Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea: A possible paleoclimate indicator

GIG OpenIR

	Wei Gang-Jian; Zou Liang; Deng Wen-Feng; Li Xian-Hua; Liu Ying; Chen Jian-Fang
	Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea: A possible paleoclimate indicator
Source Publication	Geochemical Journal
ISSN	0016-7002
	2009
Volume	43 Issue:4 Pages:235-246
Language	英语
WOS ID	WOS:000269509900003
Indexed By	sci
Citation statistics	Cited Times:3[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/14307
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	Wei Gang-Jian,Zou Liang,Deng Wen-Feng,et al. Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea: A possible paleoclimate indicator[J]. Geochemical Journal,2009,43(4):235-246.
APA	Wei Gang-Jian,Zou Liang,Deng Wen-Feng,Li Xian-Hua,Liu Ying,&Chen Jian-Fang.(2009).Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea: A possible paleoclimate indicator.Geochemical Journal,43(4),235-246.
MLA	Wei Gang-Jian,et al."Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea: A possible paleoclimate indicator".Geochemical Journal 43.4(2009):235-246.

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