[1] |
Gerhard L C, Harrison W E. Distribution of oceans and continents: A geological constraint on global climate variability[M]//Gerhard L C, Harrison W E, Hanson B M. Geological perspectives of global climate change. American: American Association of Petroleum Geologists, 2001: 35-49. |
[2] |
Raup D M, Sepkoski J J. Mass extinctions in the marine fossil record[J]. Science, 1982, 215(4539): 1501-1503. |
[3] |
Sepkoski J J. Stratigraphic biases in the analysis of taxonomic survivorship[J]. Paleobiology, 1975, 1(4): 343-355. |
[4] |
Bambach R K, Knoll A H, Wang S C. Origination, extinction, and mass depletions of marine diversity[J]. Paleobiology, 2004, 30(4): 522-542. |
[5] |
Barnes C R. Ordovician oceans and climate[M]//Webby B D, Paris F, Droser M L, et al. The great Ordovician biodiversification event (The critical moments and perspectives in earth history and paleobiology). Columbia: Columbia University Press, 2004: 72-76. |
[6] |
Stanley S M. Estimates of the magnitudes of major marine mass extinctions in earth history[J]. Proceedings of the National Academy of Sciences of the United States of America, 2016, 113(42): E6325-E6334. |
[7] |
Banner J L. Radiogenic isotopes: Systematics and applications to Earth surface processes and chemical stratigraphy[J]. Earth-Science Reviews, 2004, 65(3/4): 141-194. |
[8] |
Wang K, Chatterton B D E, Wang Y. An organic carbon isotope record of Late Ordovician to Early Silurian marine sedimentary rocks, Yangtze Sea, South China: Implications for CO2 changes during the Hirnantian glaciation[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1997, 132(1/2/3/4): 147-158. |
[9] |
Kump L R. Interpreting carbon-isotope excursions: Strangelove oceans[J]. Geology, 1991, 19(4): 299-302 |
[10] |
Chen X, Rong J Y, Fan J X, et al. The Global Boundary Stratotype Section and Point (GSSP) for the base of the Hirnantian stage (the uppermost of the Ordovician System)[J]. Episodes, 2006, 29(3): 183-196. |
[11] |
Melchin M J, Holmden C. Carbon isotope chemostratigraphy in Arctic Canada: Sea-level forcing of carbonate platform weathering and implications for Hirnantian global correlation[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 234(2/3/4): 186-200. |
[12] |
Yan D T, Chen D Z, Wang Q C, et al. Carbon and sulfur isotopic anomalies across the Ordovician-Silurian boundary on the Yangtze Platform, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009, 274(1/2): 32-39. |
[13] |
Fan J X, Peng P A, Melchin M J. Carbon isotopes and event stratigraphy near the Ordovician-Silurian boundary, Yichang, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009, 276(1/2/3/4): 160-169. |
[14] |
Chen C, Wang J S, Algeo T J, et al. Negative δ13Ccarb shifts in Upper Ordovician (Hirnantian) Guanyinqiao bed of South China linked to diagenetic carbon fluxes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 487: 430-446. |
[15] |
Le Heron D P, Craig J, Etienne J L. Ancient glaciations and hydrocarbon accumulations in North Africa and the Middle East[J]. Earth-Science Reviews, 2009, 93(3/4): 47-76. |
[16] |
Melchin M J, Mitchell C E, Holmden C, et al. Environmental changes in the Late Ordovician–early Silurian: Review and new insights from black shales and nitrogen isotopes[J]. GSA Bulletin, 2013, 125(11/12): 1635-1670. |
[17] |
尹福光,许效松,万方,等. 华南地区加里东期前陆盆地演化过程中的沉积响应[J]. 地球学报,2001,22(5):425-428.
Yin Fuguang, Xu Xiaosong, Wan Fang, et al. The sedimentary response to the evolutionary process of Caledonian Foreland Basin system in South China[J]. Acta Geoscientia Sinica, 2001, 22(5): 425-428. |
[18] |
万方,许效松. 川滇黔桂地区志留纪构造岩相古地理[J]. 古地理学报,2003,5(2):180-186.
Wan Fang, Xu Xiaosong. Tectonic- lithofacies palaeogeography of the Silurian in Sichuan-Yunnan-Guizhou-Guangxi region[J]. Journal of Palaeogeography, 2003, 5(2): 180-186. |
[19] |
郭英海,李壮福,李大华,等. 四川地区早志留世岩相古地理[J]. 古地理学报,2004,6(1):20-29.
