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Oxygen in the Arabian Sea

Krishnamurthy, R. V. (1990) Oxygen in the Arabian Sea. Nature, 348 (6297). p. 118. ISSN 0028-0836. 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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URLURL TypeDescription
http://dx.doi.org/10.1038/348118a0DOIArticle
http://www.nature.com/nature/journal/v348/n6297/abs/348118a0.htmlPublisherArticle
Additional Information:© 1990 Nature Publishing Group.
Issue or Number:6297
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:03 Oct 2019 08:25

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