New data on the Holocene evolution of the Dvina Bay (White Sea)
- Authors: Novichkova Y.A.1, Reikhard L.Y.1, Lisitzin A.P.1, Rybalko A.Y.2, de Vernal A.3
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Affiliations:
- Shirshov Institute of Oceanology
- JSC Sevmorgeo
- University of Quebec
- Issue: Vol 474, No 1 (2017)
- Pages: 607-611
- Section: Oceanology
- URL: https://ogarev-online.ru/1028-334X/article/view/189994
- DOI: https://doi.org/10.1134/S1028334X17050233
- ID: 189994
Cite item
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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