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The sulfur isotope signatures of Marinoan deglaciation captured in Neoproterozoic shallow-to-deep cap carbonate from South China

文献类型：期刊论文

作者Huang, Jing1; Chu, Xuelei2,3; Lyons, Timothy W.4; Sun, Tao5; Feng, Lianjun2; Zhang, Qirui2; Chang, Huajin6
刊名PRECAMBRIAN RESEARCH
出版日期2013-11-01
卷号238页码:42-51
关键词Neoproterozoic South China Doushantuo Formation Cap carbonate Sulfur isotope
ISSN号0301-9268
DOI10.1016/j.precamres.2013.09.002
文献子类Article
英文摘要We present high-resolution sulfur and carbon isotope records from the cap carbonate of the Doushantuo Formation, South China, a unique suite of depositional facies spanning across a pronounced paleooceanic depth gradient. The delta S-34 of carbonate-associated sulfate (CAS) decreases across a shelf-to-slope depth transect. We propose that the deeper-water slope profile represents syn-glacial sulfur isotope compositions of the seawater sulfates with impact of S-34-depleted hydrothermal sulfur inputs, while the delta S-34 of the shallow inner-shelf were dominantly controlled by the S-34-enriched terrigenous input. We suggest that the terrigenous sulfur inputs were mainly from weathering and erosion of the pre-Marinoan Datangpo Formation glacially ground and then freshly exposed during rapid deglaciation. The widespread Datangpo Formation, deposited between the Sturtian and Marinoan glacial intervals, is noted for the unusually high delta S-34 values of its pyrite.
WOS关键词EDIACARAN DOUSHANTUO FORMATION ; PB ZIRCON AGE ; SNOWBALL EARTH ; METHANE SEEPS ; HYDRATE DESTABILIZATION ; HYDROTHERMAL ORIGIN ; YANGTZE PLATFORM ; DEATH-VALLEY ; ICE AGES ; GLACIATION
WOS研究方向Geology
语种英语
WOS记录号WOS:000330818800003
出版者ELSEVIER SCIENCE BV
资助机构Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; 41003034 ; 41003034 ; 41003034 ; 41003034 ; 41025011) ; 41025011) ; 41025011) ; 41025011) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; 41003034 ; 41003034 ; 41003034 ; 41003034 ; 41025011) ; 41025011) ; 41025011) ; 41025011) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; 41003034 ; 41003034 ; 41003034 ; 41003034 ; 41025011) ; 41025011) ; 41025011) ; 41025011) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Ministry of Science and Technology of China(2011CB808805) ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; Natural Science Foundation of China(41172029 ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; State Key Laboratory of Continental Dynamics, Northwest University in China ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; NASA Astrobiology Institute ; 41003034 ; 41003034 ; 41003034 ; 41003034 ; 41025011) ; 41025011) ; 41025011) ; 41025011)
源URL[http://ir.iggcas.ac.cn/handle/132A11/87956]  
专题中国科学院地质与地球物理研究所
通讯作者Chu, Xuelei
作者单位1.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.NW Univ Xian, State Key Lab Continental Dynam, Xian 710069, Peoples R China
4.Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA
5.NASA, Johnson Space Ctr, Houston, TX 77058 USA
6.Qinghai Normal Univ, Sch Life & Geog Sci, Xining 810008, Peoples R China
推荐引用方式
GB/T 7714		 Huang, Jing,Chu, Xuelei,Lyons, Timothy W.,et al. The sulfur isotope signatures of Marinoan deglaciation captured in Neoproterozoic shallow-to-deep cap carbonate from South China[J]. PRECAMBRIAN RESEARCH,2013,238:42-51.
APA Huang, Jing.,Chu, Xuelei.,Lyons, Timothy W..,Sun, Tao.,Feng, Lianjun.,...&Chang, Huajin.(2013).The sulfur isotope signatures of Marinoan deglaciation captured in Neoproterozoic shallow-to-deep cap carbonate from South China.PRECAMBRIAN RESEARCH,238,42-51.
MLA Huang, Jing,et al."The sulfur isotope signatures of Marinoan deglaciation captured in Neoproterozoic shallow-to-deep cap carbonate from South China".PRECAMBRIAN RESEARCH 238(2013):42-51.

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来源：地质与地球物理研究所

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