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• W2473761874 abstract "The end-Guadalupian (middle Permian) mass extinction recorded the disappearance of shelf faunas such as fusulinids, small foraminifers, brachiopods, rugose corals which flourished in the warm shallow marine habitats after the late Pennsylvanian–early Permian glaciation. The causes for this mass extinction are still unclear. Marine anoxia, often as a cause for other mass extinctions, has been paid less attention in this extinction. Here we present a comprehensive study including pyrite morphology and sulfur isotopic compositions of pyrite across the Guadalupian–Lopingian (middle–upper Permian; G–L) boundary at Tianfengping in northern Yangtze Platform and at Penglaitan in southern Yangtze Platform in South China. Our results show that the sulfur isotope ratios of pyrite mainly track the framboid size distributions in these two sections. Anoxia and intermittent euxinia occur at the G–L boundary evidenced by the coincidence between reduction of framboid size and the extremely negative sulfur isotope values of pyrite involving disproportionation, and corresponds to the main mass extinction of the end-Guadalupian, suggesting a causal link between them. Long-term dysoxic conditions during the middle Capitanian are evidenced by the relative small framboid size and lower sulfur isotope ratios of pyrite, and coincide with the first pulse of the end-Guadalupian mass extinction, also suggesting a causal link between them. The oxygen-depletion conditions in the Capitanian during the global sea level falling may be the main cause for the end-Guadalupian mass extinction." @default.
• W2473761874 created "2016-07-22" @default.
• W2473761874 creator A5003297301 @default.
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• W2473761874 date "2016-11-01" @default.
• W2473761874 modified "2023-10-18" @default.
• W2473761874 title "Redox conditions across the G–L boundary in South China: Evidence from pyrite morphology and sulfur isotopic compositions" @default.
• W2473761874 cites W1534009691 @default.
• W2473761874 cites W1850306293 @default.
• W2473761874 cites W1966990309 @default.
• W2473761874 cites W1968461998 @default.
• W2473761874 cites W1969282993 @default.
• W2473761874 cites W1970673921 @default.
• W2473761874 cites W1972477780 @default.
• W2473761874 cites W1979658461 @default.
• W2473761874 cites W1980803462 @default.
• W2473761874 cites W1981837617 @default.
• W2473761874 cites W1983472402 @default.
• W2473761874 cites W1985922088 @default.
• W2473761874 cites W1986786567 @default.
• W2473761874 cites W1990648220 @default.
• W2473761874 cites W1991491867 @default.
• W2473761874 cites W1992889053 @default.
• W2473761874 cites W1996766054 @default.
• W2473761874 cites W1997853880 @default.
• W2473761874 cites W2000753816 @default.
• W2473761874 cites W2001472611 @default.
• W2473761874 cites W2002367938 @default.
• W2473761874 cites W2004964550 @default.
• W2473761874 cites W2004974947 @default.
• W2473761874 cites W2005428926 @default.
• W2473761874 cites W2005482608 @default.
• W2473761874 cites W2009254162 @default.
• W2473761874 cites W2013839205 @default.
• W2473761874 cites W2014936152 @default.
• W2473761874 cites W2016769341 @default.
• W2473761874 cites W2017260351 @default.
• W2473761874 cites W2018866466 @default.
• W2473761874 cites W2023008088 @default.
• W2473761874 cites W2027184874 @default.
• W2473761874 cites W2030045843 @default.
• W2473761874 cites W2043894211 @default.
• W2473761874 cites W2045019194 @default.
• W2473761874 cites W2054380694 @default.
• W2473761874 cites W2060617303 @default.
• W2473761874 cites W2064154081 @default.
• W2473761874 cites W2065234137 @default.
• W2473761874 cites W2066216729 @default.
• W2473761874 cites W2069628154 @default.
• W2473761874 cites W2072320126 @default.
• W2473761874 cites W2076389367 @default.
• W2473761874 cites W2076644423 @default.
• W2473761874 cites W2077384023 @default.
• W2473761874 cites W2077929362 @default.
• W2473761874 cites W2079115522 @default.
• W2473761874 cites W2079792015 @default.
• W2473761874 cites W2081641920 @default.
• W2473761874 cites W2081829616 @default.
• W2473761874 cites W2087328120 @default.
• W2473761874 cites W2087877261 @default.
• W2473761874 cites W2095242207 @default.
• W2473761874 cites W2103296666 @default.
• W2473761874 cites W2104131259 @default.
• W2473761874 cites W2107225219 @default.
• W2473761874 cites W2118715042 @default.
• W2473761874 cites W2119181573 @default.
• W2473761874 cites W2124640583 @default.
• W2473761874 cites W2128214815 @default.
• W2473761874 cites W2134314242 @default.
• W2473761874 cites W2134698830 @default.
• W2473761874 cites W2134893871 @default.
• W2473761874 cites W2137854548 @default.
• W2473761874 cites W2140605065 @default.
• W2473761874 cites W2146180563 @default.
• W2473761874 cites W2159138019 @default.
• W2473761874 cites W2161184773 @default.
• W2473761874 cites W2166869273 @default.
• W2473761874 cites W2169078581 @default.
• W2473761874 cites W2171033545 @default.
• W2473761874 cites W2191864853 @default.
• W2473761874 cites W2196128329 @default.
• W2473761874 cites W2213096039 @default.
• W2473761874 cites W2251477239 @default.
• W2473761874 cites W2330416027 @default.
• W2473761874 cites W2331013380 @default.
• W2473761874 cites W2335661622 @default.
• W2473761874 cites W313187678 @default.
• W2473761874 cites W4230917528 @default.
• W2473761874 cites W62072001 @default.
• W2473761874 cites W629495074 @default.
• W2473761874 doi "https://doi.org/10.1016/j.chemgeo.2016.07.009" @default.
• W2473761874 hasPublicationYear "2016" @default.
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