Reconstruction of Ecosystem and Biotic Recovery Following the End-Permian Mass Extinction in South China
The great Paleozoic-Mesozoic transition is characterized not only by the largest mass extinction at the end of Permian but also by the prolonged biotic recovery in the Early Triassic. Furthermore, the mass extinction happened synchronously in the sea and on land (Twitchett et al., 2001), and ultimately it ended the Paleozoic marine ecosystems lasting over 200 Myr (Erwin, 1993). From the mass extinction the Early Triassic recovery was clearly longer than those following other Phanerozoic extinctions (Erwin, 1998).
Tong Jinnan Z Q Chen Huang Yunfei
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of School of Earth and Environment, The University of Western Australia, 35 Stirling Highway,Crawley, W Key Laboratory of Biogeology and Environmental Geology of Ministry of Education,China University of
国际会议
The International Conference of Geobiology(地球生物学国际研讨会)
武汉
英文
167-169
2010-06-03(万方平台首次上网日期,不代表论文的发表时间)