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- W2000705086 abstract "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). Previously, anoxic sea-water condition was considered as the candidate responsible for the F/F mass extinction simply because of the widespread black shale near the boundary worldwide (House, 1985). Both stable carbon and sulfur isotopic signals and trace metal element features indicate that the F/F mass extinction was probably caused" @default.
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- W2000705086 date "2010-06-01" @default.
- W2000705086 modified "2023-09-23" @default.
- W2000705086 title "Euxinic ocean during the Late Devonian mass extinction inferred from organic compounds" @default.
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- W2000705086 doi "https://doi.org/10.1007/s12583-010-0178-x" @default.
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