[1] Li Yuanlü, Wang Xuzeng, Wu Chuanrong, et al. Integrated Survey Report about Stone Coal Resources of Southern China[M].Xi′an:China Coal Researh Institute, 1982.[李远虑, 王煦曾, 吴传荣, 等. 中国南方石煤资源综合考察报告[M].西安:煤炭科学院地质勘探分院地质研究所,1982.] [2] Coal Industry Admins Bureau of Zhejiang Province. Comprehensive Utilization of Coal[M]. Beijing: China Coal Industry Publish House, 1980.[浙江省煤炭工业局. 石煤的综合利用[M]. 北京: 煤炭工业出版社, 1980.] [3] Fan Delian, Yang Xiuling. Study of sedimentary petrology on the black shale and the polymetallic layers in the Lower Cambrian[C]//Sedimentary Petrology. Beijing: Science Press,1981.[范德廉, 杨秀玲.南方几省下寒武统黑色岩系及层状多金属富集层[C]//沉积岩石学研究(论文集). 北京: 科学出版社,1981.] [4] Arthur M A. Stratigraphy, geochemistry and paleogeography of organic carbon rich Cretaceoussequences[C]//Ginsburg, Bernard, eds. Cretaceous Resources Events and Rhythms. Kluwer: Kluwer Academic Publishers,1979. [5] Leggett J K. British Lower Paleozoic black shales and their paleooceanographic significance[J].Journal of the Geological Society,1980, 137(2): 139-156. [6] Jenkyns H C. Cretaceous anoxice vents: From continents to oceans[J].Journal of the Geological Society,1980, 137(2): 171-188. [7] Jiang Yuehua, Yue Wenzhe, Ye Zhizheng. Characteristics, sedimentary environment and originof the lowekr cambrian stone -like coal in southern china[J].Coal Geology of China,1994, 6(4): 26-31.[姜月华, 岳文浙, 业治铮. 中国南方下寒武统石煤的特征、沉积环境和成因[J]. 中国煤田地质, 1994, 6(4): 26-31.] [8] Cornelius F,Reinhard G. Change of black shale organic material surface area during oxidative weathering:Implications for rock-water surface evolution[J].Geochimica et Cosmochimica Acta,2005, 69(5): 1 213-1 224. [9] Martin J K, David R P, Ronald J H, Mineral surface control of organic carbon in black shale[J].Science,2002, 295(5 555):657-660. [10] Huinby-Hunt M S, Wide P. Chemical depositional environments of calcic marine black shales[J].Economic Geology,1996, 91(1):4-13. [11] Calvert S E, Fan Delian, Ye Jie, et al. Sedimentary geochemistry of manganese: Implications for the environment of formation of black shales[J].Economic Geology,1996,91(1):36-47. [12] Liu Tiebing, Fan Delian, Ye Jie,et al. Origin of the black shale-hosted Chadian phosphorus-manganese deposit[J].Economic Geology,1996, 91(1):48-54. [13] Steiner M, Zhu M, Zhao Y L, et al. Lower Cambrian Burgess Shale-type fossil associations of South China[J].Palaeogeography, Palaeoclimatology, Palaeoecology,2005, 220(1/2):129-152. [14] Zhu Liying. Petrography of early Paleozoic highly metamorphosed boghead coal and its geological significance[J].Geological Review,1983, 29(3):245-261.[朱丽英.早古生代高变质藻煤的煤岩特征及其地质意义[J]. 地质论评,1983, 29(3):245-261.] [15] Zhou Haoda. On the mechanism and the characteristics of early cambrian “stone coal” in lower Yangtze region and their relation to petroliferous potentials[J].Petroleum Geology & Expeximent,1990, 12(1): 36-43.[周浩达.下杨子区早寒武世“石煤”沉积特征与成因机理探讨——兼论与含油气性关系[J].