Abstract
434 This paper continues a series of publications devoted to study of bottom sediments of small lakes formed in local coastal depressions during retreat of the White Sea shoreline due to glacioisostatic uplift of the Baltic Shield. These studies allow us to define the timeline of shoreline position changes and, hence, estimate the rate of land uplift for different territories, depending on the paleogeographic, tectonic, and geo� morphological features of a given site. Previous studies [1, 2] have established that the sequences of bottom sediments from the lake basins on the White Sea coast are represented by five facies dif� fering in the lithological and microfossil characteris�
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