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贵州兴义中三叠世黔鱼龙属(爬行纲: 鱼龙目)一新种
引用本文:杨鹏飞,季承,江大勇,Ryosuke Motani,Andrea Tintori,孙元林,孙作玉.贵州兴义中三叠世黔鱼龙属(爬行纲: 鱼龙目)一新种[J].北京大学学报(自然科学版),2013,49(6):1002.
作者姓名:杨鹏飞  季承  江大勇  Ryosuke Motani  Andrea Tintori  孙元林  孙作玉
作者单位:1. 造山带与地壳演化教育部重点实验室, 北京大学地球与空间科学学院, 北京 100871; 2. 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, 南京 210008; 3. Department of Geology, University of California, Davis, CA 95616-8605; 4. Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Mangiagalli 34-20133 Milano;
基金项目:国家自然科学基金;国家自然科学基金;国家自然科学基金;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)开放基金;高等学校博士学科点专项科研基金
摘    要:

关 键 词:黔鱼龙  鱼龙  中三叠世  兴义动物群  贵州  
收稿时间:2013-01-07

A New Species of Qianichthyosaurus (Reptilia: Ichthyosauria) from Xingyi Fauna (Ladinian,Middle Triassic) of Guizhou
YANG Pengfei,JI Cheng,JIANG Dayong,Ryosuke Motani,rea Tintori,SUN Yuanlin,SUN Zuoyu.A New Species of Qianichthyosaurus (Reptilia: Ichthyosauria) from Xingyi Fauna (Ladinian,Middle Triassic) of Guizhou[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2013,49(6):1002.
Authors:YANG Pengfei  JI Cheng  JIANG Dayong  Ryosuke Motani  rea Tintori  SUN Yuanlin  SUN Zuoyu
Institution:1. The Laboratory of Orogenic Belt and Crustal Evolution MOE, School of Earth and Space Sciences, Peking University, Beijing 100871;2. State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, CAS, Nanjing 210008; 3. Department of Geology, University of California, Davis, CA 95616-8605; 4. Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Mangiagalli 34-20133 Milano;
Abstract:A new species of Qianichthyosaurus Li, 1999 from the Zhuganpo Member of the Falang Formation (Ladinian, Middle Triassic), Wusha Town, Xingyi City of Guizhou is described here, namely Qianichthyosaurus xingyiensis sp. nov. The recognition of the new species revises the diagnosis of the genus: tooth size relative to the skull width slightly below 0.1; ulna peripheral “shaft” notched or largely reduced; hindlimb nearly equal or longer than forelimb; tibia peripheral “shaft” notched or largely reduced. Qianichthyosaurus xingyiensis sp. nov. differs from the type species in having relatively longer snout (snout length/skull length over 60%); humerus radial facet being prominently larger than ulnar facet; unenclosed obturator foramen on pubis; fibula posterior process on the posterior margin and the ischium sub-triangular lacking shaft. The new species is stratigraphically older than Q. zhoui, the specimens of which were exclusively known from the Wayao Member of the Falang Formation (Carnian, Late Triassic). Along with askeptosaurid thalattosaur Anshunsaurus and shastasaurid ichthyosaur Guizhouich- thyosaurus, the occurrence of Q. xingyiensis sp. nov. in Xingyi Fauna suggests a closer relationship between Xingyi Fauna (late Ladinian, Middle Triassic) and Guanling Biota (Carnian, Late Triassic).
Keywords:Qianichthyosaurus  Ichthyosaur  Middle Triassic  Xingyi Fauna  Guizhou  
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