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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
Permian–Triassic extinction event - Wikipedia
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
Summary of Early Triassic carbon isotope records - ScienceDirect
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
Size variations in foraminifers from the early Permian to the Late
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
Permian-Triassic Boundary - an overview
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Timing and Provenance of Volcanic Fluxes Around the Permian
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
Paired δ 238 U and δ 13 C data from carbonate slope successions
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