石油实验地质, 1990, 12(1):36-43.] [16] Oschmann W. Microbes and balck shales[C]//Riding R E, Awramik S M, eds. Microbial Sediments.Berlin: Springer Verlag,2000,137-148. [17] Mao J, Lehmann B, Du A, et al. Re-Os dating of polymetallic Ni-Mo-PGE-Au mineralization in Lower Cambrian black shale of South China and its geological significance[J].Economic Geology,2000,97(5):1 051-1 061. [18] Coveney R M Jr, Watney W L, Maples C R. Contrasting depositional models for Pennsylvanian black shale discerned from molybdenum abundances[J].Geology,1991,19(2):147-150. [19] Algeo T J, Lyons T W. Mo-total organic carbon covariation in modern anoxic marine environments: Implication for analysis of paleoredox and paleohydrographic conditions[J].Paleooceanography,2006, 21,A1016, doi:10.1029/2009PA001112. [20] Steiner M, Willis E, Erdtmann B D, et al. Submarine-hydrothermal exhalative ore layers in black shale from South China and associate fossils-insights into a Lower Cambrian facies and bio-evolution[J].PALAEO,2001,169(3/4):165-191. [21] Li Shengrong, Gao Zhenmin. Source tracing of noble metal elements in Lower Cambrian black rock series of Guizhou-Hunan Provinces, China[J].Science in China (Series D), 2000, 30(2):169-174.[李胜荣, 高振敏.湘黔寒武系底部黑色岩系贵金属元素来源示踪[J]. 中国科学:D辑, 2000, 30(2):169-174.] [22] Li Youyu. Geochemistry characteristics of Ni Mo Pt group elements in the Lower Cambrian bone coal in Hunan province[J].Journal of China Coal Society,1996, 21(3): 261-264.[李有禹.湖南下寒武统石煤中的镍钼铂族元素的地球化学特征[J]. 煤炭学报, 1996, 21(3): 261-264.] [23] Jiang S Y, Chen Y Q, Ling H F, et al. Trance- and rare-earth element geochemistry and Pb-Pb dating of black shale and intercalated Ni-Mo-PGE-Au sulfide ores in Lower Cambrian strata, Yangtze Platform, South China[J].Mineralium Deposita,2006,41(5):453-467. [24] Murowchick J B, Coveney R M Jr, Grauch R I, et al. Cyclic variation of sulfur isotopes in Cambrian stratabound Ni-Mo-(PGE-Au) ores of southern China[J]. Geochimica et Cosmochimica Acta,1994, 58(7):1 813-1 823. [25] Goldberg T, Strauss Ha, Guo Q, et al. Reconstructing marine redox conditions for the early Cambrian Yangtze Platform: Evidence from biogenic sulphur and organic carbon isotopes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007, 254(1/2):175-193. [26] Orberger B, Vymazalova A, Wagner C, et al. Biogenic origin of intergrown Mo-sulphide- and carbonaceous matter in Lower Cambrian black shales (Zunyi Formation, southern China)[J].Chemical Geology,2007, 238(3/4):213-231. [27] Ahschuier Z S, Sehnepfe M M, Silber C C, et al.Sulfur diagenesis in neverglades peat and origin of pyrite in coa1[J].Science,1983, 221(2): 221-227. [28] Casagrande D J, Siefert I. Origins of sulfur in coal: Importance of the ester-sulphate content[J].Sciences,1977, 195(4 279): 675-676. [29] Berner R A. Sedimentary pyrite formation: An update[J].Geochimica et Cosmochimica Acta,1984, 48(4): 605-615. [30] Westgate L M, Anderson T F. Isotopic evidence for the origin of sulfur in the Herrin No. 6 Coal Member of Illinois[J].International Journal of Coal Geology,1984, 4(1): 1-20. [31] Trudinger P A, Swaine D J. Biogeochemical Cycling of Mineral-forming Elements[M].Amsterdam,New York: Elsevier Scientific Pub.Co.,1979:293-401. [32] Pasava J, Hladikova J, Dobes P. Origin of Proterozoic metal-rich black shales from the ohemian massif Czech Republic[J].Economic Geology,1996, 91(1): 63-79. [33] Dai Shifeng, Ren Deyi, Zhou Qiang,et al. Study of TOF-SIMS on the pyritized rod like bacteria in the high sulfur coal[J].Journal of China Coal Society,2000, 25(2): 190-195.[代世峰, 任德贻, 周强,等.高硫煤中菌落成因黄铁矿的TOF-SIMS研究[J]. 