首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Cambrian trilobite Ovatoryctocara granulata Tchernysheva, 1962 and its biostratigraphic significance
Authors:Jinliang Yuan  Yuanlong Zhao  Jin Peng  Xuejian Zhu  Jih-pai Lin
Institution:a) Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China; b) College of Resource and Environment Science, Guizhou University, Guiyang 550003,China; c) School of Earth Sciences, Ohio State University, Columbus, OH 43210, USA
Abstract:The genus Ovatoryctocara Tchernysheva, 1962 and its key species Ovatoryctocara granulata Tchernysheva, 1962 are revised. Ovatoryctocara granulata occurs near the base of the Ovatoryctocara Zone and ranges up into the lower portion of the Kounamkites Zone in the Siberian Platform. O. granulata also appears in southeastern Guizhou, South China, but, O. granulata in northern Greenland may represent an indefinite species. Specimens of Ovatoryctocara from Newfoundland cannot be identified to species level. Specimens including two cranidia and three pygidia from the lower part of the Aoxi Formation at Yaxi Village, Shizhu Town, eastern Tongren, northeastern Guizhou, were previously assigned to O. granulata , which is now reassigned as a new species O. yaxiensis sp. nov. It bears following main features: glabella club-shaped, slightly expanded medially, with 4 pairs of lateral furrows, of which S1-S3 triangular pits, S4 shallow , connecting with axial furrow; shorter palpebral lobe situated a little anterior to midway of facial suture across the fixigenae, longer posterolateral area (exsag.); semielliptical pygidium consisting of seven axial rings with a terminal piece and with eight pairs of marginal tips giving a sawtooth-like shape of the lateral margins in dorsal view. Although O. granulata is a widely distributed species, the FAD of O. granulata, for a global stage boundary has still some disadvantages. First, its distribution is not as wide as that of Oryctocephalus indicus (Reed, 1910). Second, specimens of O. granulata are only common in Siberia. Third, the stratigraphic range of the species has not been studied in detail in all continents. Fourth, O. granulata is relatively small and easily affected by post-burial distortion. Last but not least, there exists obviously a facies change between the Ovatoryctocara Zone ( lower Amgan Stage; deeper water facies) and underlying Anabaraspis splendens Zone (Toyonian Stage; shallow water facies) in Siberian Platform. Nevertheless, the stratigraphic correlation utility of O. granulata in South China and Siberia is discussed.
Keywords:Trilobites  Ovatoryctocara granulata Tchernysheva  1962  Cambrian  Biostratigraphy
本文献已被 维普 万方数据 ScienceDirect 等数据库收录!
点击此处可从《自然科学进展(英文版)》浏览原始摘要信息
点击此处可从《自然科学进展(英文版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号