Lei Jiajin;Li Renwei;Tobschall H J,The characteristics of the sulfur species and their implications in lower Cambrian black shales from southern margin of Yangtze Platform,中国科学D辑,2000(06).
Brasier M D;Magaritz M;Corfeld R,The carbon-and oxygen-isotopic record of the Precambrian-Cambrian boundary interval in China and Iran and their correlation,Geological Magazine,1990.
Yang Xianhe;He Yuanxiang;Deng Shouhe,Precambrian-Cambrian boundary and small shelly fossils fauna from Nanjiang, Sichuan province, China. Chengdu Institute of Geological Mineral Deposits Publication,CAGS,1983(04).
[10]
Wu Chaodong,Recovery of the Paleoocean environment in the alterating epoch of late Sinian and early Cambrian in the west Hunan,地学前缘,2000(07).
[11]
Shen Y;Schidlowski M;Chu X,Biogeochemical approach to understanding phosphogenic events of the terminal Proterozoic to Cambrian,Palaeogeography Palaeoclimatology Palaeoecology,2000.
[12]
McCrea J M,On the isotopic chemistry of carbonates and a paleo-temperture scale,Journal of Chemical Physics,1950.
[13]
Marshall J D,Climatic and oceanographic isotopic signals from the carbonate rock record and their preservation,Geological Magazine？ ,1992, 129.
[14]
Mao J W;Lehmann B;Du A D Re-Os dating of polymetallic Ni-Mo-PGE-Au mineralization in Lower Cambrian black shales of South China and its geologic significance [J] 2002
[15]
Lambert I B;Walter M R;Zhang W,Paleoenvironment and carbon isotope stratigraphy of Upper Proterozoic carbonates of the Yangtze platfrom,NATURE,1987.
[16]
GoldbergT;Strauss H;Guo Q.The late Neoproterozoic to early Cambrian sulphur cycle:an isotopic investigation of sedimentary rocks from the Yangtze platform[J].自然科学进展(英文版),2003(12)doi:10.1080/10020070312331344700
[17]
GoldbergT;Strauss H,The late Neoproterozoic to early Cambrian sulfur cycle: an isotopic investigation of sedimentary rocks from Yangtze platform,Geophysical Research Abstracts,2003.
[18]
Wang Darui;Bai Yulei;Jia Chengzao,Carbon isotope anomaly and significance at the Boundary between Precambrian and Cambrian on Keping section,Xinjiang,Northwest China,科学通报(英文版),1994(15).
[19]
Veizer J;Ala D;Azmy K,87Sr/86Sr,δ13C and δ18O evolution of Phanerozoic seawater,Chemical Geology,1999.
[20]
Veizer J,Chemical diagenesis of carbonates: theory and application,S E P M Short Course,1983(10).
[21]
雷家锦;李任伟;Tobschall H J.扬子地台南缘早寒武世黑色岩系中形态硫特征及成因意义[J].中国科学D辑,2000(06)
[22]
Fan Delian;Yang Ruiying;Huang Zhongxiang,The Lower Cambrian black shale series and iridium anomaly in South China,Developments in Geosciences,Contribution to 27th IGC.,Beijing:Moscow,Sciences Press,1984.
[23]
郑淑蕙;郑斯成;莫志超,稳定同位素地球化学分析,北京:北京大学出版社,1986.
[24]
钱逸,中国小壳化石分类学与生物地层学,北京:科学出版社,1999.
[25]
Zhen Shuhui;Zhen Sicheng;Mo Zhichao,Geochemistry analysis of stable isotopes,北京:北京大学出版社,1986.
[26]
Yang Xianhe;He Tinggui,New small shelly fossils genera of the Lower Cambrian from Nanjiang, Sichuan province, China,Strata and Palaeotology Papers Assemblage,1984(13).
Steiner M;Wallis E;Erdtmann B D,Submarine-hydrothermal exhalative ore layers in black shales from South China and associated fossils-insights into a Lower Cambrian facies and bio-evolution. Paleogeogr. Paleoclimatal,Paleoecology,2001.
[29]
Yanan Shen ；Manfred Schidlowski,New C isotope stratigraphy form southwest China: Implications for the placement of the Precambrian-Cambrian boundary on the Yangtze Platform and Global correlations,Geology？,2000, 28(7).
[30]
Samuelsson J;Strauss H,Stable isotope geochemistry and paleobiology of the upper Visings Group (early Neoproterozoic),southern Sweden,Geological Magazine,1999.
[31]
Qian Yi,Taxonomy and biostratigraphy of small shelly fossils in China,北京:科学出版社,1999.
[32]
Magaritz M,13C minima follow extinction events:A clue to faunal extinction,GEOLOGY？ ,1989, 17.
[33]
Li Renwei;Lu Jialan;Zhang Shukun,Organic carbon isotopes of the Sinian and Early Cambrian black shales on Yangtze platform, China,中国科学D辑(英文版),1999(06).
[34]
Li R;Chen J;Zhang,Spatial and temporal variations in carbon and sulfur isotopic compositions of Sinian sedimentary rocks in the Yangtze platform,South China Precambrian Res,1999.
[35]
陈锦石;闻传芬;钟华;刘培伦,古生代海洋碳同位素演化,地质科学,1995(04).
[36]
Kaufman A J,Neoproterozoic variations in the C-isotopic composition of seawater: stratigraphic and biogeochemical implications,Precambrian Research,1995.
[37]
HeYuanxiang;Yang Xianhe,Coelenterate fossils of the Early Cambrian from Nanjiang, Sichuan province, China,Chengdu Institute of Geological Mineral Deposits Publication CAGS,1986(07).
[38]
John M. Hayes ；Harald Strauss ；Alan J. Kaufman,The abundance of ~(13)C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 Ma,Chemical geology？,1999, 161(s1-3).
