Published November 8, 1990
| public
Journal Article
Oxygen in the Arabian Sea
- Creators
- Krishnamurthy, R. V.
Abstract
Sir-Variations in the oxigen isotope content (δ^(18)O) of planktonic foraminifera from the Arabian Sea have been cited as evidence for stronger northeast monsoon current at the last glacial maximum (LGM), about 18 kyr ago, than during the present day.
Additional Information
© 1990 Nature Publishing Group.Additional details
- Eprint ID
- 57493
- Resolver ID
- CaltechAUTHORS:20150513-104311043
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2015-05-13Created from EPrint's datestamp field
- Updated
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2021-11-10Created from EPrint's last_modified field