Stable carbon and oxygen isotope ratios of foraminifera from Holocene sediments of the North Atlantic

The Denmark Strait Overflow (DSO) today compensates for the northward flowing Norwegian and Irminger branches of the North Atlantic Current that drive the Nordic heat pump. During the Last Glacial Maximum (LGM), ice sheets constricted the Denmark Strait aperture in addition to ice eustatic/isostatic...

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Bibliographic Details
Main Authors: Millo, Christian, Sarnthein, Michael, Voelker, Antje H L, Erlenkeuser, Helmut
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
ARK-XVIII/1
Giant box corer
GIK23519-4
GIK23519-5
GKG
Gravity corer (Kiel type)
Greenland Sea
Iceland Sea
Impact of Gateways on Ocean Circulation
Climate
and Evolution
OceanGateways
Ocean Gateways
Oceanpassagen
PC
Piston corer
Polarstern
POS210/2
Poseidon
PS62
PS62/003-2
PS62/004-3
PS62/015-3
SL
Greenland
Irminger Basin
Mid-Atlantic Ridge
Denmark Strait
Iceland
Nordic Seas
north atlantic current
North Atlantic Deep Water
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.727694
https://doi.org/10.1594/PANGAEA.727694

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