[1]Erwin D H. The Great Paleozoic Crisis[M]. New York: Columbia University Press, 1993: 327. [2]Erwin D H, Bowring S A, Jin Y G. End-Permian Mass Extinctions: A review[M]∥Koebel C, MacLeod K G,eds. Catastrophic Events and Mass Extinctions: Impacts and Beyond. Boulder, Colorado: Geoloical Society of America Special Paper 356,2002: 363-383. [3]Bowring S A, Erwin D H, Jin Y G, et al. U/Pb zircon geochronology and tempo of the end-Permian mass extinction[J].Science, 1998, 280(5 366): 1 039-1 045. [4]Kamo S L, Czamanske G K, Amelin Y, et al. Rapid eruption of Siberian flood-volcanic rocks and evidence for coincidence with the Permian-Triassic boundary and mass extinction at 251 Ma[J]. Earth and Planetary Science Letters, 2003, 214(1/2): 75-91. [5]Wignall P B. Large igneous provinces and mass extinctions[J]. Earth-Science Reviews, 2001, 53(1/2): 1-33. [6]Payne J L, Turchyn A V, Paytan A, et al. Calcium isotope constraints on the end-Permian mass extinction[J]. Proceedings of the National Academy of Sciences,2010, 107(19): 8 543-8 548. [7]Sobolev S V, Sobolev A V, Kuzmin D V, et al. Linking mantle plumes, large igneous provinces and environmental catastrophes[J].Nature, 2011, 477(7 364): 312-316. [8]Becker L, Poreda R J, Hunt A G, et al. Impact event at the Permian-Triassic boundary: Evidence from extraterrestrial noble gases in fullerenes[J].Science, 2001, 291(5 508): 1 530-1 533. [9]Kaiho K, Kajiwara Y, Nakano T, et al. End-Permian catastrophe by a bolide impact: Evidence of a gigantic release of sulfur from the mantle[J].Geology, 2001, 29(9): 815-818. [10]Basu A R, Petaev M I, Poreda R J, et al. Chondritic meteorite fragments associated with the Permian-Triassic boundary in Antarctica[J].Science, 2003, 302(5 649): 1 388-1 392. [11]Wignall P B, Twitchett R J. Oceanic anoxia and the end Permian mass extinction[J]. Science, 1996, 272(5 265): 1 155-1 158. [12]Grice K, Cao C, Love G D, et al. Photic zone euxinia during the Permian-Triassic superanoxic event[J]. Science, 2005, 307(5 710): 706-709. [13]Cao C, Love G D, Hays L E, et al. Biogeochemical evidence for euxinic oceans and ecological disturbance presaging the end-Permian mass extinction event[J]. Earth and Planetary Science Letters, 2009, 281(3/4): 188-201. [14]Shen W, Lin Y, Xu L, et al. Pyrite framboids in the Permian-Triassic boundary section at Meishan, China: Evidence for dysoxic deposition[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007, 253(3/4): 323-331. [15]Liang H. End-Permian catastrophic event of marine acidification by hydrated sulfuric acid: Mineralogical evidence from Meishan section of South China[J].Chinese Science Bulletin,2002, 47(16): 1 393-1 397. [16]Maruoka T, Koeberl C, Hancox P J, et al. Sulfur geochemistry across a terrestrial Permian-Triassic boundary section in the Karoo Basin, South Africa[J]. Earth and Planetary Science Letters,2003, 206(1/2): 101-117. [17]Ward P D, Botha J, Buick R, et al. Abrupt and gradual extinction among Late Permian land vertebrates in the Karoo Basin, South Africa[J]. Science, 2005, 307(5 710): 709-714. [18]Krull E S, Retallack G J, Campbell H J, et al. Delta C-13(org) chemostratigraphy of the Permian-Triassic boundary in the Maitai Group, New Zealand: Evidence for high-latitudinal methane release[J]. New