holocene floodplain were identified. For paleoenvironmental reconstruction palynological and paleocarpological methods were used. The radiocarbon method was used to create a chronological basis for the area of work. The study of the economic activities of Mesolithic groups was based on osteological analysis. In the Late Glacial period the study area was not yet inhabited by ancient people due to unfavorable natural environments. The settlement started only in the second half of the Boreal period of the Holocene, after the formation of the second terrace and the spread of taiga pine and birch forests with the participation of spruce. By this time, the sites of Kosa I and II, located on the banks of the Lolog river were inhabited. The population was mostly engaged in hunting and partly fishing. The natural environments at the beginning of the Atlantic period of the Holocene were still favorable for the existence of human groups here. Formation of the first terrace in the Lolog valley contributed to the colonization of this territory too. The Kosa III site dates back to this time, which population was still mainly engaged in hunting, and probably also fishing. Later, due to the continued lateral migration of the Kosa and Lolog river beds to the east and the emergence of waterlogged floodplains, people left this area and began to inhabit it again only in the Late Holocene.

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About the authors

D. A. Demakov

Perm State Humanitarian Pedagogical University

Author for correspondence.
Email: demakov-denis@mail.ru
SPIN-code: 8351-8408

аспирант кафедры Отечественной и всеобщей истории, археологии

Russian Federation, Perm

E. L. Lychagina

Perm State Humanitarian Pedagogical University; Perm State University

Email: demakov-denis@mail.ru
Russian Federation, Perm; Perm

N. E. Zaretskaya

Institute of Geography, RAS; Geological Institute, RAS

Email: demakov-denis@mail.ru
Russian Federation, Moscow; Moscow

S. V. Kopytov

Perm State University

Email: demakov-denis@mail.ru
Russian Federation, Perm

A. V. Chernov

Lomonosov Moscow State University; Moscow Pedagogical State University

Email: demakov-denis@mail.ru
Russian Federation, Moscow; Moscow

E. G. Lapteva

Institute of Plant and Animal Ecology Urals Branch of the RAS

Email: demakov-denis@mail.ru
Russian Federation, Yekaterinburg

S. S. Trofimova

Institute of Plant and Animal Ecology Urals Branch of the RAS

Email: demakov-denis@mail.ru
Russian Federation, Yekaterinburg

P. A. Kosintsev

Institute of Plant and Animal Ecology Urals Branch of the RAS

Email: demakov-denis@mail.ru
Russian Federation, Yekaterinburg

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Supplementary files

Supplementary Files
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1. JATS XML
2. Fig. 1. Study area.

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3. Fig. 2. Geomorphological map of the study area. 1 – low floodplain; 2 – high floodplain; 3 – 1st terrace; 4 – 2nd terrace; 5 – palaeochannels of Lolog and its tributaries on the 2nd terrace; 6 – location of boreholes and 14C dates; 7 – location of deep-drilling boreholes; 8 – archaeological sites: 1 – Kosa I, 2 – Kosa II, 3 – Kosa III; 9 – settlements.

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4. Fig. 3. The structure of sections (boreholes) of palaeochannel fillings in the vicinity of the Kosinsky sites and the results of radiocarbon dating. 1 – sand; 2 – silt; 3 – peat; 4 – silty peat (peaty silt); 5 – gyttja; 6 – 14C sampling sites; 7 – radiocarbon dates.

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5. Fig. 4. Pollen diagram of the culture-bearing and underlying sediments of the Kosa II site. 1 – sand “podzol”; 2 – sandy loam “cultural layer”; 3 – sand “sterile layer”.

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6. Fig. 5. The results of osteological analysis. The question mark means that the bones belong to an animal comparable in size to the one indicated.

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7. Fig. 6. Results of pollen and carpological analyses. Summary pollen diagram (а) and summary carpologic diagram (б) of Kosa boreholes.

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