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Mammals of the periglacial hyperzone of the end of the Pleistocene and formation of the modern rodent fauna in the mountains of Western and Middle Siberia.
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- Author(s): Dupal, T.; Andrenko, O.; Vinogradov, V.
- Source:
Contemporary Problems of Ecology; Feb2013, Vol. 6 Issue 1, p94-104, 11p- Subject Terms:
- Source:
- Additional Information
- Subject Terms:
- Abstract: The fossil and modern faunas of small mammals from the end of the Pleistocene to modern times in the south of West and Middle Siberia were analyzed. It was shown that during the Sartan, the typical hyperborean complex of mammals was spread to the middle reaches of the Yenisei. In the northwest of Altai a hyperborean complex of mammals of the southern type existed at the end of the Pleistocene; it had its specific regional features. Warming and an increase in humidity in the Holocene led to the disappearance of the periglacial landscape and reduction of the area occupied by the tundra-steppe ecotopes. Expansion of the forest belt resulted in degradation of the hyperborean complex of mammals. In the second half of the Holocene, the formation of forest and forest-steppe complexes of small mammals took place. [ABSTRACT FROM AUTHOR]
- Abstract: Copyright of Contemporary Problems of Ecology is the property of Springer Nature and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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