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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 10 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
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
Frontiers Biotic Response to Rapid Environmental Changes During
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
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
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U
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
Upper limits on the extent of seafloor anoxia during the PETM from
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Permian–Triassic mass extinction pulses driven by major marine
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
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