煤炭学报, 2000, 25(2): 190-195.] [34] Ye Lianjun,Li Juying, Chen Qiying, et al. Microbial-organic Minerallization and the Background[M]. Beijing: Ocean Press, 1998:225-253.[叶连俊,李菊英,陈其英,等.生物有机质成矿作用和成矿背景[M]. 北京: 海洋出版社, 1998:225-253.] [35] Yan Baorui, Zhang Xigen. Microbial Metallogeny[M]. Beijing: Science Press, 2000.[阎葆瑞, 张锡根. 微生物成矿学[M].北京:科学出版社, 2000.] [36] Dai Yongding, Song Haiming, Shen Jiying. Fossil bacteria in Xuanlong iron ore deposits of Hebei province[J]. Science in China (Series D), 2003, 33(8): 75l-759.[戴永定, 宋海明, 沈继英.河北宣龙铁矿化石细菌[J]. 中国科学:D辑, 2003, 33(8): 75l-759.] [37] Ren Deyi, Zhao Fenghua, Dai Shifeng,et al. Trace Element Geochemistry of Coal[M]. Beijing: Science Press, 2006.[任德贻, 赵峰华, 代世峰,等. 煤的微量元素地球化学[M].北京: 科学出版社, 2006.] [38] Swaine D J, Goodarzi F. Environmental Aspects of Trace Elements in coal[M]. Kluwer: Academic Publishers, 1995. [39] Finkelman R B. Trace and minor elements in coal[C]//Michael H,ed. Organic Geochemistry. New York: Plenum Press, 1993:593-607. [40] Deyi Ren, Fenghua Zhao, Yunquan Wang, et al. Distribution of minor and trace elements in Chinese coals[J].International Journal of Coal Geology,1999, 40(3/4): 109-118.[ [41] Tang Xiuyi, Huang Wenhui. Trace Element of China Coal\[M\]. Beijing: Commercial Press, 2004.[唐修义, 黄文辉. 中国煤中微量元素\[M\]. 北京: 商务印书馆, 2004.] [42] Wu Chaodong,Yang Chengyun. The origin and geochemical characteristics of upper sinain_lower cambrian black shales in Western Hunan[J].Acta Petrrologica et Mineralogica,1999, 18(1): 26-39.[吴朝东, 杨承运. 湘西黑色岩系地球化学特征和成因意义[J]. 岩石矿物学杂志, 1999, 18(1): 26-39.] [43] Zhang Ruguo.Study on Sulphur accumulation and cycling in mangrove forest in Pear River mouth[J].Soil and Environmental Sciences,1996, 5(2): 67-73.[张汝国. 珠江口红树林硫的累积和循环研究[J]. 热带亚热带土壤科学, 1996, 5(2): 67-73.] [44] White D, Theissen R. The Origin of Coal[M]. US Bureau of Mines Bulletin, 1914:38. [45] Williams E G, Keith M L. Relationship between sulfur in coals and the occurrence of marine roof[J].Economic Geology,1963, 58(5): 720-729. [46] Hunt J W, Hobday D K. Petrographic composition and sulfur content of coals associated with alluvial fans in the Permian Sydney and Gunnedah Basins, eastern Australia[J].International Association of Sedimentologists,1984, 7: 43-60. [47] Rimmer S M, Davis A. Geologic controls on the inorganic composition of Lower Kittanning Coal[C]//Vorres K S,ed. Mineral Matter and Ash in Coal, 301.American Chemical Society Symposium Series,1986: 41-52. [48] Goodarzi F. Concentration of elements in lacustrine coals from zone A, Hat Creek Deposits No.1, British Columbia, Canada[J].International Journal of Coal Geology,1987, 8(3): 247-268. [49] Cohen A D, Spackman W S, Dolsen P. Occurrence and distribution of sulfur in peat-forming environments of southern Florida[J].International Journal of Coal Geology,1984, 4(1): 73-96. [50] Tang Dazhen, Yang Qi, Zhou Chunguang, et al. Genetic relationships between swamp microenvironment and sulfur distribution of the Late Paleozoic coals in North China[J].Science in China (Series D),2000,30(6): 584-591.[汤达祯, 杨起, 周春光,等. 华北晚古生代成煤沼泽微环境与煤中硫成因关系研究[J]. 