(Table 3) Oxygen isotope ratios of benthic foraminifera from DSDP Hole 80-548

Presently, the intermediate depths of the North Atlantic Ocean are occupied by a great lens of warm, saline water whose source is the Mediterranean Sea. This water flows both westward and northward, finally entering the Norwegian Sea where it may contribute to the formation of North Atlantic Deep Wa...

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Bibliographic Details
Main Author: Loubere, Paul
Format: Dataset
Language:English
Published: PANGAEA 1987
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.761049
https://doi.org/10.1594/PANGAEA.761049