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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
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
Ecosystem changes through the Permian–Triassic and Triassic
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
Volcanic CO2 degassing postdates thermogenic carbon emission
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Transient ocean oxygenation at end-Permian mass extinction onset
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
Massive and rapid predominantly volcanic CO2 emission during the
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
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
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