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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
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 extinction event - Wikipedia
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Depositional sequences in northern Peru: new insights on the
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
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
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
Volcanic CO2 degassing postdates thermogenic carbon emission
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
An enormous sulfur isotope excursion indicates marine anoxia
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
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
The Permian–Triassic boundary section at Baghuk Mountain, Central
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
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