Glacial–interglacial contrast in deep-water δ13C of the Arabian Sea

Author:

Naik Smita N,Naik Sushant S

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference88 articles.

1. 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.

2. Ahmad S M, Babu G A, Padmakumari V M and Raza W 2008 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; Palaeogeogr. Palaeoclimatol. Palaeoecol. 262 182–188.

3. Banse K and English D C 1993 Revision of satellite-based phytoplankton pigment data from the Arabian Sea during northeast monsoon; J. Mar. Res. 2 83–103.

4. Banakar V K 2005 δ13C depleted oceans before the termination 2: More nutrient-rich deep-water formation or light-carbon transfer?; Indian J. Mar. Sci. 34(3) 249–258.

5. Bereiter B, Shackleton S, Baggenstos D, Kawamura K and Severinghaus J 2018 Mean global ocean temperatures during the last glacial transition; Nature 553 39–44.

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