Zealand Journal of Geology and Geophysics,2000, 43(1): 21-32. [19]Ryskin G. Methane-driven oceanic eruptions and mass extinctions[J].Geology, 2003, 31(9): 741-744. [20]Wu Y, Fan J. Quantitative evaluation of the sea-level drop at the end-Permian: Based on reefs[J]. Acta Geologica Sinica, 2003, 77(1): 95-102. [21]Yin H, Feng Q, Lai X, et al. The protracted Permo-Triassic crisis and multi-episode extinction around the Permian-Triassic boundary[J]. Global and Planetary Change, 2007, 55(1/3): 1-20. [22]Yin H, Huang S, Zhang K, et al. The effects of volcanism on the Permo-Triassic mass extinction in South China[M]∥Sweet W C, Yang Zunyi, Dickins J M, et al, eds. Permo-Triassic Events in the Eastern Tethys, Stratigraphy, Classifiction, and Relations with the Western Tethys. London: Cambridge University Press,1992: 146-157. [23]Yin H, Huang S, Zhang K, et al. Volcanism at the Permian-Triassic boundary in South China and its effects on mass extinction[J]. Acta Geologica Sinica,1989, 63(2): 169-180. [24]Koeberl C, Farley K A, Peucker-Ehrenbrink B, et al. Geochemistry of the end-Permian extinction event in Austria and Italy: No evidence for an extraterrestrial component[J]. Geology, 2004, 32(12): 1 053-1 056. [25]Farley K A, Ward P, Garrison G, et al. Absence of extraterrestrial 3He in Permian-Triassic age sedimentary rocks[J]. Earth and Planetary Science Letters,2005, 240(2): 265. [26]Xu L, Lin Y, Shen W, et al. Platinum-group elements of the Meishan Permian-Triassic boundary section: Evidence for flood basaltic volcanism[J].Chemical Geology, 2007, 246(1/2): 55-64. [27]Page S E, Siegert F, Rieley J O, et al. The amount of carbon released from peat and forest fires in Indonesia during 1997[J]. Nature, 2002, 420(6 911): 61-65. [28]Abram N J, Gagan M K, McCulloch M T, et al. Coral reef death during the 1997 Indian Ocean dipole linked to Indonesian wildfires[J]. Science, 2003, 301(5 635): 952-955. [29]Wolbach W S, Gilmour I, Anders E, et al. Global fire at the Cretaceous-Tertiary boundary[J]. Nature, 1988, 334(25): 665-669. [30]Wolbach W S, Widicus S, Kyte F T. A search for soot from global wildfires in Central Pacific Cretaceous-Tertiary boundary and other extinction and impact horizon sediments[J]. Astrobiology, 2003, 3(1): 91-97.[31]Venkatesan M I, Dahl J. Organic geochemical evidence for global fires at the Cretaceous/Tertiary boundary[J]. Nature, 1989, 338(6 210): 57-60. [32]Harvey M C, Brassell S C, Belcher C M, et al. Combustion of fossil organic matter at the Cretaceous-Paleogene (K-P) boundary[J].Geology, 2008, 36(5): 355-358. [33]Belcher C M, Finch P, Collinson M E, et al. Geochemical evidence for combustion of hydrocarbons during the K-T impact event[J]. Proceedings of the National Academy of Sciences, 2009, 106(11): 4 112-4 117.[34]Chijiwa T, Arai T, Sugai T, et al. Fullerenes found in the Permian-Triassic mass extinction period[J]. Geophysical Research Letters, 1999, 26(6): 767-770. [35]Wang Shangyan, Yin Hongfu. Study on Terrestrial Permian-Triassic Boundary Strata in East Yunnan and West Guizhou[M].Wuhan: Press of China University of Geosciences, 2001.[王尚彦, 殷鸿福, 滇东黔西陆相二叠纪—三叠纪界线地层研究[M]. 