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• W2783753929 endingPage "104" @default.
• W2783753929 startingPage "92" @default.
• W2783753929 abstract "The links between large-scale volcanism, carbon cycle perturbations and the biotic crises at the End-Triassic Extinction event (ETE) are not well understood. The ETE seems to be marked by three carbon isotope excursions (CIEs) likely triggered by different eruptive phases of the Central Atlantic Magmatic Province (CAMP). These three CIEs appear to occur during the late Rhaetian, close to the Triassic/Jurassic boundary (TJB), but the relative timing connecting the volcanism, carbon perturbations and extinctions is still subject to debate resulting from: i) the difficulties in long-distance biostratigraphic correlations of Rhaetian successions due to the step-like extinction pattern characterizing the ETE, and to the lack of globally correlatable key-fossil group(s) across the system boundary; ii) the limit of coverage of available δ13C profiles to the system boundary interval, rather than the entire Rhaetian; iii) the inherent difficulties in correlating CIEs without clear biostratigraphic markers. Here we present a δ13Corg curve from the Lombardy Basin which covers for the first time the entire Rhaetian. Using this chemostratigraphy, we propose two possible correlations (option 1 and option 2) with other late Rhaetian to early Hettangian successions worldwide. These two possible correlations rely on a combination of paleontological (ammonoids, pollens, conodonts), lithostratigraphic and geochemical constraints. Option 2 in particular has important implications for the causality and geochronology of the ETE events by suggesting that the sharp negative peak usually considered to be the “initial” CIE in the Lombardy might represent a carbon perturbation within the negative trend of the “main” CIE. This implies that a reconsideration of the succession of biotic events occurring during this time interval is required." @default.
• W2783753929 created "2018-01-26" @default.
• W2783753929 creator A5002423302 @default.
• W2783753929 creator A5036309577 @default.
• W2783753929 creator A5089435793 @default.
• W2783753929 date "2018-03-01" @default.
• W2783753929 modified "2023-09-30" @default.
• W2783753929 title "A new Rhaetian δ13Corg record: Carbon cycle disturbances, volcanism, End-Triassic mass Extinction (ETE)" @default.
• W2783753929 cites W1492179824 @default.
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• W2783753929 cites W1502180668 @default.
• W2783753929 cites W1505358646 @default.
• W2783753929 cites W1617554277 @default.
• W2783753929 cites W1917729849 @default.
• W2783753929 cites W1963202973 @default.
• W2783753929 cites W1967424909 @default.
• W2783753929 cites W1971652932 @default.
• W2783753929 cites W1972359313 @default.
• W2783753929 cites W1974817692 @default.
• W2783753929 cites W1975799571 @default.
• W2783753929 cites W1976700644 @default.
• W2783753929 cites W1979240913 @default.
• W2783753929 cites W1984450591 @default.
• W2783753929 cites W1985174323 @default.
• W2783753929 cites W1985210594 @default.
• W2783753929 cites W1989594034 @default.
• W2783753929 cites W1991980404 @default.
• W2783753929 cites W1997469183 @default.
• W2783753929 cites W2004987366 @default.
• W2783753929 cites W2007663434 @default.
• W2783753929 cites W2008268722 @default.
• W2783753929 cites W2011346321 @default.
• W2783753929 cites W2021089559 @default.
• W2783753929 cites W2021096449 @default.
• W2783753929 cites W2022609833 @default.
• W2783753929 cites W2027540032 @default.
• W2783753929 cites W2028032600 @default.
• W2783753929 cites W2030648663 @default.
• W2783753929 cites W2040535069 @default.
• W2783753929 cites W2048459684 @default.
• W2783753929 cites W2051601543 @default.
• W2783753929 cites W2053385554 @default.
• W2783753929 cites W2067067936 @default.
• W2783753929 cites W2075525949 @default.
• W2783753929 cites W2079852953 @default.
• W2783753929 cites W2080822284 @default.
• W2783753929 cites W2086473743 @default.
• W2783753929 cites W2088197346 @default.
• W2783753929 cites W2091732975 @default.
• W2783753929 cites W2096237922 @default.
• W2783753929 cites W2104345436 @default.
• W2783753929 cites W2104767413 @default.
• W2783753929 cites W2104996180 @default.
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• W2783753929 cites W2107051375 @default.
• W2783753929 cites W2120596386 @default.
• W2783753929 cites W2121834312 @default.
• W2783753929 cites W2138014738 @default.
• W2783753929 cites W2139806332 @default.
• W2783753929 cites W2143502003 @default.
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• W2783753929 cites W2144115502 @default.
• W2783753929 cites W2146743797 @default.
• W2783753929 cites W2148519074 @default.
• W2783753929 cites W2148919921 @default.
• W2783753929 cites W2152700412 @default.
• W2783753929 cites W2153097587 @default.
• W2783753929 cites W2159506993 @default.
• W2783753929 cites W2165717667 @default.
• W2783753929 cites W2166913044 @default.
• W2783753929 cites W2169413716 @default.
• W2783753929 cites W2182246028 @default.
• W2783753929 cites W2292098794 @default.
• W2783753929 cites W2316800547 @default.
• W2783753929 cites W2323609894 @default.
• W2783753929 cites W2331303754 @default.
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• W2783753929 cites W2619246666 @default.
• W2783753929 cites W3012722194 @default.
• W2783753929 cites W322753937 @default.
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• W2783753929 doi "https://doi.org/10.1016/j.earscirev.2018.01.004" @default.
• W2783753929 hasPublicationYear "2018" @default.
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