Surface and deep water changes in the northeast Indian Ocean during the last 60 ka inferred from carbon and oxygen isotopes of planktonic and benthic foraminifera-Reference-Cited by-同舟云学术

Surface and deep water changes in the northeast Indian Ocean during the last 60 ka inferred from carbon and oxygen isotopes of planktonic and benthic foraminifera

Published:2008-06 Issue:3-4 Volume:262 Page:182-188
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Ahmad S. Masood,Babu G. Anil,Padmakumari Vathachira M.,Raza Waseem

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference42 articles.

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2. Glacial–interglacial changes in the surface water characteristics of the Andaman Sea: evidence from the stable isotopic ratios of planktonic foraminifera;Ahmad;Proceedings Indian Academy of Sciences,2000

3. Radiocarbon age differences between coexisting foraminiferal species;Broecker;Paleoceanography,1999

4. Anomalous radiocarbon ages for foraminifera shells;Broecker;Paleoceanography,2006

5. Evidence from Southern Ocean sediments for the effect of North Atlantic Deep Water flux on climate;Charles;Nature,1992

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