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Marine Upper Carboniferous and Lower Permian sediments are widely distributed in Panxian, weining and Shuicheng of western Guizhou. They are extensively exposed in simple structures and are represented by several hundreds-of-metres thick rocks, most of which are limestones containing abundant fusulinid foraminifers. The rock succession is normal. In panxian section, the fusulinids are associated with conodonts and ammonoids. The fusulinids described and illustrated comprise 357 species and subspecies belonging to 35 genera, of which 21 species are new forms.
SELECTED CONTENTS
  Order Fusulinida Fursenko, 1958
  Superfamily fusulinacea Moeller, 1878
  Ozawainellidae Thompson et Foster, 1937
  Family Schubertellidae Skinner, 1931
  Family Fusulinidae moeller, 1878
  Family Schwagerinidae Dunbar et Henbest, 1930
  Family(?) Staffellidae M.-Maclay, 1949

 

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