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


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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.

Sobre autores

Ye. Novichkova

Shirshov Institute of Oceanology

Autor responsável pela correspondência
Email: enovichkova@mail.ru
Rússia, Moscow, 117997

L. Reikhard

Shirshov Institute of Oceanology

Email: enovichkova@mail.ru
Rússia, Moscow, 117997

A. Lisitzin

Shirshov Institute of Oceanology

Email: enovichkova@mail.ru
Rússia, Moscow, 117997

A. Rybalko

JSC Sevmorgeo

Email: enovichkova@mail.ru
Rússia, St. Petersburg, 198095

A. de Vernal

University of Quebec

Email: enovichkova@mail.ru
Canadá, Montreal

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