Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
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An enormous sulfur isotope excursion indicates marine anoxia
Permian–Triassic extinction event - Wikipedia
Frontiers Modeling hyperthermal events in the Mesozoic-Paleogene
The Permian–Triassic boundary section at Baghuk Mountain
Permian–Triassic extinction event - Wikipedia
A) The δ 238 U and (B) [U] boxplots. Whiskers denote the minimum
Ecosystem changes through the Permian–Triassic and Triassic
Ecosystem changes through the Permian–Triassic and Triassic
Summary of Early Triassic carbon isotope records - ScienceDirect
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Present-day and late Permian location of the investigated
Late Permian‐Early Triassic intracontinental tectonic inversion in
Permian δ 13 C carb , δ 18 O apatite and 87 Sr/ 86 Sr ratio
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Marine anoxia and delayed Earth system recovery after the end
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