武汉: 中国地质大学出版社, 2001.] [36]Shen Wenjie, Lin Yangting, Sun Yongge, et al. Black carbon record across the Permian-Triassic boundary section at Meishan, Changhsing county, Zhejiang province and its significance[J]. Acta Petrologica Sinica,2008, 24(10): 2 407-2 414.[沈文杰, 林杨挺, 孙永革, 等, 浙江省长兴县煤山剖面二叠—三叠系过渡地层中的黑碳记录及其地质意义[J]. 岩石学报, 2008, 24(10): 2 407-2 414.] [37]Wang Z Q, Chen A S. Traces of arborescent lycopsids and dieback of the forest vegetation in relation to the terminal Permian mass extinction in North China[J]. Review of Palaeobotany and Palynology, 2001, 117(4): 217-243. [38]Grice K, Nabbefeld B, Maslen E. Source and significance of selected polycyclic aromatic hydrocarbons in sediments (Hovea-3 well, Perth Basin, Western Australia) spanning the Permian-Triassic boundary[J]. Organic Geochemistry, 2007, 38(11): 1 795-1 803. [39]Xie S, Pancost R D, Huang J, et al. Changes in the global carbon cycle occurred as two episodes during the Permian-Triassic crisis[J]. Geology, 2007, 35(12): 1 083-1 086. [40]Cao C, Wang W, Liu L, et al. Two episodes of 13C-depletion in organic carbon in the Latest Permian: Evidence from the terrestrial sequences in northern Xinjiang, China[J]. Earth and Planetary Science Letters, 2008, 270(3/4): 251-257. [41]Nabbefeld B, Grice K, Summons R E, et al. Significance of Polycyclic Aromatic Hydrocarbons (PAHs) in Permian/Triassic boundary sections[J]. Applied Geochemistry, 2010, 25(9): 1 374-1 382. [42]Shen W, Sun Y, Lin Y, et al. Evidence for wildfire in the Meishan section and implications for Permian-Triassic events[J]. Geochimica et Cosmochimica Acta,2011, 75(7): 1 992-2 006. [43]Yin H, Yang F, Yu J, et al. An accurately delineated Permian-Triassic boundary in continental successions[J]. Science in China (Series D), 2007, 50(9): 1 281-1 292. [44]Yu J, Li H, Zhang S, et al. Timing of the terrestrial Permian-Triassic boundary biotic crisis: Implications from U-Pb dating of authigenic zircons[J]. Science in China (Series D), 2008, 51(11): 1 633-1 645. [45]Yin H, Zhang K, Tong J, et al. The Global Stratotype Section and Point of the Permian-Triassic boundary (GSSP) [J]. Episodes, 2001, 24(2): 102-114. [46]Mundil R, Ludwig K R, Metcalfe I, et al. Age and timing of the Permian mass extinctions: U/Pb dating of closed-system zircons[J]. Science, 2004, 305(5 691): 1 760-1 763. [47]Mundil R, Metcalfe I, Ludwig K R, et al. Timing of the Permian-Triassic biotic crisis: Implications from new zircon U/Pb age data (and their limitations) [J]. Earth and Planetary Science Letters, 2001, 187(1/2): 131-145. [48]Fang Zongjie. The Permain-Triassic boundary crisis: Patterns of extinction, collapse of various ecosystem, and their causes[M]∥Rong Jiayu, Fang Zongjie, eds. Mass Extinction and Recovery-Evidences from the Palaeozoic and Triassic of South China. Hefei: University of Science and Technology of China Press,2004: 785-928, 1 075-1 076.[方宗杰. 二叠纪—三叠纪之交生物大灭绝的型式、全球生态系统的巨变及其起因 [M]∥戎嘉余, 方宗杰编. 生物大灭绝与复苏——来自华南古生代和三叠纪的证据. 