New data on the Holocene evolution of the Dvina Bay (White Sea)

Аннотация

The Holocene sediments from the inner part of the Dvina Bay of the White Sea (core no. 6042) were analyzed with multidisciplinary methods for the first time. The age of the sediments was determined using biostratigraphy and AMS ¹⁴C method. The result of analytical studies indicate two major stages of sedimentation in the bay during the Holocene. The water masses parameters were reconstructed and the results were compared with the modern data on the coastal sediments of the White Sea region.