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Published in 2025 at "Geophysical Research Letters"
DOI: 10.1029/2025gl116574
Abstract: Phanerozoic extinctions may have been influenced by oceanic redox oscillations, as indicated by mixing‐induced negative pyrite Δ33S (Δ33Spy). However, the frequencies, intensities, and timescales of these oscillations remain elusive. Here, we measured stratigraphic Δ33Spy from…
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Keywords:
oceanic redox;
redox;
negative pyrite;
phanerozoic extinctions ... See more keywords