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

Journal of Asian Earth Sciences

Volumn 36, Issue 6, 2009, Pages 442-458

  Chen, Jun ^a,b   Beatty, Tyler W ^b   Henderson, Charles M ^b   Rowe, Harry ^c  

^a NANJING INSTITUTE OF GEOLOGY AND PALAEONTOLOGY   (China)

^b UNIVERSITY OF CALGARY   (Canada)

^c UNIVERSITY OF KENTUCKY   (United States)

Author keywords

Conodonts; Dawen section; Great Bank of Guizhou; Late Permian extinction; Permian Triassic boundary; South China

Indexed keywords

BIOSTRATIGRAPHY; CONODONT; MASS EXTINCTION; MORPHOMETRY; PERMIAN-TRIASSIC BOUNDARY; TAXONOMY;

ASIA; CHINA; EURASIA; FAR EAST; GUIZHOU; MEISHAN; ZHEJIANG;

CLARKINA; HINDEODUS; HINDEODUS PARVUS; HINDEODUS PRAEPARVUS; HINDEODUS TYPICALIS; ISARCICELLA STAESCHEI;

EID: 69249212333     PISSN: 13679120     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jseaes.2008.08.002     Document Type: Article

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