Deep water masses in the Iceland Basin during the Last Interglacial (MIS 5e): Evidence from benthic foraminiferal data

Deep water masses in the Iceland Basin during the Last Interglacial (MIS 5e): Evidence from benthic foraminiferal data

The Last Interglacial period, marine isotope stage (MIS) 5e, is a potential analogue for the Holocene. In this study, we investigated a marine sediment core, AMK-4442, recovered from the northern part of the Iceland Basin. The multiproxy approach used in this study, which includes foraminiferal and...

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Bibliographic Details
Main Authors: Nadezhda P. Lukashina, Leyla D. Bashirova
Format: Article
Language:English
Published: Elsevier 2015-04-01
Series:Oceanologia
Subjects:
Holocene
Last Interglacial
Paleoceanography
Deep water circulation
Benthic foraminifera
Online Access:http://www.sciencedirect.com/science/article/pii/S0078323414000177

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http://www.sciencedirect.com/science/article/pii/S0078323414000177

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