Chen Z Q,Kaiho K,Survival brachiopod faunas of the endPermian mass extinction from the southern Alps (Italy) and South China,London:cambridge University Press,2006.
Erwin D H,The End-Permian Mass Extinction,Annual Review of Ecology and Systematics,1990.
[18]
Erwin D H,The Permo-Triassic extinction,Nature,1994.
[19]
Hallam A,Wignal P B,Mass extinctions and their aftermath,Oxford:Oxford University Press,1997.
[20]
Jiang H S,Lai X L,Luo G M,et,al,Restudy of conodont zonation and evolution across the P/T boundary at Meishan section,Changxing,Zhejiang,China,Global and Planetary Change,2007.
[21]
Kajiwara Y,Yamakita S,Ishida K,et,al,Development of a largely anoxic stratified ocean and its temporary massive mixing at the Permian/Triassic boundary supported by the sulfur isotopic record,Palaeogeography Palaeoclimatology Palaeoecology,1994.
[22]
Sepkoski J J,A factor analytic description of the Phanerozoic marine fossil record,Paleobiology,1981.
[23]
Stanley S M,Paleozoic mass extinction,shared patterns suggest global cooling as a common cause,American Journal of Science,1988.
[24]
Wignal P B,Hallam A,Anoxia as a cause of the PermoTriassic mass extinction:facies evidence from northern Italy and the western United States,Palaeogeography,Palaeoclimatology,Palaeoecology,1992.
[25]
Wignal P B,Hallam A,Facies changes and the endPermian mass extinction in S.E.Sichuan,China,Palaios,1996.
[26]
Wu S B,Liu J H,Zhu Q,The beginning climax and amplitude of transgression,北京:地质出版社,1996.
[27]
Xu D Y,Ma S L,Chai Z F,Mao,X,Y,et,al,Abundance variation of iridium and trace elements at the Permian/Triassic boundary at Shangsi in China,Nature,1985.