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...
Main Authors: | , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2006
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.727694 https://doi.org/10.1594/PANGAEA.727694 |