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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
A) The δ 238 U and (B) [U] boxplots. Whiskers denote the minimum
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
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
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
Flat latitudinal diversity gradient caused by the Permian–Triassic
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
Minerals, Free Full-Text
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Eccentricity and obliquity paced carbon cycling in the Early
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
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
PDF) Stepwise and large-magnitude negative shift in δ 13C carb
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
Minerals, Free Full-Text
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Stratigraphic, glacio-eustatic, δ 238 U, δ 13 C carb , and δ 18 O
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