δ18O and salinity variability from the Last Glacial Maximum to Recent in the Bay of Bengal and Andaman Sea-Reference-Cited by-同舟云学术

δ18O and salinity variability from the Last Glacial Maximum to Recent in the Bay of Bengal and Andaman Sea

Published:2016-03 Issue: Volume:135 Page:79-91
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Sijinkumar A.V.^ORCID,Clemens Steven,Nath B. Nagender,Prell Warren,Benshila Rachid,Lengaigne Matthieu

Funder

Brown University

CSIR

IFCPAR

Publisher

Elsevier BV

Subject

Geology,Archaeology,Archaeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference63 articles.

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3. Glacial-interglacial changes in the surface water characteristics of the Andaman Sea: evidence from stable isotopic ratios of planktonic foraminfera;Ahmad;Proc. Indian Acad. Sci. (Earth Planet. Sci.),2000

4. A modeling study of the processes of surface salinity seasonal cycle in the Bay of Bengal;Akhil;J. Geophys. Res.,2014

5. South Asian monsoon history over the past 60 kyr recorded by radiogenic isotopes and clay mineral assemblages in the Andaman Sea;Ali;Geochem. Geophys. Geosyst.,2015

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