Guo Yinghai, Li Zhuangfu, Li Dahua, et al. Lithofacies palaeogeography of the Early Silurian in Sichuan area[J].Journal of Palaeogeography, 2004, 6(1): 20-29. |
[20] |
戎嘉余,陈旭,王怿,等. 奥陶—志留纪之交黔中古陆的变迁:证据与启示[J]. 中国科学(D辑):地球科学,2011,41(10):1407-1415.
Rong Jiayu, Chen Xu, Wang Yi, et al. Northward expansion of Central Guizhou Oldland through the Ordovician and Silurian transition: Evidence and implications[J]. Science China (Seri. D): Earth Sciences, 2011, 41(10): 1407-1415. |
[21] |
冯增昭,彭勇民,金振奎,等. 中国南方中及晚奥陶世岩相古地理[J]. 古地理学报,2001,3(4):10-24.
Feng Zengzhao, Peng Yongmin, Jin Zhenkui, et al. Lithofacies palaeogeography of the Middle and Late Ordovician in South China[J]. Journal of Palaeogeography, 2001, 3(4): 10-24. |
[22] |
苏文博,李志明, Ettensohn F R,等. 华南五峰组—龙马溪组黑色岩系时空展布的主控因素及其启示[J]. 地球科学:中国地质大学学报,2007,32(6):819-827.
Su Wenbo, Li Zhiming, Ettensohn F R, et al. Distribution of black shale in the Wufeng–Longmaxi Formations (Ordovician–Silurian), South China: Major controlling factors and implications[J]. Earth Science: Journal of China University of Geosciences, 2007, 32(6): 819-827. |
[23] |
牟传龙,周恳恳,梁薇,等. 中上扬子地区早古生代烃源岩沉积环境与油气勘探[J]. 地质学报,2011,85(4):526-532.
Mu Chuanlong, Zhou Kenken, Liang Wei, et al. Early Paleozoic sedimentary environment of hydrocarbon source rocks in the Middle-Upper Yangtze region and petroleum and gas exploration[J]. Acta Geologica Sinica, 2011, 85(4): 526-532. |
[24] |
Chen X, Rong J Y, Li Y, et al. Facies patterns and geography of the Yangtze region, South China, through the Ordovician and Silurian transition[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 204(3/4): 353-372. |
[25] |
Tribovillard N, Algeo T J, Lyons T, et al. Trace metals as paleoredox and paleoproductivity proxies: An update[J]. Chemical Geology, 2006, 232(1/2): 12-32. |
[26] |
Nesbitt H W, Young G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature, 1982, 299(5885): 715-717. |
[27] |
McLennan S M. Weathering and global denudation[J]. The Journal of Geology, 1993, 101(2): 295-303. |
[28] |
Dymond J, Suess E, Lyle M. Barium in deep-sea sediment: A geochemical proxy for paleoproductivity[J]. Paleoceanography, 1992, 7(2): 163-181. |
[29] |
Böning P, Shaw T, Pahnke K, et al. Nickel as indicator of fresh organic matter in upwelling sediments[J]. Geochimica et Cosmochimica Acta, 2015, 162: 99-108. |
[30] |
Sepkoski J J. The Ordovician radiations: Diversification and extinction shown by global genus-level taxonomic data[M]//Cooper J D, Droser M L, Finney S C. Ordovician odyssey: Short papers for the Seventh International Symposium on the Ordovician System. Las Vegas, Nevada, USA: Pacific Section Society for Sedimentary Geology (SEPM), 1995: 393-396. |
[31] |
Sepkoski J J. A kinetic model of Phanerozoic taxonomic diversity. III. Post-Paleozoic families and mass extinctions[J]. Paleobiology, 1984, 10(2): 246-267. |
[32] |
Copper P. Frasnian/Famennian mass extinction and cold-water oceans[J]. Geology, 1986, 14(10): 835-839. |
[33] |
McGhee G R. The Frasnian–Famennian event[M]//Donovan S K. Mass extinction: Processes and evidences. California: The University of California, 1989: 266. |
[34] |
McGhee G R. The Late Devonian mass extinction: The Frasnian/Famennian crisis[M]. New York: Columbia University Press, 1996: 378. |
