Late Permian (P.) to early Early Triassic (A) δ 13 C, (B) δ 238 U, and
Por um escritor misterioso
Descrição
Diachronous end-Permian terrestrial ecosystem collapse with its
Flat latitudinal diversity gradient caused by the Permian–Triassic
Marine anoxia and delayed Earth system recovery after the end
Minerals, Free Full-Text
Stratigraphic, glacio-eustatic, δ 238 U, δ 13 C carb , and δ 18 O
Permian-Triassic Boundary - an overview
Multiple S-isotopic evidence for episodic shoaling of anoxic water
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
Timing and Provenance of Volcanic Fluxes Around the Permian
Paleoclimate-induced stress on polar forested ecosystems prior to
Frontiers Carbon Isotope Chemostratigraphy Across the Permian
PDF) Marine anoxia and delayed Earth system recovery after the end
Collapse of Late Permian chert factories in the equatorial Tethys
Frontiers Evidence of a Continuous Continental Permian-Triassic
de
por adulto (o preço varia de acordo com o tamanho do grupo)