Abstract
This paper presents the results of SEM-examination of palynological complexes of two paleosols at the base of the Staraya Ladoga section. There was obtained evidence of the floodplain genesis of the paleosol directly under- lying the cultural layer of Zemlyanoye hillfort. A new palynological marker has been identified here which enables us to ground the synchronous character of the end of the Ladoga Transgression (in the southern Ladoga region) and the regression of Lake Ilmen (in the northwestern region).
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