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


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Abstract

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.

About the authors

Ye. A. Novichkova

Shirshov Institute of Oceanology

Author for correspondence.
Email: enovichkova@mail.ru
Russian Federation, Moscow, 117997

L. Ye. Reikhard

Shirshov Institute of Oceanology

Email: enovichkova@mail.ru
Russian Federation, Moscow, 117997

A. P. Lisitzin

Shirshov Institute of Oceanology

Email: enovichkova@mail.ru
Russian Federation, Moscow, 117997

A. Ye. Rybalko

JSC Sevmorgeo

Email: enovichkova@mail.ru
Russian Federation, St. Petersburg, 198095

A. de Vernal

University of Quebec

Email: enovichkova@mail.ru
Canada, Montreal

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