Carbon, sulfur, and oxygen isotope evidence for a strong depth gradient and oceanic oxidation after the Ediacaran Hankalchough glaciation

	Carbon, sulfur, and oxygen isotope evidence for a strong depth gradient and oceanic oxidation after the Ediacaran Hankalchough glaciation
	Shen, Bing ; Xiao, Shuhai (肖书海) ; Bao, Huiming (鲍惠铭) ; Kaufman, Alan J. ; Zhou, Chuanming (周传明) ; Yuan, Xunlai (袁训来)
刊名	GEOCHIMICA ET COSMOCHIMICA ACTA
	2011
卷号	75 期号:5 页码:1357-1373
ISSN号	0016-7037
公开日期	2012-08-15
内容类型	期刊论文
源URL	[http://ir.nigpas.ac.cn/handle/332004/467]
专题	中国科学院南京地质古生物研究所南京地质古生物研究所_其他
推荐引用方式 GB/T 7714	Shen, Bing,Xiao, Shuhai ,Bao, Huiming ,et al. Carbon, sulfur, and oxygen isotope evidence for a strong depth gradient and oceanic oxidation after the Ediacaran Hankalchough glaciation[J]. GEOCHIMICA ET COSMOCHIMICA ACTA,2011,75(5):1357-1373.
APA	Shen, Bing,Xiao, Shuhai ,Bao, Huiming ,Kaufman, Alan J.,Zhou, Chuanming ,&Yuan, Xunlai .(2011).Carbon, sulfur, and oxygen isotope evidence for a strong depth gradient and oceanic oxidation after the Ediacaran Hankalchough glaciation.GEOCHIMICA ET COSMOCHIMICA ACTA,75(5),1357-1373.
MLA	Shen, Bing,et al."Carbon, sulfur, and oxygen isotope evidence for a strong depth gradient and oceanic oxidation after the Ediacaran Hankalchough glaciation".GEOCHIMICA ET COSMOCHIMICA ACTA 75.5(2011):1357-1373.