[35] |
Hallam A, Wignall P B. Mass extinctions and sea-level changes[J]. Earth-Science Reviews, 1999, 48(4): 217-250. |
[36] |
House M R. Strength, timing, setting and cause of mid-Palaeozoic extinctions[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 181(1/2/3): 5-25. |
[37] |
Brenchley P J, Cullen B. The environmental distribution of associations belonging to the Hirnantia fauna–evidence from North Wales and Norway[M]//Bruton D L. Aspeels of the Ordovician system. Oslo: Paleontological Contributions University Oslo, 1984: 113-125. |
[38] |
Hatch J R, Leventhal J S. Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale member of the Dennis Limestone, Wabaunsee County, Kansas, U.S.A.[J]. Chemical Geology, 1992, 99(1/2/3): 65-82. |
[39] |
Jones B, Manning D A C. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J]. Chemical Geology, 1994, 111(1/2/3/4): 111-129. |
[40] |
Klinkhammer G P, Palmer M R. Uranium in the oceans: Where it goes and why[J]. Geochimica et Cosmochimica Acta, 1991, 55(7): 1799-1806. |
[41] |
Crusius J, Calvert S, Pedersen T, et al. Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition[J]. Earth and Planetary Science Letters, 1996, 145(1/2/3/4): 65-78. |
[42] |
Calvert S E, Pedersen T F. Chapter fourteen elemental proxies for Palaeoclimatic and Palaeoceanographic variability in marine sediments: Interpretation and application[J]. Developments in Marine Geology, 2007, 1: 567-644. |
[43] |
Taylor S R, McLennan S M. The continental Crust: Its composition and evolution[M]. Oxford: Blackwell Scientific Publications, 1985: 12-13. |
[44] |
Rowe H D, Loucks R G, Ruppel S C, et al. Mississippian Barnett Formation, Fort Worth Basin, Texas: Bulk geochemical inferences and Mo-TOC constraints on the severity of hydrographic restriction[J]. Chemical Geology, 2008, 257(1/2): 16-25. |
[45] |
Marynowski L, Zatoń M, Rakociński M, et al. Deciphering the Upper Famennian Hangenberg Black Shale depositional environments based on multi-proxy record[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 346-347: 66-86. |
[46] |
Algeo T J, Tribovillard N. Environmental analysis of paleoceanographic systems based on molybdenum-uranium covariation[J]. Chemical Geology, 2009, 268(3/4): 211-225. |
[47] |
Algeo T J, Lyons T W. Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions[J]. Paleoceanography, 2006, 21(1): PA1016. |
[48] |
Ross D J K, Bustin R M. Investigating the use of sedimentary geochemical proxies for paleoenvironment interpretation of thermally mature organic-rich strata: Examples from the Devonian-Mississippian shales, western Canadian Sedimentary Basin[J]. Chemical Geology, 2009, 260(1/2): 1-19. |
[49] |
Fedo C M, Nesbitt H W, Young G M. Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance[J]. Geology, 1995, 23(10): 921-924. |
[50] |
张喜,张廷山,赵晓明,等. 天文轨道周期及火山活动对中上扬子区晚奥陶世—早志留世有机碳聚集的影响[J]. 石油勘探与开发,2021,48(4):732-744.
Zhang Xi, Zhang Tingshan, Zhao Xiaoming, et al. Effects of astronomical orbital cycle and volcanic activity on organic carbon accumulation during Late Ordovician-Early Silurian in the Upper Yangtze area, South China[J]. Petroleum Exploration and Development, 2021, 48(4): 732-744. |
[51] |
邱振,邹才能. 非常规油气沉积学:内涵与展望[J]. 沉积学报,2020,38(1):1-29.