中国科学:D辑, 2000, 30(6): 584-591.] [51] Spears D A, Caswell S A. Mineral matter in coals: cleat minerals and their origin in some coals from the English Midlands[J].International Journal of Coal Geology,1986, 6(2):107-125. [52] Demchuk T D. Epigenetic pyrite in a low-sulfur, sub-bituminous coal from the central Alberta Plains[J].International Journal of Coal Geology,1992, 21(3): 187-196. [53] Amend J P, Edwards K J, Lyons T W, eds. Special Paper-Geological Society of America, 379. Sulfur Biogeochemistry Past and Present[M]. Washington DC: American Chemical Society,2004. [54] Liao Jialong,Yao Suping, Ding Hai. The characteristics and controlling factor of sulfur in the sediments of coastal mangrove peat[J].Geological Journal of China Universities,2008, 14(4): 620-630.[廖家隆, 姚素平, 丁海.滨海红树林泥炭沉积物中硫的赋存特点及其控制因素[J]. 高校地质学报, 2008,14(4): 620-630.] [55] Chou C L. Geochemistry of sulfur in coal[C]//Orr W L, White C M, eds. Geochemistry of Sulfur in Fossil Fuels. American Chemical Society Symposium Series, 429. Washington DC, 1990:30-52. [56] Ren Deyi, Lei Jiajin, Tang Yuegang. The microarea analysis and distribution characteristics of the organic sulfur in macerals[J].Coal Geology & Exploration,1993, 21(1): 27-29.[任德贻, 雷加锦, 唐跃刚.煤中显微组分有机硫的微区分析和分布特征[J]. 煤田地质与勘探, 1993, 21(1): 27-29.] [57] Lei Jiajin, Ren Deyi, Tang Yuegang. Sulfur-accumulating model of superhigh organosulfur coal from Guiding, China[J].Chinese Science Bulletin,1994, 39(15): 1 405-1 408.[雷加锦, 任德贻, 唐跃刚. 贵州超高有机硫煤硫的的聚集模式[J]. 科学通报, 1994, 39(15): 1 405-1 408.] [58] Lin S, Morse J W. Sulfate reduction and iron sulfide mineral formation in Gulf of Mexico anoxic sediments[J].American Journal of Science,1991, 291(1): 55-89. [59] Borowski W S, Paui C K, Ussler W. Marine porewater sulfate profiles indicate in situ methane flux from underlying gas hydrate[J].Geology,1996, 24(7): 655-658. [60] Westrich J T, Berner R A. The role of sedimentary organic matter in bacterial sulfate reduction: The G-Model tested[J].Limnology Oceanography,1984, 29(2):236-249. [61] Dellwig O, Watermann F, Brumsack H J, et al. Sulphur and iron geochemistry of Holocene coastal peats (NW Germany): A tool for palaeoenvironmental reconstruction[J].Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 167(3): 359-379. [62] Pelsh A D.About New Autotrophic Hydrogenthiobacteria[M].Trudy Solyanoi Laboratorii, vypusk,1936, 5: 109-126. [63] Holmer M, Kristensen E, Banta G, et al. Biogeochemical cycling of sulfur and iron in sediments of a south-east Asian mangrove, Phuket Island, Thailand[J]. Oceanographic Literature Review,1995, 42(5): 346. [64] Wang Zhenle. The mineral composition of stone coal in Western Zhejiang[J].Coal Geology & Exploration,1980,(3): 30-33.[王真乐. 浙西石煤的矿物组成[J]. 煤田地质与勘探, 1980,(3): 30-33.] [65] Miller L P. Formation of metal sulphides through the activities of sulphate-reducing bacteria[J].Contributions from Boyce Thompson Institute,1950, 16:85-89. [66] Baas Becking L G M, Moore D. Biogenic sulfides[J].Economic Geology,1961, 56(2):259-272. [67] Labrens M,Druschel G K, Thomsen-Ebert T. Formation of sphalerite (ZnS) deposits in natural biofilms of sulfate-reducing bacteria[J].Science,2000,290(5 497):1 744-1 747. [68] Kramarenko L E. Bacterial biocenoses in underground waters of some mineral fields and their geological importance[J].Mikrobiologiya,1962, 31: 564-569. [69] Sakaguchi T, Burgess J G, Matsunaga T. Magnetite formation by a sulphate-reducing