Abstract
Integrated study of the multilayer Zaktui site supplied a large volume of paleontological materials and a series of radiocarbon dates falling within the MIS 3–MIS 1 interval. Multidisciplinary data provided evidence of the past dynamics of environments and climate. Paleontological data point to a mosaic structure of landscapes, and suggest a temperate warm and humid climate in the south-western Baikal region during MIS 3 interval, with some regional deviations.
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