Qiu Zhen, Zou Caineng. Unconventional petroleum sedimentology: Connotation and prospect[J]. Acta Sedimentologica Sinica, 2020, 38(1): 1-29. |
[52] |
Ripperdan R L, Magaritz M, Kirschvink J L. Carbon isotope and magnetic polarity evidence for non-depositional events within the Cambrian- Ordovician boundary section near Dayangcha, Jilin province, China[J]. Geological Magazine, 1993, 130(4): 443-452. |
[53] |
Ripperdan R L, Magaritz M, Nicoll R S, et al. Simultaneous changes in carbon isotopes, sea level, and conodont biozones within the Cambrian-Ordovician boundary interval at Black Mountain, Australia[J]. Geology, 1992, 20(11): 1039-1042. |
[54] |
Underwood C J, Deynoux M, Ghienne J F. High palaeolatitude (Hodh, Mauritania) recovery of graptolite faunas after the Hirnantian (end Ordovician) extinction event[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1998, 142(3/4): 91-105. |
[55] |
LaPorte D F, Holmden C, Patterson W P, et al. Local and global perspectives on carbon and nitrogen cycling during the Hirnantian glaciation[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009, 276(1/2/3/4): 182-195. |
[56] |
Munnecke A, Zhang Y D, Liu X, et al. Stable carbon isotope stratigraphy in the Ordovician of South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 307(1/2/3/4): 17-43. |
[57] |
Bergström S M, Lehnert O, Calner M, et al. A new Upper Middle Ordovician–Lower Silurian drillcore standard succession from Borenshult in Östergötland, southern Sweden: 2. Significance of δ13C chemostratigraphy[J]. GFF, 2012, 134(1): 39-63. |
[58] |
Harper D A T, Hammarlund E U, Rasmussen C M Ø. End Ordovician extinctions: A coincidence of causes[J]. Gondwana Research, 2014, 25(4): 1294-1307. |
[59] |
Harper D A T, Hints L. Hirnantian (Late Ordovician) brachiopod faunas across Baltoscandia: A global and regional context[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 444: 71-83. |
[60] |
Boucot A J, Rong J Y, Chen X, et al. Pre-Hirnantian Ashgill climatically warm event in the Mediterranean Region[J]. Lethaia, 2002, 36(2): 119-131. |
[61] |
Fortey R A, Cocks L R M. Late Ordovician global warming-the Boda event[J]. Geology, 2005, 33(5): 405-408. |
[62] |
Finnegan S, Heim N A, Peters S E, et al. Climate change and the selective signature of the Late Ordovician mass extinction[J]. Proceedings of the National Academy of Sciences of the United States of America, 2012, 109(18): 6829-6834. |
[63] |
Gorjan P, Kaiho K, Fike D A, et al. Carbon- and sulfur-isotope geochemistry of the Hirnantian (Late Ordovician) Wangjiawan (Riverside) section, South China: Global correlation and environmental event interpretation[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 337-338: 14-22. |
[64] |
Trotter J A, Williams I S, Barnes C R, et al. Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometry[J]. Science, 2008, 321(5888): 550-554. |
[65] |
Jeppsson L. Lithological and conodont distributional evidence for episodes and anomalous oceanic conditions during the Silurian[M]//Aldridge R J. Palaeobiology of conodonts. Chichester: Ellis Horwood, 1987: 129-145. |
[66] |
Bickert T, Pätzold J, Samtleben C, et al. Paleoenvironmental changes in the Silurian indicated by stable isotopes in brachiopod shells from Gotland, Sweden[J]. Geochimica et Cosmochimica Acta, 1997, 61(13): 2717-2730. |
[67] |
Brenchley P J, Carden G A, Hints L, et al. High-resolution stable isotope stratigraphy of Upper Ordovician sequences: Constraints on the timing of bioevents and environmental changes associated with mass extinction and glaciation[J]. GSA Bulletin, 2003, 115(1): 89-104. |
[68] |
Brenchley P J, Marshall J D, Carden G A F, et al. Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse Period[J]. Geology, 1994, 22(4), 295-298. |
[69] |
Kump L R, Arthur M A, Patzkowsky M E, et al. A weathering hypothesis for glaciation at high atmospheric pCO2 during the Late Ordovician[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1999, 152(1/2): 173-187. |
[70] |
Armstrong H A, Coe A L. Deep-sea sediments record the geophysiology of the Late Ordovician glaciation[J]. Journal of the Geological Society, 1997, 154(6): 929-934. |
[71] |
贵州省地质矿产局 .贵州省区域地质志[M].北京: 地质出版社, 1987: 97-137.
