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...

Бүрэн тодорхойлолт

Номзүйн дэлгэрэнгүй

Үндсэн зохиолчид:	Nadezhda P. Lukashina, Leyla D. Bashirova
Формат:	Artigo
Хэл сонгох:	Inglês
Хэвлэсэн:	Institute of Oceanology of the Polish Academy of Sciences 2015-04-01
Цуврал:	Oceanologia
Нөхцлүүд:	Holocene Last Interglacial Paleoceanography Deep water circulation Benthic foraminifera
Онлайн хандалт:	http://www.sciencedirect.com/science/article/pii/S0078323414000177
Шошгууд:	Шошго нэмэх Шошго байхгүй, Энэхүү баримтыг шошголох эхний хүн болох!