Planktic foraminiferal δ18O values indicate precipitation variability in the southeastern South China Sea over the last 175 ka BP

Author:

Zhou QixianORCID,Yin Jian,Yang Xiaoqiang,Chen Qiong,Xie Yixuan,Zhang Huodai

Funder

National Natural Science Foundation of China

Guangdong Province Introduction of Innovative R&D Team

Publisher

Elsevier BV

Subject

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

Reference74 articles.

1. Global Hydrological Isotope Data and Data Networks;Aggarwal,2010

2. The history and variability of the East Asian paleomonsoon climate;An;Quat. Sci. Rev.,2000

3. A study of cleaning procedures used for foraminifer Mg/Ca paleothermometry;Barker;G-cubed,2013

4. Reevaluation of the oxygen isotope composition of planktonic foraminifera: experimental results and revised paleotemperature equations;Bemis;Paleoceanography,1998

5. Interglacials of the last 800,000 years;Berger;Rev. Geophys.,2015

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