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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 20 setembro 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
Sedimentary factories and ecosystem change across the Permian
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Frontiers Hg Isotopes and Enhanced Hg Concentration in the
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Full article: Lithogeochemical and sulfide trace-element
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
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
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
Frontiers Volcanically-Induced Environmental and Floral Changes
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
Volcanic CO2 degassing postdates thermogenic carbon emission
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
Ecosystem changes through the Permian–Triassic and Triassic
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
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