[1] 杜远生,黄虎,杨江海,等. 2013. 晚古生代—中三叠世右江盆地的格局和转换[J]. 地质论评,59(1):1-11.

Du Yuansheng, Huang Hu, Yang Jianghai, et al. 2013. The basin translation from Late Paleozoic to Triassic of the Youjiang Basin and its tectonic signification[J]. Geological Review, 59(1): 1-11.
[2] 冯增昭,鲍志东,吴胜和,等. 1997. 中国南方早中三叠世岩相古地理[J]. 地质科学,32(2):212-220.

Feng Zengzhao, Bao Zhidong, Wu Shenghe, et al. 1997. Lithofacies palaeogeography of the Early and Middle Triassic of South China[J]. Chinese Journal of Geology, 32(2): 212-220.
[3] 梁乐文,侯佳林,隋维康,等. 2023. 海洋沉积物微生物介导有机碳转化研究进展[J]. 微生物学报,63(5):1771-1786.

Liang Lewen, Hou Jialin, Sui Weikang, et al. 2023. Research progress on microbiome and organic carbon transformation in marine sediment[J]. Acta Microbiologica Sinica, 63(5): 1771-1786.
[4] 刘贝. 2023. 泥页岩中有机质:类型、热演化与有机孔隙[J]. 地球科学,48(12):4641-4657.

Liu Bei. 2023. Organic matter in shales: Types, thermal evolution, and organic pores[J]. Earth Science, 48(12): 4641-4657.
[5] 刘建波,江崎洋一,杨守仁,等. 2007. 贵州罗甸二叠纪末生物大灭绝事件后沉积的微生物岩的时代和沉积学特征[J]. 古地理学报,9(5):473-486.

Liu Jianbo, Yoichi E, Yang Shouren, et al. 2007. Age and sedimentology of microbialites after the end-Permian mass extinction in Luodian, Guizhou province[J]. Journal of Palaeogeography, 9(5): 473-486.
[6] 宋虎跃,童金南,田力,等. 2014. 南盘江地区二叠纪—三叠纪之交浅水台地古氧相研究[J]. 中国科学:地球科学,44(6):1273-1282.

Song Huyue, Tong Jinnan, Tian Li, et al. 2014. Paleo-redox conditions across the Permian-Triassic boundary in shallow carbonate platform of the Nanpanjiang Basin, South China[J]. Science China Earth Sciences, 44(6): 1273-1282.
[7] 田野,田云涛. 2020. 石墨化碳质物质拉曼光谱温度计原理与应用[J]. 地球科学进展,35(3):259-274.

Tian Ye, Tian Yuntao. 2020. Fundamentals and applications of Raman spectroscopy of carbonaceous material (RSCM) thermometry[J]. Advances in Earth Science, 35(3): 259-274.
[8] 王民, Li Zhongsheng. 2016. 激光拉曼技术评价沉积有机质热成熟度[J]. 石油学报,37(9):1129-1136.

Wang Min, Li Zhongsheng. 2016. Thermal maturity evaluation of sedimentary organic matter using laser Raman spectroscopy[J]. Acta Petrolei Sinica, 37(9): 1129-1136.
[9] 王永标,童金南,王家生,等. 2005. 华南二叠纪末大绝灭后的钙质微生物岩及古环境意义[J]. 科学通报,50(6):552-558.

