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The Pleistocene loess-soil sequence from West Siberia has provided a continuous record of Quaternary climate change in Northern Asia. The Middle-Late Pleistocene loess-paleosol stratigraphy of West Siberia has become recently a subject of discussion after a considerable revision was suggested by equating the Shipunovo pedocomplex to the Late Pleistocene stage 5 (MIS 5) instead of the previous correlation...
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