Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio

	Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio
	Wang XiaoYan (王晓燕); Li BaoHua (李保华)
	2012
发表期刊	SCIENCE CHINA-EARTH SCIENCES
ISSN	1674-7313
卷号	55 期号:11 页码:1827-1836
文献类型	期刊论文
条目标识符	http://ir.nigpas.ac.cn/handle/332004/4528
专题	中国科学院南京地质古生物研究所其他
推荐引用方式 GB/T 7714	Wang XiaoYan ,Li BaoHua . Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio[J]. SCIENCE CHINA-EARTH SCIENCES,2012,55(11):1827-1836.
APA	Wang XiaoYan ,&Li BaoHua .(2012).Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio.SCIENCE CHINA-EARTH SCIENCES,55(11),1827-1836.
MLA	Wang XiaoYan ,et al."Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio".SCIENCE CHINA-EARTH SCIENCES 55.11(2012):1827-1836.