Wang Yongbiao, Tong Jinnan, Wang Jiasheng, et al. 2005. Calcareous microbialites and paleoenvironmental significance after the Late Permian mass extinction in South China[J]. Chinese Science Bulletin, 50(6): 552-558.
[10] Adachi N, Asada Y, Ezaki Y, et al. 2017. Stromatolites near the Permian-Triassic boundary in Chongyang, Hubei province, South China: A geobiological window into palaeo-oceanic fluctuations following the end-Permian extinction[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 475: 55-69.
[11] Adachi N, Ezaki Y, Liu J B. 2004. The fabrics and origins of peloids immediately after the end-Permian extinction, Guizhou province, South China[J]. Sedimentary Geology, 164(1/2): 161-178.
[12] Alexandersson T. 1972. Intragranular growth of marine aragonite and Mg-calcite; evidence of precipitation from supersaturated seawater[J]. Journal of Sedimentary Research, 42(2): 441-460.
[13] Algeo T J, Henderson C M, Tong J N, et al. 2013. Plankton and productivity during the Permian-Triassic boundary crisis: An analysis of organic carbon fluxes[J]. Global and Planetary Change, 105: 52-67.
[14] Beyssac O, Goffé B, Chopin C, et al. 2002. Raman spectra of carbonaceous material in metasediments: A new geothermometer[J]. Journal of Metamorphic Geology, 20(9): 859-871.
[15] Broughton P L. 2023. Morphogenesis of crystal fan fabrics of the Wolfenden cool water tufa deposit in western Canada[J]. Facies, 69(1): 3.
[16] Canfield D E, van Zuilen M A, Nabhan S, et al. 2021. Petrographic carbon in ancient sediments constrains Proterozoic Era atmospheric oxygen levels[J]. Proceedings of the National Academy of Sciences of the United States of America, 118(23): e2101544118.
[17] Carlson C A, Hansell D A. 2015. sources DOM, sinks, reactivity, and budgets[M]//Hansell D A, Carlson C A. Biogeochemistry of marine dissolved organic matter. Amsterdam: Elsevier: 65-126.
[18] Chafetz H S. 1986. Marine peloids; a product of bacterially induced precipitation of calcite[J]. Journal of Sedimentary Research, 56(6): 812-817.
[19] Chen Z Q, Benton M J. 2012. The timing and pattern of biotic recovery following the end-Permian mass extinction[J]. Nature Geoscience, 5(6): 375-383.
[20] Chen Z Q, Fang Y H, Wignall P B, et al. 2022. Microbial blooms triggered pyrite framboid enrichment and oxygen depletion in carbonate platforms immediately after the latest Permian extinction[J]. Geophysical Research Letters, 49(7): e2021GL096998.
[21] Chen Z Q, Tu C Y, Pei Y, et al. 2019. Biosedimentological features of major microbe-metazoan transitions (MMTs) from Precambrian to Cenozoic[J]. Earth-Science Reviews, 189: 21-50.
[22] Derrien M, Jeanneau L, Jardé E, et al. 2023. Exploration of changes in the chemical composition of sedimentary organic matter and the underlying processes during biodegradation through advanced analytical techniques[J]. Environmental Chemistry, 20(5): 212-225.
[23] Dufresne W J B, Rufledt C J, Marshall C P. 2018. Raman spectroscopy of the eight natural carbonate minerals of calcite structure[J]. Journal of Raman Spectroscopy, 49(12): 1999-2007.
[24] Erwin D H. 1994. The Permo-Triassic extinction[J]. Nature, 367: 231-236.
[25] Ezaki Y, Liu J B, Nagano T, et al. 2008. Geobiological aspects of the earliest Triassic microbialites along the southern periphery of the tropical Yangtze Platform: Initiation and cessation of a microbial regime[J]. Palaios, 23(6): 356-369.
[26] Fang Y H, Chen Z Q, Kershaw S, et al. 2017. Permian-Triassic boundary microbialites at Zuodeng section, Guangxi province, South China: Geobiology and palaeoceanographic implications[J]. Global and Planetary Change, 152: 115-128.
[27] Flügel E. 2004. Microfacies of carbonate rocks: Analysis, interpretation and application[M]. Heidelberg, Berlin/New York: Springer: 1-976.
[28] Foster W J, Lehrmann D J, Yu M, et al. 2018. Persistent environmental stress delayed the recovery of marine communities in the aftermath of the latest Permian mass extinction[J]. Paleoceanography and Paleoclimatology, 33(4): 338-353.
[29] Gale L, Skaberne D, Peybernes C, et al. 2016. Carnian reefal blocks in the Slovenian Basin, eastern southern Alps[J]. Facies, 62(4): 23.
[30] Heindel K, Foster W J, Richoz S, et al. 2018. The formation of microbial-metazoan bioherms and biostromes following the latest Permian mass extinction[J]. Gondwana Research, 61: 187-202.
[31] Hong H L, Fang Q, Zhao L L, et al. 2017. Weathering and alteration of volcanic ashes in various depositional settings during the Permian-Triassic transition in South China: Mineralogical, elemental and isotopic approaches[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 486: 46-57.
[32] Kershaw S, Crasquin S, Li Y, et al. 2012. Microbialites and global environmental change across the Permian-Triassic boundary: A synthesis[J]. Geobiology, 10(1): 25-47.
[33] Kouketsu Y, Mizukami T, Mori H, et al. 2014. A new approach to develop the Raman carbonaceous material geothermometer for low‐grade metamorphism using peak width[J]. Island Arc, 23(1): 33-50.
