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朝鲜南部的Pseudogl yptagnostus(三叶虫)并论朝鲜寒武纪斜坡相的意义
引用本文:张文堂. 朝鲜南部的Pseudogl yptagnostus(三叶虫)并论朝鲜寒武纪斜坡相的意义[J]. 古生物学报, 2000, 39(1): 92-99
作者姓名:张文堂
作者单位:中国科学院南京地质古生物研究所南京 210008
摘    要:朝鲜南部Machari组Olenoides带的Agnostus(Ptychagnostus?)orientalis Kobayasbhi一种应归于Agnos-totes(Pseudoglyptagnostus)Lu,1964一属,时代是晚寒武世长山期,不是早期中寒琥世,小林贞一的Olenoides带是中及晚寒武三叶虫混杂在一起的一个化石带。他建立的该组5个化石带也有问题。Coreolenus,Ch

关 键 词:三叶虫 朝鲜寒武纪 斜坡相 扬子地台 中朝地台
修稿时间:1999-07-01

OCCURRENCE OF PSEUDOGLYPTAGNOSTUS (CAMBRIAN TRILOBITA) IN SOUTH KOREA AND THE SIGNIFICANCE OF THE SLOPE BIOFACIES OF KOREA
ZHANG Wen-Tang. OCCURRENCE OF PSEUDOGLYPTAGNOSTUS (CAMBRIAN TRILOBITA) IN SOUTH KOREA AND THE SIGNIFICANCE OF THE SLOPE BIOFACIES OF KOREA[J]. Acta Palaeontologica Sinica, 2000, 39(1): 92-99
Authors:ZHANG Wen-Tang
Abstract:Agnostus (Ptychagnostus?) orientalis Kobayashi, 1935 from the Olenoides Zone of the Machari Formation of South Korea, is a species of Agnostotes (Pseudoglyptagnostus) Lu, 1964, which is an agnostoid trilobite of medial Late Cambrian age rather than early Middle Cambrian. Kobayashi used the Olenoides to denominate a mixed zone of trilobites of Middle and Late Cambrian ages, and his 5 biozonations for the Machari Formation are incorrect. The occurrence of Core olenus , Cheiruroides , Oryctocephalus , Pagetia , Tonkinella , Glyptagnostus, Pseudoglyptagnostus and Hedinaspis of Early to Late Cambrian age in Chunghwa, North Korea and in Neietsu and Bunkei, South Korea, shows the presence of a slopebiofacies, which should be affiliated with the North China Platform, as the side facing the Pacific Ocean. This slope biofacies in Korea, was the northeast extension of the Chiangnan Belt of South China, where a continuous belt of slope biofacies with southwest-northeast direction, existed from North Vietnam, via southwest Guangxi, eastern Guizhou, western Hunan, northern Jianggxi, southern Anhui, western Zhejiang, southern Jiangsu (including Shanghai) to Korea. This belt is continuous without any serious geographical displacement. It clearly shows that the North China (or Sino-Korean) and Yangtze Platforms, or "Blocks” of some authors, have kept their northern and southern geographical positions as shown on the present geographical map, they probably belonged to one larger platformal area, and there is no separation of the North and South China Blocks during the Cambrian, as many authors have indicated in different reconstruction maps for Cambrian paleo geography (e. g., Lin, Fuller and Zhang, 1985; Zhao and Robert, 1987). Agnostus (Ptychagnostus?) orientalis Kobayashi and its associated species of Irvingella and Pseudagnostus, are redescribed and refigured. Komaspis Kobayashi, 1935 may be a junior synonym of Irvingella Ulrich and Resser, in Walcott, 1924. Komaspis and Eochuangia are of Late Cambrian Changshanian age rather than Middle Cambrian as suggested by Kobayashi in 1935.
Keywords:Korean Cambrian   slope litho and biofacies   Sino Korean and Yangtze Platforms   drift  
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