J4

• 基础地质·矿床·盆地 •    下一篇

西藏申扎地区奥陶纪鹦鹉螺化石

程立人1,张予杰2,张以春1   

  1. 1.吉林大学 地球科学学院,吉林 长春 130061;2.成都地质矿产研究所,四川 成都 610082
  • 收稿日期:2004-06-05 修回日期:1900-01-01 出版日期:2005-05-26 发布日期:2005-05-26
  • 通讯作者: 程立人

Ordovician Nautiloid Fossils of Xainza Region,Tibet

CHENG Li-ren1, ZHANG Yu-jie2, ZHANG Yi-chun1   

  1. 1.College of Earth Sciences, Jilin University, Changchun 130061, China; 2. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China
  • Received:2004-06-05 Revised:1900-01-01 Online:2005-05-26 Published:2005-05-26
  • Contact: CHENG Li-ren

摘要: 申扎地区塔尔玛桥东-扎扛一带的奥陶系是藏北地区有可靠古生物化石依据的第二个出露区。地层发育好,含化石门类多,数量大,时代依据可靠,界线清楚,是藏北地区目前已知研究奥陶系(纪)的最理想地区。经鉴定,该区鹦鹉螺化石有29种,10未定种,分别隶属3目8科15属,其中3新属9新种。这为该区奥陶纪地层划分、对比及研究古地理格局,探讨藏北地质构造演化提供了重要资料。文中仅描述了1新属6新种,老属种描述从略。

关键词: 西藏, 申扎地区, 奥陶纪, 鹦鹉螺

Abstract: The Taerma bridge-Zhakang in the Xainza area is the second spot of Ordovician in northern Tibet based on the discovery of some reliable fossils. The strata contain a large amount of fossils of many taxa, which developed well enough to attain reliable support for era and distinctive boundary. It is the best spot for the fossil study of the Ordovician in the northern Tibet up to now and provides important clues to the classification and correlation of the Ordovician and to the paleogeography distribution as well as to the tectonic evolution of the northern Tibet. 29 species of Nautiloid fossils, which belong to 3 orders, 8 families and 15 genera, have been identified. Among them,3 genera and 9 species are new. Here only one new genus Eneoceras gen. nov. and six new species are described in detail as example. Other two new genera Taremaoceras and Variabioceras will be described in other papers.Genus Eneoceras gen.nov.Diagnosis:The new genus Eneoceras gen. nov. is characterized by the features as “Conch orthoconic, medium in size. The surface is decorated with annulus which array in a distance as the septa. Conch enlarging slowly. Compressed laterally. Circular in cross section. Siphuncle small, situated central from ventral in position. Spetal neck subcyrtochoanitic. Slightly expanded in connecting rings. Siphuncle appears as a string of beads with thin parietal deposits in it. Medium in spetal density. Thin epithecal and hypothecal deposits developed in cameras.”

Key words: Tibet, Xainza region, Ordovician, Nautiloid

中图分类号: 

  • P534.42
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