Mg/Ca ratios of Globigerinoides sacculifer and sea surface temperature calculation of ODP Hole 184-1144A in the northen South China Sea (Appendix), supplement to: Wei, Gangjian; Deng, Wenfeng; Liu, Ying; Li, Xianhua (2007): High-resolution sea surface temperature records derived from foraminiferal Mg/Ca ratios during the last 260 ka in the northern South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 250(1-4), 126-138

Gangjian Wei, Wenfeng Deng, Ying Liu & Xianhua Li
High-resolution sea surface temperatures (SST) derived from Mg/Ca ratios of Globeriginoides sacculifer at ODP Site 1144 were reported to reveal the SST changes during the last 260 ka in the northern South China Sea (SCS). The results indicate an average Holocene SST of about 26.7 °C, about 3.6 °C increase from LGM to the Holocene, and higher temperature during MIS 5.5 than the Holocene. These agree well with other foraminifer Mg/Ca and Uk 37 SST...
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