合肥: 中国科技大学出版社,2004: 785-928, 1 075-1 076.] [49]Shen W J, Lin Y T. Environmental conditions and events prior to the Permian-Triassic boundary at Meishan section, China[J]. Journal of Earth Science, 2010, 21: 151-153. [50]Zhang F, Feng Q, He W, et al. Multidisciplinary stratigraphy across the Permian-Triassic boundary in deep-water environment of the Dongpan section, South China[J]. Norwegian Journal of Geology, 2006, 86: 125-131. [51]He W, Shi G R, Feng Q, et al. Brachiopod miniaturization and its possible causes during the Permian-Triassic crisis in deep water environments, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 252(1/2): 145-163. [52]Zhang Fan, Feng Qinglai, He Weihong, et al. Multidisciplinary stratigraphy correlation of the Permian-Triassic boundary between Dongpan deep-water environment section,Guangxi and Meishan section[J]. Geological Science and Technology Information,2007, 26(1): 41-45.[张凡, 冯庆来, 何卫红, 等, 广西东攀P-T界线深水相剖面与煤山剖面地层学对比[J]. 地质科技情报, 2007, 26(1): 41-45.] [53]Peng Y, Shi G R. Life crises on land across the Permian-Triassic boundary in South China[J]. Global and Planetary Change, 2009, 65(3/4): 155-165. [54]Scott A C. The Pre-Quaternary history of fire[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 164(1/4): 281-329. [55]Hedges J I, Eglinton G, Hatcher P G, et al. The molecularly-uncharacterized component of nonliving organic matter in natural environments[J]. Organic Geochemistry, 2000, 31(10): 945-958. [56]Masiello C A. New directions in black carbon organic geochemistry[J]. Marine Chemistry, 2004, 92(1/4): 201-213. [57]Killops S D, Massoud M S. Polycyclic aromatic hydrocarbons of pyrolytic origin in ancient sediments: Evidence for Jurassic vegetation fires[J]. Organic Geochemistry, 1992, 18(1): 1-7. [58]Kennedy I M. Models of soot formation and oxidation[J]. Progress in Energy and Combustion Science, 1997, 23(2): 95-132. [59]Jiang C, Alexander R, Kagi R I, et al. Polycyclic aromatic hydrocarbons in ancient sediments and their relationships to palaeoclimate[J]. Organic Geochemistry, 1998, 29(5/7): 1 721-1 735. [60]Chylek P, Johnson B, Damiano P A, et al. Biomass burning record and black carbon in the GISP2 ice core[J]. Geophysical Research Letters, 1995, 22: 89-92. [61]Yalcin K, Wake C P, Kreutz K J, et al. A 1000-yr record of forest fire activity from Eclipse Icefield, Yukon, Canada[J]. The Holocene, 2006, 16(2): 200-209. [62]Huang C, Pang J, Chen S E, et al. Charcoal records of fire history in the Holocene loess-soil sequences over the southern Loess Plateau of China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 239(1/2): 28-44. [63]Miao X, Mason J A, Johnson W C, et al. High-resolution proxy record of Holocene climate from a loess section in southwestern Nebraska, USA[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 245(3/4): 368-381. [64]Zhou B, Shen C, Sun W, et al. Elemental carbon record of paleofire history on the Chinese Loess Plateau during the last 420 ka and its response to environmental and climate changes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 252(3/4): 617-625. [65]Arinobu T, Ishiwatari R, Kaiho K, et al. Spike of pyrosynthetic polycyclic aromatic hydrocarbons associated with an abrupt decrease in delta 13C of a terrestrial biomarker at the Cretaceous-Tertiary boundary at Caravaca, Spain[J]. Geology, 1999, 27(8): 723-726. [66]Marynowski L, Scott A C, Zaton M, et al. First multi-proxy record of Jurassic wildfires from Gondwana: Evidence from the Middle Jurassic of the Neuquén Basin, Argentina[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 299(1/2): 129-136. [67]Marynowski L, Filipiak P. Water column euxinia and wildfire evidence during deposition