Earth SciencesCommunications Earth & Environment
Shifts in magnetic mineral assemblages support ocean deoxygenation before the end-Permian mass extinction
M. Zhang, H. Qin, et al.
Dive into the remarkable findings of a study led by Min Zhang and colleagues, which reveals how long-term oceanic redox conditions and deoxygenation trends started over 0.9 million years before the end-Permian mass extinction. Discover the environmental changes that set the stage for this significant extinction event.
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