Oxygen in the Arabian Sea
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.
| Published in: | Nature |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
Nature Publishing Group
1990
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| Subjects: | |
| Online Access: | https://authors.library.caltech.edu/57493/ https://resolver.caltech.edu/CaltechAUTHORS:20150513-104311043 |
| Summary: | 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. |
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