The Ocean Redox State Evolution and Its Controls during the Cambrian Series 1-2: Evidence from Lijiatuo Section, South China

doi:10.1007/s12583-016-0695-3

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 中国科学院油气资源研究重点实验室

	The Ocean Redox State Evolution and Its Controls during the Cambrian Series 1-2: Evidence from Lijiatuo Section, South China
	Xiang, Lei 1,2; Cai, Chunfang 2; He, Xunyun 3; Jiang, Lei 2; Yuan, Yuyang 2; Wang, Tiankai 2; Jia, Lianqi 2; Yu, Lei 4
刊名	JOURNAL OF EARTH SCIENCE
	2016-04-01
卷号	27 期号:2 页码:255-270
关键词	trace element redox state seawater sulfate level Cambrian Series 1-2 South China
DOI	10.1007/s12583-016-0695-3
文献子类	Article
英文摘要	Well-exposed Lijiatuo Section was chosen to explore the temporal evolution and controls of the oceanic redox state, primary productivity and seawater sulfate levels during the Cambrian Series 1-2, South China. This section consists of Xiaoyanxi Formation (Fm.) mudstones and Liuchapo Fm. cherts that deposited in the slope and basin environment. Five oxic-anoxic cycles were identified based on V/Sc, Th/U and the enrichment factors of Mo, U, V, Ni and Cu. The Middle-Upper Liuchapo Fm. and the Middle Xiaoyanxi Fm. were deposited under oxic-suboxic conditions, and the rest of the strata were under anoxic conditions. The Re/Mo ratio demonstrated that the oxic-suboxic conditions in the Middle Xiaoyanxi Fm. were accompanied by transient sulfidic conditions, and the rest of the section was underanoxic and non-sulfidic conditions. All the TOC and the enrichment factors of Ba, Ni, Cu, Zn and Cd demonstrated that both the sinking and burial flux of organic matter (OM) in Liuchapo Fm. were lower than that in the overlying Xiaoyanxi Fm. The highest sinking and burial flux of OM in the Xiaoyanxi Fm. appeared at its lower parts; however, the lowest sinking and burial flux of OM in the Xiaoyanxi Fm. appeared in its middle parts. TOC/TS, TS and the vertical trend of 834Spy demonstrated that the seawater was dominated by low oceanic sulfate levels, which resulted in the absence of free H2S. The rise of the atmospheric oxygen content may be the principal driver for the associated, transient suboxic-oxic and nearly sulfidic environment in the middle Xiaoyanxi Fm.
WOS关键词	ORGANIC-CARBON ISOTOPE ; PERMIAN MASS EXTINCTION ; FERRUGINOUS DEEP-WATER ; YANGTZE PLATFORM ; TERMINAL EDIACARAN ; LAOBAO FORMATION ; XIAOTAN SECTION ; PRECAMBRIAN/CAMBRIAN BOUNDARY ; ATMOSPHERIC OXYGEN ; GUIZHOU PROVINCE
WOS研究方向	Geology
语种	英语
WOS记录号	WOS:000373423300011
资助机构	China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Funds for Distinguished Young Scientists(41125009) ; China National Funds for Distinguished Young Scientists(41125009) ; China National Funds for Distinguished Young Scientists(41125009) ; China National Funds for Distinguished Young Scientists(41125009) ; NSFC(41290260 ; NSFC(41290260 ; NSFC(41290260 ; NSFC(41290260 ; 41502023) ; 41502023) ; 41502023) ; 41502023) ; China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Program on Key Basic Research Project (973 Program)(2011CB808800) ; China National Funds for Distinguished Young Scientists(41125009) ; China National Funds for Distinguished Young Scientists(41125009) ; China National Funds for Distinguished Young Scientists(41125009) ; China National Funds for Distinguished Young Scientists(41125009) ; NSFC(41290260 ; NSFC(41290260 ; NSFC(41290260 ; NSFC(41290260 ; 41502023) ; 41502023) ; 41502023) ; 41502023)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/53459]
专题	地质与地球物理研究所_中国科学院油气资源研究重点实验室
作者单位	1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.PetroChina, Hangzhou Res Inst Geol, Hangzhou 310023, Zhejiang, Peoples R China 4.PetroChina, PetroChina Changqing Oilfield Co, Explorat & Dev Res Inst, Xian 710018, Peoples R China
推荐引用方式 GB/T 7714	Xiang, Lei,Cai, Chunfang,He, Xunyun,et al. The Ocean Redox State Evolution and Its Controls during the Cambrian Series 1-2: Evidence from Lijiatuo Section, South China[J]. JOURNAL OF EARTH SCIENCE,2016,27(2):255-270.
APA	Xiang, Lei.,Cai, Chunfang.,He, Xunyun.,Jiang, Lei.,Yuan, Yuyang.,...&Yu, Lei.(2016).The Ocean Redox State Evolution and Its Controls during the Cambrian Series 1-2: Evidence from Lijiatuo Section, South China.JOURNAL OF EARTH SCIENCE,27(2),255-270.
MLA	Xiang, Lei,et al."The Ocean Redox State Evolution and Its Controls during the Cambrian Series 1-2: Evidence from Lijiatuo Section, South China".JOURNAL OF EARTH SCIENCE 27.2(2016):255-270.