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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 17 novembro 2024
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
The Permian–Triassic boundary section at Baghuk Mountain, Central
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Different triggers for the two pulses of mass extinction across
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Coeval Nevada (blue) and Illinois (red) δ 238 U trends. Gray
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
Boreal earliest Triassic biotas elucidate globally depauperate
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Permo–Triassic boundary carbon and mercury cycling linked to
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Geosciences, Free Full-Text
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Stratigraphic log from Island Bay, Waiheke Island, New Zealand
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
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