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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 30 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
Sedimentary factories and ecosystem change across the Permian
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
Minerals, Free Full-Text
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
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
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
Summary of Early Triassic carbon isotope records - ScienceDirect
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
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