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

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Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Permian-Triassic Boundary - an overview
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Minerals, Free Full-Text
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Diachronous end-Permian terrestrial ecosystem collapse with its
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Persistent late Permian to Early Triassic warmth linked to
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Frontiers Biotic Response to Rapid Environmental Changes During
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
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
Permian–Triassic extinction event - Wikipedia
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Minerals, Free Full-Text
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Altered fluvial patterns in North China indicate rapid climate
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Multiple S-isotopic evidence for episodic shoaling of anoxic water
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