(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...
Main Author: | |
---|---|
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 |