of the Upper Famennian Hangenberg event horizon from the Holy Cross Mountains (central Poland)[J]. Geological Magazine, 2007, 144(3): 569-595. [68]Marynowski L, Filipiak P, Pisarzowska A. Organic geochemistry and palynofacies of the Early-Middle Frasnian transition (Late Devonian) of the Holy Cross Mountains, southern Poland[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2008, 269(3/4): 152-165. [69]Poort R J, Clement-Westerhof J A, Looy C V, et al. Aspects of Permian palaeobotany and palynology. XVII. Conifer extinction in Europe at the Permian-Triassic junction: Morphology, ultrastructure and geographic/stratigraphic distribution of Nuskoisporites dulhuntyi (prepollen of Ortiseia, Walchiaceae)[J]. Review of Palaeobotany and Palynology, 1997, 97(1/2): 9. [70]Looy C V, Brugman W A, Dilcher D L, et al. The delayed resurgence of equatorial forests after the Permian-Triassic ecologic crisis[J]. Proceedings of the National Academy of Sciences, 1999, 96(24): 13 857-13 862. [71]Uhl D, Kerp H. Wildfires in the Late Palaeozoic of central Europe—The Zechstein (Upper Permian) of NW-Hesse (Germany)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 199(1/2): 1-15. [72]Uhl D, Lausberg S, Noll R, et al. Wildfires in the Late Palaeozoic of central Europe—An overview of the Rotliegend (Upper Carboniferous-Lower Permian) of the Saar-Nahe Basin (SW-Germany)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 207(1/2): 23-35. [73]Glasspool I. A major fire event recorded in the mesofossils and petrology of the Late Permian, Lower Whybrow coal seam, Sydney Basin, Australia[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 164(1/4): 357-380. [74]Uhl D, Abu Hamad A, Kerp H, et al. Evidence for palaeo-wildfire in the Late Permian palaeotropics-charcoalified wood from the Um Irna Formation of Jordan[J]. Review of Palaeobotany and Palynology, 2007, 144(3/4): 221-230. [75]Thomas B M, Willink R J, Grice K, et al. Unique marine Permian-Triassic boundary section from Western Australia[J]. Australian Journal of Earth Sciences, 2004, 51(3): 423-430. [76]Shen Wenjie. Mineral and Geochemical Explanation of Boundary Events: Evidence from Meishan Permian-Triassic Section[D]. Guangzhou: Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,2007.[沈文杰.二叠纪—三叠纪界线事件的矿物学、地球化学解译:以煤山剖面为例[D]. 广州: 中国科学院广州地球化学研究所, 2007.] [77]Grasby S E, Sanei H, Beauchamp B. Catastrophic dispersion of coal fly ash into oceans during the Latest Permian extinction[J]. Nature Geoscience, 2011,4(2):104-107. [78]Berner R A. Phanerozoic atmospheric oxygen: New results using the GEOCARBSULF model[J]. American Journal of Science, 2009, 309(7): 603-606. [79]Faure K, de Wit M J, Willis J P. Late Permian global coal hiatus linked to 13C-depleted CO2 flux into the atmosphere during the final consolidation of Pangea[J]. Geology, 1995, 23(6): 507-510. [80]Retallack G J, Jahren A H. Methane release from igneous intrusion of coal during Late Permian extinction events[J]. Journal of Geology, 2008, 116(1): 1-20. [81]Berner R A. Carbon, sulfur and O2 across the Permian-Triassic boundary[J]. Journal of Geochemical Exploration, 2006, 88(1/3): 416-418. [82]Wignall P B, Newton R, Brookfield M E. Pyrite framboid evidence for oxygen-poor deposition during the Permian-Triassic crisis