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Multiple episodes o...
Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction
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- Zhang, Feifei (författare)
- Arizona State University
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- Romaniello, Stephen J. (författare)
- Arizona State University
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- Algeo, Thomas J. (författare)
- China University of Geosciences,University of Cincinnati
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- Lau, Kimberly V. (författare)
- University of California, Riverside
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- Clapham, Matthew E. (författare)
- University of California, Santa Cruz
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- Richoz, Sylvain (författare)
- Lund University,Lunds universitet,Geologiska institutionen,Naturvetenskapliga fakulteten,Department of Geology,Faculty of Science,Karl-Franzens-University of Graz
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- Herrmann, Achim D. (författare)
- Louisiana State University
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- Smith, Harrison (författare)
- Arizona State University
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- Horacek, Micha (författare)
- Higher Federal Education and Research Institute Francisco Josephinum,University of Vienna,Karl-Franzens-University of Graz
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- Anbar, Ariel D. (författare)
- Arizona State University
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(creator_code:org_t)
- American Association for the Advancement of Science (AAAS), 2018
- 2018
- Engelska.
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Ingår i: Science Advances. - : American Association for the Advancement of Science (AAAS). - 2375-2548. ; 4:4
- Relaterad länk:
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http://dx.doi.org/10... (free)
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https://doi.org/10.1...
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https://lup.lub.lu.s...
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https://doi.org/10.1...
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Abstract
Ämnesord
Stäng
- Explaining the ∼5-million-year delay in marine biotic recovery following the latest Permian mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for both geological and biological sciences. Ocean redox perturbations may have played a critical role in this delayed recovery. However, the lack of quantitative constraints on the details of Early Triassic oceanic anoxia (for example, time, duration, and extent) leaves the links between oceanic conditions and the delayed biotic recovery ambiguous. We report high-resolution U-isotope (δ238U) data from carbonates of the uppermost Permian to lowermost Middle Triassic Zal section (Iran) to characterize the timing and global extent of ocean redox variation during the Early Triassic. Our δ238U record reveals multiple negative shifts during the Early Triassic. Isotope mass-balance modeling suggests that the global area of anoxic seafloor expanded substantially in the Early Triassic, peaking during the latest Permian to mid-Griesbachian, the late Griesbachian to mid-Dienerian, the Smithian-Spathian transition, and the Early/Middle Triassic transition. Comparisons of the U-, C-, and Sr-isotope records with a modeled seawater PO4 3- concentration curve for the Early Triassic suggest that elevated marine productivity and enhanced oceanic stratification were likely the immediate causes of expanded oceanic anoxia. The patterns of redox variation documented by the U-isotope record show a good first-order correspondence to peaks in ammonoid extinctions during the Early Triassic. Our results indicate that multiple oscillations in oceanic anoxia modulated the recovery of marine ecosystems following the latest Permian mass extinction.
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
Publikations- och innehållstyp
- art (ämneskategori)
- ref (ämneskategori)
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Zhang, Feifei
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Romaniello, Step ...
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Algeo, Thomas J.
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Lau, Kimberly V.
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Clapham, Matthew ...
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Richoz, Sylvain
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visa fler...
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Herrmann, Achim ...
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Smith, Harrison
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Horacek, Micha
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Anbar, Ariel D.
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