[34] Luo G M, Wang Y B, Grice K, et al. 2013. Microbial-algal community changes during the latest Permian ecological crisis: Evidence from lipid biomarkers at Cili, South China[J]. Global and Planetary Change, 105: 36-51.
[35] Macintyre I G. 1985. Submarine cements-the peloidal question[M]//Schneidermann N, Harris P M. Carbonate cements: Based on a symposium sponsored by the society of economic paleontologists and mineralogists. Tulsa: SEPM Society for Sedimentary Geology: 508-508.
[36] Megonigal J P, Hines M E, Visscher P T. 2004. Anaerobic metabolism: Linkages to trace gases and aerobic processes[M]//Schlesinger W H. Biogeochemistry. Oxford: Elsevier-Pergamon: 1-18.
[37] Monty C L V. 1976. The origin and development of cryptalgal fabrics[J]. Developments in sedimentology, 20: 193-249.
[38] Neuweiler F. 1993. Development of Albian microbialites and micro-bialite reefs at marginal platform areas of the Vasco-Cantabrian Basin (Soba reef area, Cantabria, N. Spain)[J]. Facies, 29(1): 231-249.
[39] Pei Y, Chen Z Q, Fang Y H, et al. 2019. Volcanism, redox conditions, and microbialite growth linked with the end-Permian mass extinction: Evidence from the Xiajiacao section (western Hubei province), South China[J]. Palaeogeography, Palaeoclimatology, Palaeo-ecology, 519: 194-208.
[40] Pei Y, Duda J P, Reitner J. 2021. Sedimentary factories and ecosystem change across the Permian-Triassic Critical Interval (P-TrCI): Insights from the Xiakou area (South China)[J]. PalZ, 95(4): 709-725.
[41] Philp R P. 1985. Petroleum formation and occurrence[J]. Eos, Transactions American Geophysical Union, 66(37): 643-644.
[42] Reid R P. 1987. Nonskeletal peloidal precipitates in Upper Triassic reefs, Yukon Territory (Canada)[J]. Journal of Sedimentary Research, 57(5): 893-900.
[43] Samankassou E, Tresch J, Strasser A. 2005. Origin of peloids in Early Cretaceous deposits, Dorset, South England[J]. Facies, 51(1/2/3/4): 264-274.
[44] Sepkoski J J. 1984. A kinetic model of Phanerozoic taxonomic diversity. III. Post-Paleozoic families and mass extinctions[J]. Paleo-biology, 10(2): 246-267.
[45] Shen J, Schoepfer S D, Feng Q L, et al. 2015. Marine productivity changes during the end-Permian crisis and Early Triassic recovery[J]. Earth-Science Reviews, 149: 136-162.
[46] Sparkes R, Hovius N, Galy A, et al. 2013. Automated analysis of carbon in powdered geological and environmental samples by Raman spectroscopy[J]. Applied Spectroscopy, 67(7): 779-788.
[47] Sparkes R B, Hovius N, Galy A, et al. 2020. Survival of graphitized petrogenic organic carbon through multiple erosional cycles[J]. Earth and Planetary Science Letters, 531: 115992.
[48] Steinhauff D M, Abubshait A, Purkis S J. 2021. Red Sea Holocene carbonates: Windward platform margin and lagoon near Al-Wajh, northern Saudi Arabia[J]. Journal of Sedimentary Research, 91(8): 847-875.
[49] Sun S Q, Wright V P. 1989. Peloidal fabrics in Upper Jurassic reefal limestones, Weald Basin, southern England[J]. Sedimentary Ge-ology, 65(1/2): 165-181.
[50] Sun Y D, Joachimski M M, Wignall P B, et al. 2012. Lethally hot temperatures during the Early Triassic greenhouse[J]. Science, 338(6105): 366-370.
[51] Tang H, Kershaw S, Liu H, et al. 2017. Permian-Triassic boundary microbialites (PTBMs) in Southwest China: Implications for paleoenvironment reconstruction[J]. Facies, 63(1): 2.
[52] Wada S, Aoki M N, Tsuchiya Y, et al. 2007. Quantitative and qualitative analyses of dissolved organic matter released from Ecklonia cava Kjellman, in Oura Bay, Shimoda, Izu Peninsula, Japan[J]. Journal of Experimental Marine Biology and Ecology, 349(2): 344-358.
[53] Wu S Q, Chen Z Q, Fang Y H, et al. 2017. A Permian-Triassic boundary microbialite deposit from the eastern Yangtze Platform (Jiangxi province, South China): Geobiologic features, ecosystem composition and redox conditions[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 486: 58-73.
[54] Wu S Q, Chen Z Q, Fang Y H, et al. 2022. Benthic Pleurocapsales (Cyanobacteria) blooms catalyzing carbonate precipitation and dolomitization following the end-Permian mass extinction[J]. Geophysical Research Letters, 49(24): e2022GL100819.
[55] Wu S Q, Reitner J, Harper D A T, et al. 2024. New keratose sponges after the end-Permian extinction provide insights into biotic recoveries[J]. Geobiology, 22(1): e12582.
[56] Yuan D X, Zhang Y C, Shen S Z. 2018. Conodont succession and reassessment of major events around the Permian-Triassic boundary at the Selong Xishan section, southern Tibet, China[J]. Global and Planetary Change, 161: 194-210.
[57] Zheng Z J, Chen Z Q, Grasby S E, et al. 2024. Carbon-sulfur isotope and major and trace element variations across the Permian-Triassic boundary on a shallow platform setting (Xiejiacao, South China)[J]. Chemical Geology, 657: 122115.
[58] Zhou K, Pratt B R. 2019. Upper Devonian (Frasnian) stromatactis-bearing mud mounds, western Alberta, Canada: Reef framework dominated by peloidal microcrystalline calcite[J]. Journal of Sedimentary Research, 89(9): 833-848.