В статье приведены результаты диатомового анализа голоценовых отложений, полученных из кутовой части Ругозерской губы Кандалакшского залива Белого моря. В исследованных осадках выделены 5 диатомовых зон, отражающих основные этапы эволюции природной среды, начиная с середины атлантического периода.
In this paper we present the results of diatom study of Holocene sediments from the inner part of the Rugozerskaya Bay (Kandalaksha Bay of the White Sea). Five diatom ecological zones were established, that clarify the main stages of the natural environment evolution, since the second part of the Atlantic.
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