Bureau of Geology and Mineral Resources of Guizhou Province. Regional geology of Guizhou province[M]. Beijing: Geology Publishing House, 1987: 97-137. |
[72] |
Wilde P, Berry W B N. Destabilization of the oceanic density structure and its significance to marine “extinction” events[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1984, 48(2/3/4): 143-162. |
[73] |
Hammarlund E U, Dahl T W, Harper D A T, et al. A sulfidic driver for the end-Ordovician mass extinction[J]. Earth and Planetary Science Letters, 2012, 331-332: 128-139. |
[74] |
Pope K. Impact dust not the cause of the Cretaceous-Tertiary mass extinction[J]. Geology, 2002, 30(2): 99-102. |
[75] |
Harper D A T, Rong J Y. Patterns of change in the brachiopod faunas through the Ordovician-Silurian interface[J]. Modern Geology, 1995, 20(1): 83-100. |
[76] |
Sheehan P M. The Late Ordovician mass extinction[J]. Annual Review of Earth and Planetary Sciences, 2001, 29(1): 331-364. |
[77] |
Rasmussen C M Ø, Harper D A T. Interrogation of distributional data for the End Ordovician crisis interval: Where did disaster strike?[J]. Geological Journal, 2011, 46(5): 478-500. |
[78] |
Yan D T, Chen D Z, Wang Q C, et al. Carbon and sulfur isotopic anomalies across the Ordovician–Silurian boundary on the Yangtze Platform, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009, 274, 32-39. |
[79] |
Zhang T G, Shen Y N, Zhan R B, et al. Large perturbations of the carbon and sulfur cycle associated with the Late Ordovician mass extinction in South China[J]. Geology, 2009, 37(4): 299-302. |
[80] |
Bergström S M, Eriksson M E, Young S A, et al. Hirnantian (latest Ordovician) δ13C chemostratigraphy in southern Sweden and globally: A refined integration with the graptolite and conodont zone successions[J]. GFF, 2014, 136(2): 355-386. |
[81] |
Barnes C R. Ordovician oceans and climate[M]//Webby B D, Paris F, Droser M L, et al. The great Ordovician biodiversification event (The critical moments and perspectives in earth history and paleobiology). Columbia: Columbia University Press, 2004: 72-76. |
[82] |
Frakes L A, Francis J E, Syktus J I. Climate modes of the Phanerozoic[M]. Cambridge: Cambridge University Press, 1992: 15-25. |
[83] |
Hallam A. Phanerozoic sea-level changes[M]. New York: Columbia University Press, 1992. |
[84] |
Berner R A. Palaeo-CO2 and climate[J]. Nature, 1992, 358(6382): 114. |
[85] |
Berner R A. GEOCARB II; a revised model of atmospheric CO2 over Phanerozoic time[J]. American Journal of Science, 1994, 294(1): 56-91. |
[86] |
Yapp C J, Poths H. Ancient atmospheric CO2 pressures inferred from natural goethites[J]. Nature, 1992, 355(6358): 342-344. |
[87] |
Berner R A, Kothavala Z. Geocarb III; a revised model of atmospheric CO2 over Phanerozoic time[J]. American Journal of Science, 2001, 301(2): 182-204. |
[88] |
Tabor N J, Poulsen C J. Palaeoclimate across the Late Pennsylvanian–Early Permian tropical palaeolatitudes: A review of climate indicators, their distribution, and relation to palaeophysiographic climate factors[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2008, 268(3/4): 293-310. |
[89] |
Parrish J T. Upwelling and petroleum source beds, with reference to Paleozoic[J]. AAPG Bulletin, 1982, 66(6): 750-774. |
[90] |
Pohl A, Nardin E, Vandenbroucke T R A, et al. High dependence of Ordovician ocean surface circulation on atmospheric CO2 levels[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 458: 39-51. |
[91] |
Boucot A J, Xu C, Scotese C R, et al. Phanerozoic Paleoclimate: An atlas of Lithologic indicators of climate[M]. Tulsa, Oklahoma: SEPM Society for Sedimentary Geology, 2013: 38-47. |
[92] |
Gerhard L C, Harrison W E, “Bruno” Hanson B M. Introduction and Overview[M]//Gerhard L C, Harrison W E, Hanson B M. Geological perspectives of global climate change. American: American Association of Petroleum Geologists. 2001: 35-49. |
[93] |
Pope M, Read J F. Ordovician metre-scale cycles: Implications for climate and eustatic fluctuations in the central Appalachians during a global greenhouse, non-glacial to glacial transition[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1998, 138(1/2/3/4): 27-42. |
[94] |
Bigg G R. The Oceans and climate[M]. Cambridge: Cambridge University Press, 1996: 266. |