| 1 | A new section of Kaili Formation (Cambrian) and a biostratigraphic study of the boundary interval across the undefined Cambrian Series 2 and Series 3 at Jianshan,Jianhe County,China with a discussion of global correlation based on the first appearance dat显示文摘在 Jianshan 的 Kaili 形成的新节的三叶虫 biostratigraphic 研究, Chuandong 村庄, Jianhe 县,贵州被报导。与 Ovatoryctocara granulata Bathynotus holopygus 地区和原来在 Kaili 的 Wuliu-Zengjiayan 节从三叶虫集合被定义的 overlying Oryctocephalus indicus 地区联系的关键种类的另外的出现从这新节被报导。Oryctocephalus indicus 的第一本外观资料(一度时髦的风尚) 在单位的底上面发生在 44.52 m。基于丰富的标本的学习(n = 800 ) 从 Kaili 形成,我们主张那 Oryctocephalus indicus 是普遍的税在上与全球分布。O。reticulatus (Lermontova, 1940 ) 从在西伯利亚和 O 的 Molodo 河区域的 Amganian 阶段的 Kounamkites 地区的中间的部分。americanus (Sundberg 和 McCollum, 2003 ) 从内华达,北美洲类似于 O 的代表。发生在 O 的 indicus。Kaili 形成的 indicus 地区。O。reticulatus 和 O。americanus 这里与 O 被举出。indicus (里德, 1910 ) 。这研究为未命名的寒武纪的系列 3 的底为全球 Stratotype 作为候选人节加强 Kaili 形成的 Wuliu-Zengjiayan 节。 | Yuanlong Zhao Jinliang Yuan Shanchi Peng Loren E. Babcock Jin Peng Qingjun Guo Jihpai Lin Tongshu Tai Ruidong Yang Yuxian Wang | 2008 | Progress in Natural Science:Materials International2008，18，12： | 8 |
| 2 | A restudy of Oryctocephalus indicus (Reed,1910)显示文摘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. | ZHAO Yuanlong YUAN Jinlian PENG Shanchi YANG Xinglian PENG Jin LIN Jihpai GUO Qingjun | 2006 | Progress in Natural Science:Materials International2006，16，11： | 4 |
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