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云南曲靖下泥盆统洛霍考夫阶花鳞鱼类新材料

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  • 1 中国科学院古脊椎动物与古人类研究所,中国科学院脊椎动物演化与人类起源重点实验室 北京 100044
    2 中国科学院生物演化与环境卓越创新中心 北京 100044
    3 中国科学院大学 北京 100049
    4 曲靖师范学院自然历史文化研究中心 云南曲靖 655000

收稿日期: 2019-04-25

  网络出版日期: 2020-01-20

基金资助

国家自然科学基金(41530102);国家自然科学基金(41672006);中国科学院战略性先导科技专项(XDA19050102);中国科学院战略性先导科技专项(XDB26010401);中国科学院前沿科学重点研究计划(QYZDJ-SSW-DQC002);现代古生物学和地层学国家重点实验室(中国科学院南京地质古生物研究所)(193121);中国科学院古生物化石发掘与修理专项经费资助

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《古脊椎动物学报》编辑部, 2020, 版权所有,未经授权,不得转载、摘编本刊文章,不得使用本刊的版式设计。

New material of thelodonts from Lochkovian (Lower Devonian) of Qujing, Yunnan, China

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  • 1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044
    2 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044
    3 University of Chinese Academy of Sciences Beijing 100049
    4 Research Center of Natural History and Culture, Qujing Normal University Yunnan 655000

Received date: 2019-04-25

  Online published: 2020-01-20

Copyright

, 2020, Copyright reserved © 2020.

摘要

采用高精度计算机断层扫描和三维重建技术,获取了大量来自云南下泥盆统洛霍考夫阶西屯组和西山村组下部花鳞鱼鳞片的三维重建模型。描述了花鳞鱼类的一个已知属——副花鳞鱼属(Parathelodus)的共7个种,三裂副花鳞鱼(P. trilobatus)、亚洲副花鳞鱼(P. asiaticus)、角状副花鳞鱼(P. cornuformis)、雅致副花鳞鱼(P. scitulus)、西屯副花鳞鱼(新种) (P. xitunensis sp. nov.)、王氏副花鳞鱼(新种) (P. wangi sp. nov.)和寥廓副花鳞鱼(新种) (P. liaokuoensis sp. nov.)。新材料的发现将副花鳞鱼的地层分布从洛霍考夫阶西屯组至西山村组上部延伸到西山村组下部,最低层位已非常靠近志留系与泥盆系的界线。西屯副花鳞鱼、王氏副花鳞鱼和廖廓副花鳞鱼3个新种的发现提高了我们对中国早泥盆世花鳞鱼类多样性的认识。

本文引用格式

崔心东, 李强, 乔妥, 朱敏 . 云南曲靖下泥盆统洛霍考夫阶花鳞鱼类新材料[J]. 古脊椎动物学报, 2020 , 58(1) : 1 -15 . DOI: 10.19615/j.cnki.1000-3118.190612

Abstract

We reconstructed a wealth of three-dimensional virtual models of vertebrate micro-remains from the Xitun Formation and lower part of the Xishancun Formation (Lochkovian, Lower Devonian) of Qujing, Yunnan by means of high-resolution computed tomography. One genus (Parathelodus) and seven species (P. trilobatus, P. asiaticus, P. cornuformis, P. scitulus, P. xitunensis sp. nov., P. wangi sp. nov. and P. liaokuoensis sp. nov.) of thelodonts are described. The new discovery extends the stratigraphic distribution of Parathelodus from the Xitun Formation and the upper part of the Xishancun Formation to the lower part of the Xishancun Formation, the horizon close to the Silurian-Devonian boundary. The three new species, P. xitunensis, P. wangi and P. liaokuoensis, enhance our knowledge of the thelodont diversity from the Early Devonian of China.

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