Krishnamurthy, R. V. (1990) Oxygen in the Arabian Sea. Nature, 348 (6297). p. 118. ISSN 0028-0836. doi:10.1038/348118a0. https://resolver.caltech.edu/CaltechAUTHORS:20150513-104311043
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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.
| Item Type: | Article | |||||||||
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| Additional Information: | © 1990 Nature Publishing Group. | |||||||||
| Issue or Number: | 6297 | |||||||||
| DOI: | 10.1038/348118a0 | |||||||||
| Record Number: | CaltechAUTHORS:20150513-104311043 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20150513-104311043 | |||||||||
| Official Citation: | Oxygen in the Arabian Sea 118 R. V. KRISHNAMURTHY doi:10.1038/348118a0 | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 57493 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Ruth Sustaita | |||||||||
| Deposited On: | 13 May 2015 17:55 | |||||||||
| Last Modified: | 10 Nov 2021 21:50 |
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