The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal

Author:

Yu Zhoufei,Li Baohua,Li Hongliang,Zhang Jingjing,Chen Jianfang

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Tongji University

State Key Laboratory of Marine Geology

National Program on Global Change and Air-Sea Interaction

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference68 articles.

1. Planktonic Foraminifera in the Sea of Okhotsk: Population and Stable Isotopic Analysis from a Sediment Trap. Master thesis;Alderman,1996

2. Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series;Anand;Paleoceanography,2003

3. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations;Bemis;Paleoceanography,1998

4. Carbon and oxygen isotopic composition of planktonic foraminifera from laboratory culture, plankton tows and recent sediment; implications for the reconstruction of paleoclimatic conditions and of the global carbon cycle;Bouvier-Soumagnac;J. Foraminiferal Res.,1985

5. Preliminary report on the stable isotopic change of planktonic foraminifers from the sediment traps in the central South China Sea (In Chinese with English abstract);Cheng;Mar. Geol. Quat. Geol.,2002

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