Epibenthic foraminifera stable isotope and planktic foraminifera Ba/Ca data of sediment core MD03-2664

Deep ocean circulation has been considered relatively stable during interglacial periods, yet little is known about its behavior on submillennial time scales. Using a subcentennially resolved epibenthic foraminiferal d13C record we show that North Atlantic Deep Water (NADW) influence was strong at t...

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Bibliographic Details
Main Authors: Galaasen, Eirik Vinje, Ninnemann, Ulysses S, Irvalı, Nil, Kleiven, Helga F, Rosenthal, Yair, Kissel, Catherine, Hodell, David A
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Arctic
arctic cryosphere
Foraminifera*
NADW
North Atlantic Deep Water
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.830081
https://doi.org/10.1594/PANGAEA.830081

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