Revision of the conodont Erraticodon hexianensis from the upper Meitan Formation (Middle Ordovician) of Guizhou, South China

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概要

• 論文の詳細を見る

• Erraticodon hexianensis, a conodont with an octomembrate species apparatus, is described and illustrated from the upper part of the Meitan Formation in Guizhou, South China. Cooccurrence of Erraticodon hexianensis and Lenodus variabilis at the top of the Meitan Formation in the Honghuayuan Section of Tongzi suggests an early Darriwilian age for this level. Recovery of Oepikodus communis from the base of the Meitan Formation in the Ganxi Section of Yanhe indicates a correlation with the communis Zone of the Early Ordovician.

• 日本古生物学会の論文
• 2007-06-30

著者

• Liu Jianbo

  State Key Lab. Palaeobiology And Stratigraphy Chinese Acad. Sci. Nanjing Chn

• Liu Jianbo

  Department Of Geology Peking University

• ZHEN YONG

  Palaeontology Section, The Australian Museum

• PERCIVAL IAN

  Geological Survey of New South Wales, NSW Department of Primary Industries, State Geoscience Centre

• Percival Ian

  Geological Survey Of New South Wales Nsw Department Of Primary Industries State Geoscience Centre

• Zhen Yong

  Palaeontology Section The Australian Museum

関連論文

• Revision of the conodont Erraticodon hexianensis from the upper Meitan Formation (Middle Ordovician) of Guizhou, South China
• Sedimentary Evolution of the Ordovician Basin in Central Ningxia, North China
• Marine sedimentary response to the Great Ordovician Biodiversification Event : Examples from North China and South China
• Sea-level control of Gravity-flow deposits in the Middle Ordovician in Pingliang, north China

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