bacterium[J].Nature,1993, 365(6 441): 47-49. [70] Tebo B M, Obraztsova A Y. Sulfate-reducing bacterium grows with Cr(Ⅵ), V(Ⅵ), Mn(Ⅳ)and Fe(Ⅲ)as electron acceptors[J].FEMS Microbiology Letters,1998, 162(1): l93-198. [71] Watson J H P, Ellwood D C, Deng Q X, et al. Heavy metal adsorption on bacterially produced FeS[J].Minerals Engineering,1995,8(10):1 097-1 108. [72] Watson J H P, Cressey B A, Roberts A P, et al. Structural and magnetic studies on heavy-metal-absorbing iron sulfide nanoparticles produced by sulfate-reducing bacteria[J].Journal of Magnestism and Magnetic Materials,2000, 214(1/2):13-20. [73] Goldhaber M B, Kaplan I R. The sulfur cycle[C]//Goldberg E D, ed. The Sea (vol. 5).New York:Wiley,1974:569-655. [74] Rickard D T, Luther G W. Kinetics of pyrite formation by the H2S oxidation of iron (Ⅱ) monosulfide in aqueous solutions between 25 and 125℃: The mechanism[J].Geochimica et Cosmochimica Acta,1997, 61(1): 135-147. [75] Tang Yuegang, Ren Deyi. The genesis of pyrites in coal[J].Geological Review,1996, 42(1): 64-70.[唐跃刚, 任德贻. 煤中黄铁矿的成因研究[J]. 地质论评, 1996, 42(1): 64-70.] [76] Raiswell R. Kinetic controls on depth variations in localized pyrite formation[J].Chemical Geology,1993, 107(1 993):467-469. [77] Raiswell R, Plant J. The incorporation of trace elements into pyrite during diagenesis of Black Shales, Yorkshire, England[J].Economic Geology,1980, 75(5):684-699. [78] Wang Q, Morse J W. Pyrite formation under conditions approximating those in anoxic sediments I. Pathway and morphology[J].Marine Chemistry,1996, 52(2):99-121. [79] Schoonen M A A, Barnes H L. Reactions forming pyrite and marcasite from solution:Ⅰ.Nucleation of FeS2 below 100℃[J].Geochimica et Cosmochimica Acta,1991,55(6):1 495-1 504. [80] Schoonen M A A, Barnes H L. Reactions forming pyrite and marcasite from solution:Ⅱ.Via FeS precursors below 100℃[J].Geochimica et Cosmochimica Acta,1991,55(6): 1 505-1 514. [81] Schoonen M A A, Barnes H L. Reactions forming pyrite and marcasite from solution: Ⅲ. Hydrothermal processes[J].Geochimica et Cosmochimica Acta,1991, 55(12): 3 491-3 504. [82] Donald R, Southam G. Low temperature anaerobic bacterial diagenesis of ferrous monosulfide to pyrite[J]. Geochimica et Cosmochimica Acta,1999, 63(13/14): 2 019-2 023. [83] Wilkin R T, Barnes H L. Pyrite formation by reactions of iron monosulfides with dissolved inorganic and organic sulfur species[J]. Geochimica et Cosmochimica Acta,1996, 60(21): 4 167-4 179. [84] Canfield D E, Thamdrup B, Fleischer S. Isotope fractionation and sulfur metabolism by pure and enrichment cultures of elemental sulfur-disproportionating bacteria[J]. Limnology and Oceanography,1998, 43(2): 253-264. [85] Rickard D T. Kinetics and mechanism of pyrite formation at low temperatures[J].American Journal of Science,1975, 275(6): 636-652. [86] Hurtgen M T, Lyons T W, Ingall E D. Anomalous enrichments of iron monosulfides transformations: Examples from Effingham Inlet, Orca Basin, and the Black Sea[J].American Journal of Science,1999, 299(7): 100-101. [87] Neal A L, Techkamjanaruk S, Dohnalkova A, et al. Iron sulfide and sulfur species produced at hematite surfaces in the presence of sulfate-reducing bacteria[J].Geochimica et Cosmochiamica Acta,2001, 65(2): 223-235. |