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Hunter-gatherer foraging ranges, migrations, and travel in the middle Holocene Baikal region of Siberia: insights from carbon and nitrogen stable isotope signatures

Hunter-gatherer foraging ranges, migrations, and travel in the middle Holocene Baikal region of Siberia: insights from carbon and nitrogen stable isotope signatures
Hunter-gatherer foraging ranges, migrations, and travel in the middle Holocene Baikal region of Siberia: insights from carbon and nitrogen stable isotope signatures
Foragingranges, migrations, and travel among MiddleHolocenehunter–gatherers in the Baikalregion of Siberia are examined based on carbon and nitrogenstableisotopesignatures obtained from 350 human and 203 faunal bone samples. The human materials represent Early Neolithic (8000–6800 cal BP), Late Neolithic (6000–5000 cal BP), and Early Bronze Age periods (?5000–4000 cal BP) and come from the following four smaller areas of the broader region: the Angara and upper Lena valleys, Little Sea of Baikal’s northwest coast, and southwest Baikal. Forager diets from each area occupy their own distinct position within the stableisotope spectrum. This suggests that foragingranges were not as large as expected given the distances involved and the lack of geographic obstacles between the micro-regions. All examined individuals followed a similar subsistence strategy: harvesting game and local fishes, and on Lake Baikal also the seal, and to a more limited extent, plant foods. Although well established in their home areas, exchange networks with the other micro-regions appear asymmetrical both in time and direction: more travel and contacts between some micro-regions and less between others. The Angara valley seems to be the only area with the possibility of a temporal change in the foraging strategy from more fishing during the Early Neolithic to more ungulate hunting during the Late Neolithic–Early Bronze Age. However, the shift in stableisotope values suggesting this change can be viewed also as evidence of climate change affecting primary productivity of the Baikal–Angara freshwater system
0278-4165
523-548
Weber, Andzej W.
acd23aa9-4421-4bed-a886-de09e7688f0f
White, Dustin
5c77fb12-78b8-4a94-b25a-8697ccf5480b
Bazaliiskii, Vladimir I.
e468f096-37a5-4981-a7ad-ce8c024e554f
Goriunova, Oolga I.
f599552e-8f17-49c0-95d1-ed9c5f0e9ff1
Savel'ev, Nikolai
ea47d8de-5680-4ffd-92a6-daec8513b0c1
Katzenberg, M. Anne
78f28e35-9078-49e1-9455-77129e79940c
Weber, Andzej W.
acd23aa9-4421-4bed-a886-de09e7688f0f
White, Dustin
5c77fb12-78b8-4a94-b25a-8697ccf5480b
Bazaliiskii, Vladimir I.
e468f096-37a5-4981-a7ad-ce8c024e554f
Goriunova, Oolga I.
f599552e-8f17-49c0-95d1-ed9c5f0e9ff1
Savel'ev, Nikolai
ea47d8de-5680-4ffd-92a6-daec8513b0c1
Katzenberg, M. Anne
78f28e35-9078-49e1-9455-77129e79940c

Weber, Andzej W., White, Dustin, Bazaliiskii, Vladimir I., Goriunova, Oolga I., Savel'ev, Nikolai and Katzenberg, M. Anne (2011) Hunter-gatherer foraging ranges, migrations, and travel in the middle Holocene Baikal region of Siberia: insights from carbon and nitrogen stable isotope signatures. Journal of Anthropological Archaeology, 30 (4), 523-548. (doi:10.1016/j.jaa.2011.06.006).

Record type: Article

Abstract

Foragingranges, migrations, and travel among MiddleHolocenehunter–gatherers in the Baikalregion of Siberia are examined based on carbon and nitrogenstableisotopesignatures obtained from 350 human and 203 faunal bone samples. The human materials represent Early Neolithic (8000–6800 cal BP), Late Neolithic (6000–5000 cal BP), and Early Bronze Age periods (?5000–4000 cal BP) and come from the following four smaller areas of the broader region: the Angara and upper Lena valleys, Little Sea of Baikal’s northwest coast, and southwest Baikal. Forager diets from each area occupy their own distinct position within the stableisotope spectrum. This suggests that foragingranges were not as large as expected given the distances involved and the lack of geographic obstacles between the micro-regions. All examined individuals followed a similar subsistence strategy: harvesting game and local fishes, and on Lake Baikal also the seal, and to a more limited extent, plant foods. Although well established in their home areas, exchange networks with the other micro-regions appear asymmetrical both in time and direction: more travel and contacts between some micro-regions and less between others. The Angara valley seems to be the only area with the possibility of a temporal change in the foraging strategy from more fishing during the Early Neolithic to more ungulate hunting during the Late Neolithic–Early Bronze Age. However, the shift in stableisotope values suggesting this change can be viewed also as evidence of climate change affecting primary productivity of the Baikal–Angara freshwater system

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Published date: December 2011
Organisations: Archaeology

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Local EPrints ID: 345473
URI: http://eprints.soton.ac.uk/id/eprint/345473
ISSN: 0278-4165
PURE UUID: 5565c520-e4d8-48d8-bac8-571c9c41bdc0

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Date deposited: 22 Nov 2012 14:52
Last modified: 14 Mar 2024 12:25

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Contributors

Author: Andzej W. Weber
Author: Dustin White
Author: Vladimir I. Bazaliiskii
Author: Oolga I. Goriunova
Author: Nikolai Savel'ev
Author: M. Anne Katzenberg

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