Radiocarbon evidence for reduced deep water ventilation of the northern Indian Ocean during the last glacial maxima and early deglaciation

Author:

Nisha KumariORCID,Naik Sushant Suresh,Kumar Pankaj,Banerjee Barnita,Murty P.B. Rama

Funder

University Grants Commission

National Institute of Oceanography, India

Inter-University Accelerator Centre

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference63 articles.

1. Glacial to Holocene changes in the surface and deep waters of the northeast Indian Ocean;Ahmad;Mar. Geol.,2012

2. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2;Anderson;Science,2009

3. Deep-water circulation over the last two glacial cycles reconstructed from authigenic neodymium isotopes in the equatorial Indian Ocean (core HI1808-GPC04);Bang;Ocean Sci. J.,2021

4. Extreme deepening of the Atlantic overturning circulation during deglaciation;Barker;Nat. Geosci.,2010

5. Evidence of poorly ventilated deep central Indian Ocean during the last glaciation;Bharti;Earth Planet. Sci. Lett.,2022

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