Re‐Evaluating Water Column Reoxygenation During the End Permian Mass Extinction

Abstract Ocean anoxia is considered a key driver of the end‐Permian mass extinction (EPME). However, it is much debated whether there was an ocean reoxygenation phase during, and in the aftermath, of the EPME. Evidence for ocean reoxygenation is often inferred from the absence of framboidal pyrite i...

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Main Authors: F. Yang, S. Li, K. Y. An, D. P. G. Bond, R. Ao, X. B. Wu, L. L. Ma, Y. D. Sun
פורמט: Article
שפה:English
יצא לאור: Wiley 2024-10-01
סדרה:Geochemistry, Geophysics, Geosystems
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גישה מקוונת:https://doi.org/10.1029/2024GC011779