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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 21 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
Geosciences, Free Full-Text
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
2 (a) Comparison of Triassic-Jurassic δ 13 C carb , δ 13 C TOC
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Mercury isotope evidence for marine photic zone euxinia across the
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Severest crisis overlooked—Worst disruption of terrestrial
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
Frontiers Volcanically-Induced Environmental and Floral Changes
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Age and pattern of the southern high-latitude continental end
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
Collapse of Late Permian chert factories in the equatorial Tethys
Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Frontiers Biotic Response to Rapid Environmental Changes During
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
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