Euxinic Ocean during the Late Devonian Mass Extinction Inferred from Organic Compounds
There were five mass extinctions of Earth life during the past 500 million years. The second crisis of the big five mass extinctions occurred near the Frasnian/Famennian (F/F) boundary in the Late Devonian. This extinction impacted mainly oceanic regime and resulted in 21% of families and 50% of genera among oceanic life being wiped out (Sepkoski, 1986). In particular, brachiopods, trilobites, conodonts, tabulate corals, and stromatoporoids have been severely affected and suffered high extinction rates (McGhee,1996, 1989; Stanley, 1987).
Susumu Yatsu Kunio Kaiho Masahiro Oba ZQ Chen Jean-Georges Casier James D Wright
Graduate School of Science, Tohoku University, Aoba-ku, Sendai 980-8578, Japan School of Earth & Environment, The University of Western Australia, 35 Stirling Highway,Crawley, WA Department of Paleontology, Belgian Royal Institute of Natural Sciences, Vautier Street, 29 B-1000,B Department of Geological Sciences, Rutgers University, 610 Taylor Road, Piscataway, NJ 08854, USA
国际会议
The International Conference of Geobiology(地球生物学国际研讨会)
武汉
英文
94-95
2010-06-03(万方平台首次上网日期,不代表论文的发表时间)