Q915
MA Xueping1,Paul COPPER2,SUN Yuanlin1 and LIAO Weihua3 1 The Key Laboratory of Orogenic Belts and Crustal Evolution,Department of Geology,Peking University,Beijing 100871,China, E-mail: maxp@pku.edu.cn 2 Department of Earth Sciences,Laurentian University,Sudbury,Canada P3E 2C6 3 Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing,Jiangsu 210008,China
1 Introduction Southern Guizhou, especially the Dushan area, has been one of the most important areas for the study of the Devonian in South China, for example, Hou and Xian’s (1975) study of the Eifelian brachiopod fauna. The Upper Devonian in the Dushan section is mainly composed of carbonate rocks, with rare siliciclastics. Abundant benthic fossils (corals and brachiopods) have been found in these Frasnian strata (Liao et al., 1979). The Frasnian corals were described by Liao (1977)…
1 Introduction Southern Guizhou, especially the Dushan area, has been one of the most important areas for the study of the Devonian in South China, for example, Hou and Xian’s (1975) study of the Eifelian brachiopod fauna. The Upper Devonian in the Dushan section is mainly composed of carbonate rocks, with rare siliciclastics. Abundant benthic fossils (corals and brachiopods) have been found in these Frasnian strata (Liao et al., 1979). The Frasnian corals were described by Liao (1977)…
Paul COPPER.2005. Atrypid Brachiopods from the Upper Devonian Wangchengpo Formation (Frasnian) of southern Guizhou, China — Extinction Patterns in the Frasnian of South China[J]. ACTA GEOLOGICA SINICA(English edition),79(4):
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