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A restudy of Oryctocephalus indicus (Reed,1910)
作者单位:1. College of Resource and Environment of Guizhou University,Guiyang 550003,China; 2. Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing 210008,China; 3. State Key Laboratory of Papaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology,Nanjing 210008,China; 4. Department of Geological Science,Ohio State University,Columbus,OH 43210,USA; 5. Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China
摘    要:Since both Chinese1]and American Palaeontolo-gists2]proposed separately to mark the beginning ofthe Middle Cambrian based on the first appearancedatum (FAD) ofOryctocephalus indicus3]in thesame year ,the suggestion has been considered seri-ously and adoptedfrequently4—18].The InternationalSubcommission on Cambrian Stratigraphy (ISCS) hasorganized the Working Group,chaired by L.B. Mc-Collum,to select candidate sections that bear poten-tial to become a GSSPfor the traditional Lowe…


A restudy of Oryctocephalus indicus (Reed, 1910)
Authors:ZHAO Yuanlong  YUAN Jinliang  PENG Shanchi  YANG Xinglian  PENG Jin  LIN Jihpai  GUO Qingjun
Abstract:Restudy on morphology of Oryctocephalus indicus (Reed, 1910), based on specimens from Guizhou, China and Nevada USA, suggests that the subspecies regarded previously as Oryctocephalus indicus indicus (Reed, 1910), O. indicus latus Zhao et Yuan 2002, and O. indicus kobayashi Saito, 1934, are synonymous, and Oryctocephalus americanus Sundberg et McCollum, 2003 is a similar form of O. indicus. Oryctocephalus indicus is rediagnosed as having a glabella that is subconical in outline and tapering forward slightly; a thorax that comprises 12 segments, and a small pygidium that bears 2-3 axial rings with a terminal piece and a postaxial ridge.Oryctocephalus indicus is widely distributed in eastern Guizhou and ranges through a great interval of Kaili Formation. Its first appearance is almost identical with these events of trilobite extinction-recovery occurring at the end of the Early Cambrian, the alternation of acritach assemblages, the change of trace elements (REE) and stable isotopes (carbon) at the Wuliu-Zengjiaya section. As one of the key forms for defining the traditional Lower - Middle Cambrian boundary (the base of Cambrian Series 3 and Stage 5 in the new Cambrian chronstratigraphic standard), O. indicus has received detailed study and has more advantages than other species such as Ovatoryctocara granulata Tchernysheva, 1962 or Arthricocephalus chauveaui Bergeron, 1899.
Keywords:Oryctocephalus indicus  restudy  Kaili Formation  Cambrian  Guizhou  China
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