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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Hauptverfasser:	Nadezhda P. Lukashina, Leyla D. Bashirova
Format:	Artigo
Sprache:	Inglês
Veröffentlicht:	Institute of Oceanology of the Polish Academy of Sciences 2015-04-01
Schriftenreihe:	Oceanologia
Schlagworte:	Holocene Last Interglacial Paleoceanography Deep water circulation Benthic foraminifera
Online-Zugang:	http://www.sciencedirect.com/science/article/pii/S0078323414000177
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