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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 31 maio 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
Major Early-Middle Devonian oceanic oxygenation linked to early
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Summary of Early Triassic carbon isotope records - ScienceDirect
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Provenance and sedimentary evolution from the Middle Permian to
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
Mercury isotope evidence for marine photic zone euxinia across the
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Paired δ 238 U and δ 13 C data from carbonate slope successions
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Paleoclimate-induced stress on polar forested ecosystems prior to
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
The Permian–Triassic boundary section at Baghuk Mountain
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
Sedimentary factories and ecosystem change across the Permian
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