Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction

Feifei Zhang, Stephen J. Romaniello, Thomas J. Algeo, Kimberly V. Lau, Matthew E. Clapham, Sylvain Richoz, Achim D. Herrmann, Harrison Smith, Micha Horacek, Ariel Anbar

Research output: Contribution to journalArticle

24 Citations (Scopus)

Abstract

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.

Original languageEnglish (US)
Article numbere1602921
JournalScience advances
Volume4
Issue number4
DOIs
StatePublished - Apr 11 2018

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mass extinction
anoxia
global warming
Permian
Triassic
weathering
isotope
ocean
Phanerozoic
marine ecosystem
mass balance
stratification
seafloor
extinction
oscillation
perturbation
seawater
carbonate
productivity
modeling

ASJC Scopus subject areas

  • General

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Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction. / Zhang, Feifei; Romaniello, Stephen J.; Algeo, Thomas J.; Lau, Kimberly V.; Clapham, Matthew E.; Richoz, Sylvain; Herrmann, Achim D.; Smith, Harrison; Horacek, Micha; Anbar, Ariel.

In: Science advances, Vol. 4, No. 4, e1602921, 11.04.2018.

Research output: Contribution to journalArticle

Zhang, F, Romaniello, SJ, Algeo, TJ, Lau, KV, Clapham, ME, Richoz, S, Herrmann, AD, Smith, H, Horacek, M & Anbar, A 2018, 'Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction', Science advances, vol. 4, no. 4, e1602921. https://doi.org/10.1126/sciadv.1602921
Zhang, Feifei ; Romaniello, Stephen J. ; Algeo, Thomas J. ; Lau, Kimberly V. ; Clapham, Matthew E. ; Richoz, Sylvain ; Herrmann, Achim D. ; Smith, Harrison ; Horacek, Micha ; Anbar, Ariel. / Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction. In: Science advances. 2018 ; Vol. 4, No. 4.
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AB - 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.

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