A 23000 year old record of paleoclimatic and environmental changes from the eastern Arabian Sea

Author:

Saravanan Ponnusamy,Gupta Anil K.,Zheng Hongbo,Majumder Jeet,Panigrahi Mruganka K.,Kharya Aditya

Funder

Ministry of Earth Sciences

National Natural Science Foundation of China

Strategic Priority Research Program of Chinese Academy of Sciences

Second Tibetan Plateau Expedition and Research

Publisher

Elsevier BV

Subject

Paleontology,Oceanography

Reference127 articles.

1. Oxygen Minimum Zone Vis-À-Vis distribution of carbon and phosphorus in the eastern Arabian Shelf: A geochemical reappraisal;Acharya,2016

2. The effect of millennial-scale changes in Arabian Sea denitrification on atmospheric CO2;Altabet;Nature,2002

3. Scaling percetages and distributional patterns of benthic foraminifera with flux rates of organic carbon;Altenbach;J. Foraminifer. Res.,1999

4. Impact of interrelated and interdependent ecological controls on benthic foraminifera: an example from the Gulf of Guinea;Altenbach;Palaeogeography, Palaeoclimatology, Palaeoecology,2003

5. The structure of the southwest monsoon winds over the Arabian Sea during the late Quaternary: observations, simulations, and marine Geological evidence;Anderson;J. Geophys. Res.,1992

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