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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 29 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
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
Volcanic CO2 degassing postdates thermogenic carbon emission
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
Present-day and late Permian location of the investigated
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
Marine anoxia linked to abrupt global warming during Earth's
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 δ 13 C carb , δ 18 O apatite and 87 Sr/ 86 Sr ratio
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Paleogeographic map during the Permian‐Triassic (P‐Tr) transition
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