in Kashmir[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 216(3/4): 183-188. [83]Wignall P B, Twitchett R J. Extent, duration, and nature of the Permian-Triassic superanoxic event[M]∥Koebel C, MacLeod K G,eds. Catastrophic Events and Mass Extinctions: Impacts and Beyond. Boulder, Colorado: Geoloical Society of America Special Paper 356, 2002: 395-413. [84]Wignall P B, Newton R. Pyrite framboid dimeter as a measure of oxygen deficiency in ancient mudrocks[J]. American Journal of Science, 1998, 298: 537-552. [85]Wilkin R T, Barnes H L, Brantley S L. The size distribution of framboidal pyrite in modern sediments: An indicator of redox conditions[J]. Geochimica et Cosmochimica Acta, 1996, 60(20): 3 897-3 912. [86]Scott A C, Glasspool I J. The diversification of Paleozoic fire systems and fluctuations in atmospheric oxygen concentration[J]. Proceedings of the National Academy of Sciences, 2006, 103(29): 10 861-10 865.[87]Belcher C M, McElwain J C. Limits for combustion in low O2 redefine paleoatmospheric predictions for the Mesozoic[J]. Science, 2008, 321(5 893): 1 197-1 200. [88]Finkelstein D B, Pratt L M, Curtin T M, et al. Wildfires and seasonal aridity recorded in Late Cretaceous strata from south-eastern Arizona, USA[J]. Sedimentology, 2005, 52(3): 587-599. [89]Pyne S J, Andrews P L, Laven R D. Introduction to Wildland Fire[M].New York: John Wiley & Sons, Inc. 1996. [90]Vega J A, Fernández C, Fonturbel T. Throughfall, runoff and soil erosion after prescribed burning in gorse shrubland in Galicia (NW Spain)[J]. Land Degradation & Development, 2005, 16(1): 37-51. [91]Kunimaru T, Shimizu H, Takahashi K, et al. Differences in geochemical features between Permian and Triassic cherts from the Southern Chichibu terrane, southwest Japan: REE abundances, major element compositions and Sr isotopic ratios[J]. Sedimentary Geology, 1998, 119(3/4): 195-217. [92]Kato Y, Nakao K, Isozaki Y. Geochemistry of Late Permian to Early Triassic pelagic cherts from southwest Japan: Implications for an oceanic redox change[J]. Chemical Geology, 2002, 182(1): 15-34. [93]Zhou Yaoqi, Chai Zhifang, Mao Xueying, et al. Abnormal Sr isotope event in the Permian-Triassic boundary in Meishan section, Zhejiang[J]. Journal of the Graduate School of the Chinese Academy of Sciences,1990, 7(1): 83-88.[周瑶琪, 柴之芳, 毛雪瑛, 等.浙江长兴煤山二叠、三叠系界线Sr同位素异常事件[J]. 中国科技大学研究生院学报, 1990, 7(1): 83-88.] [94]Korte C, Kozur H W, Bruckschen P, et al. Strontium isotope evolution of Late Permian and Triassic seawater[J]. Geochimica et Cosmochimica Acta, 2003, 67(1): 47-62. [95]Sephton M A, Looy C V, Brinkhuis H, et al. Catastrophic soil erosion during the end-Permian biotic crisis[J]. Geology, 2005, 33(12): 941-944. [96]Wang C, Visscher H. Abundance anomalies of aromatic biomarkers in the Permian-Triassic boundary section at Meishan, China—Evidence of end-Permian terrestrial ecosystem collapse[J].Palaeogeography, Palaeoclimatology, Palaeoecology,2007, 252(1/2): 291-303. [97]Xiong C, Wang Q. Permian-Triassic land-plant diversity in South China: Was there a mass extinction at the Permian/Triassic boundary?[J]. Paleobiology, 2011, 37(1): 157-167. [98]Shen S Z, Crowley J L, Wang Y, et al. Calibrating the end-Permian mass extinction[J]. Science, 2011, 334(6 061): 1 367-1 372. |