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

Oxygen-18 records of benthic foraminifera from the Atlantic Ocean are significantly different from those of the Pacific and Indian Oceans indicating that the Glacial North Atlantic Deep Water was about 1.3°C cooler than today because different deep water sources appeared in the North Atlantic Ocean...

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Bibliographic Details
Main Author: Duplessy, Jean-Claude
Format: Dataset
Language:English
Published: PANGAEA 1982
Subjects:
PC
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.726217
https://doi.org/10.1594/PANGAEA.726217