Microalgae and the Climate of the North Atlantic

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Abstract

The results of a micropaleontological study of the sediment core obtained in the northeastern part of the Norwegian–Greenland basin from a sea depth of 3013 m are presented. The microalgae species composition indicates repeated changes in marine environments during the sedimentation.

About the authors

T. S Klyuvitkina

Lomonosov Moscow State University

Email: t.klyuvitkina@mail.ru
Moscow, Russia

E. A Novichkova

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

L. A Kireenko

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

M. P Chekhovskaya

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

A. G Matul

Shirshov Institute of Oceanology, Russian Academy of Sciences

Moscow, Russia

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