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首页> 外文期刊>Acta geologica Sinica: Journal of the Geological Society of China >Taxonomy and Stratigraphy of Late Mesozoic Anurans and Urodeles from China
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Taxonomy and Stratigraphy of Late Mesozoic Anurans and Urodeles from China

机译:中国晚中生代无脊椎动物和乌头类的分类学和地层学

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摘要

Three anurans (Callobatrachus sanyanensis, Liaobatrachus grabaui, Mesophryne beipiaoensis) and six urodeles (Laccotriton subsolanus, Liaoxitriton zhongjiani, Jeholotriton paradoxus, Sinerpeton fengshanensis, Chunerpeton tianyiensis, Liaoxitriton daohugouensis) are reported from the late Mesozoic tuff-interbedded lacustrine deposits (mostly of the Jehol Group) in northeastern China. They document the first discovery of Chinese Mesozoic lissamphibians, and their old geological age, superb preservation condition, and large taxonomic diversity are unique compared with other findings worldwide. The anurans occupy a higher evolutionary position than typical Jurassic taxa, supporting a post-Late Jurassic age of the fossil horizons. The urodeles all have unicapitate ribs, suggesting an evolutionary grade at the cryptobranchoid level, and are advanced in osteological features over non-urodeles from the Middle and Upper Jurassic in England and Central Asia. Some urodeles (Jeholotriton and Chunerpeton) exhibit neotenic features, representing the earliest occurrence among such findings. Six fossil horizons are recognized for the known Chinese Mesozoic anurans and urodeles: the Daohugou fossil bed, the Dabeigou Formation, the Lujiatun Bed, Jianshangou Bed and Dawangzhangzi Bed of the Yixian Formation, and the Jiufotang Formation. As implied from the osteological and phylogenetical studies, the geological age of these anurans and urodeles is the Early Cretaceous.
机译:三种无头an(三叶Call 、,皮,、中phr北ip)和六个小de(黑毛豆,辽西tri子,剑tri,Je蛇,凤山Si,田中Chun竹,河床中Me鱼)集团)在中国东北。他们记录了中国中生代两栖类的首次发现,与世界其他发现相比,它们的地质年龄,优良的保存条件和巨大的分类学多样性是独特的。与典型的侏罗纪分类单元相比,无脊椎动物的进化位置更高,这支持了化石层位的后侏罗纪时代。这些小尾虫均具有单腔肋骨,表明在隐分支支配体水平上具有进化等级,并且在骨学特征方面比英格兰和中亚的侏罗纪中上侏罗统的非小尾虫更为先进。某些乌头类动物(Jeholotriton和Chunerpeton)表现出新手性特征,代表这些发现中最早出现的特征。已知的中国中生代无氧铀和尾甲类动物有六个化石层位:稻县沟化石床,大北沟组,陆家屯床,Jian县组的剑山沟床和大王丈子床以及九佛堂组。从骨学和系统发育学研究中可以看出,这些无核动物和尾乌德雷德的地质年龄是早白垩世。

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