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Conodont biostratigraphy across the Permian–Triassic boundary at the Dawen section, Great Bank of Guizhou, Guizhou Province, South China: Implications for the Late Permian extinction and correlation with Meishan

Late Permian ExtinctionPermian–triassic BoundaryEast Asian StudiesTectonic EvolutionConodont BiostratigraphyEast Asian LanguagesBiostratigraphyLanguage StudiesGeochronology