Articles | Volume 22, issue 8
https://doi.org/10.5194/cp-22-1481-2026
https://doi.org/10.5194/cp-22-1481-2026
Research article
 | 
06 Aug 2026
Research article |  | 06 Aug 2026

Permian-Triassic redox shift and its ferruginous aftermath in epicontinental seas

Fen Yang, Sen Li, Stephen E. Grasby, David P. G. Bond, Ming Pan, and Yadong Sun

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Cited articles

Alcott, L. J., Krause, A. J., Hammarlund, E. U., Bjerrum, C. J., Scholz, F., Xiong, Y., Hobson, A. J., Neve, L., Mills, B. J. W., März, C., Schnetger, B., Bekker, A., and Poulton, S. W.: Development of Iron Speciation Reference Materials for Palaeoredox Analysis, Geostand. Geoanal. Res., 44, 581–591, https://doi.org/10.1111/ggr.12342, 2020. 
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Algeo, T. J. and Tribovillard, N.: Environmental analysis of paleoceanographic systems based on molybdenum–uranium covariation, Chem. Geol., 268, 211–225, https://doi.org/10.1016/j.chemgeo.2009.09.001, 2009. 
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Algeo, T. J., Ellwood, B., Nguyen, T. K. T., Rowe, H., and Maynard, J. B.: The Permian–Triassic boundary at Nhi Tao, Vietnam: evidence for recurrent influx of sulfidic watermasses to a shallow-marine carbonate platform, Palaeogeogr. Palaeoclimatol. Palaeoecol., 252, 304–327, https://doi.org/10.1016/j.palaeo.2006.11.055, 2007. 
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Short summary
The end-Permian mass extinction was the most severe loss of life in Earth history, yet the role of ocean oxygen restriction remains debated. We examined rock records from South China and western Canada to track redox conditions before and after the crisis. Oxygen levels were already low prior to the extinction, and widespread seafloor anoxia developed at its peak. Afterwards, ferruginous conditions dominated, reducing nutrient availability, limiting productivity, and slowing life’s recovery.
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