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...
Gardado en:
| Principais autores: | , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Institute of Oceanology of the Polish Academy of Sciences
2015-04-01
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| Series: | Oceanologia |
| Assuntos: | |
| Acceso en liña: | http://www.sciencedirect.com/science/article/pii/S0078323414000177 |
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