Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera-Reference-Cited by-同舟云学术

Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: Evidence from stable isotopic ratios of planktonic foraminifera

Published:2000-03 Issue:1 Volume:109 Page:153-156
ISSN:0253-4126
Container-title:Journal of Earth System Science
language:en
Short-container-title:J Earth Syst Sci

Author:

Ahmad S. M.,Patil D. J.,Rao P. S.,Nath B. N.,Rao B. R.,Rajagopalan G.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/BF02719159.pdf

Reference21 articles.

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2. Ahmad S M 1995 Carbon and oxygen isotopic records of planktonic and benthic foraminifera from a new deep sea core of the northeast Indian Ocean;Curr. Sci. 69 691–695

3. Alley R B and 10 others 1993 Abrupt increase in Greenland snow accumulation at the end of Younger Dryas event;Nature 362 527–529

4. Broecker W S, Andree M, Wolfil W, Oeschger H, Bonani G, Kennett J, Peteet D 1988 The chronology of the last deglaciation: Implications to the cause of Younger Dryas event;Paleoceanography 3 1–19

5. CLIMAP Project Members 1981 Seasonal reconstruction of the earth’s surface at the last glacial maximum;Geol. Soc. Am. Map Chart Ser. MC-36 Boulder CO

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