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Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and

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Last updated 25 março 2025
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Age and pattern of the southern high-latitude continental end
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Present-day and late Permian location of the investigated
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
A) Smoothed δ 238 U curve. (B) Modeled percent euxinic seafloor
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Rapid expansion of oceanic anoxia immediately before the end
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Frontiers Modeling hyperthermal events in the Mesozoic-Paleogene
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Ecosystem changes through the Permian–Triassic and Triassic
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Severest crisis overlooked—Worst disruption of terrestrial
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
PDF) Marine anoxia and delayed Earth system recovery after the end
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Timing and Provenance of Volcanic Fluxes Around the Permian
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