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来自亚利桑那州晚三叠世的最早的赤道地区青蛙记录。

The earliest equatorial record of frogs from the Late Triassic of Arizona.

机构信息

1 Department of Geosciences, Virginia Tech , Blacksburg, VA 24061 , USA.

2 Petrified Forest National Park , 1 Park Road, Petrified Forest, AZ 86028 , USA.

出版信息

Biol Lett. 2019 Feb 28;15(2):20180922. doi: 10.1098/rsbl.2018.0922.

Abstract

Crown-group frogs (Anura) originated over 200 Ma according to molecular phylogenetic analyses, though only a few fossils from high latitudes chronicle the first approximately 60 Myr of frog evolution and distribution. We report fossils that represent both the first Late Triassic and the earliest equatorial record of Salientia, the group that includes stem and crown-frogs. These small fossils consist of complete and partial ilia with anteriorly directed, elongate and distally hollow iliac blades. These features of these ilia, including the lack of a prominent dorsal protuberance and a shaft that is much longer than the acetabular region, suggest a closer affinity to crown-group Anura than to Early Triassic stem anurans Triadobatrachus from Madagascar and Czatkobatrachus from Poland, both high-latitude records. The new fossils demonstrate that crown anurans may have been present in the Late Triassic equatorial region of Pangea. Furthermore, the presence of Early Jurassic anurans in the same stratigraphic sequence ( Prosalirus bitis from the Kayenta Formation) suggests that anurans survived the climatic aridification of this region in the early Mesozoic. These fossils highlight the importance of the targeted collection of microfossils and provide further evidence for the presence of crown-group representatives of terrestrial vertebrates prior to the end-Triassic extinction.

摘要

根据分子系统发育分析,冠群蛙类(无尾目)起源于 2 亿多年前,尽管只有少数来自高纬度地区的化石记录了青蛙进化和分布的最初约 6000 万年的历史。我们报告了一些化石,它们代表了晚三叠世最早的和赤道地区最早的有尾目,包括茎蛙和冠蛙。这些小化石由完整和部分的髂骨组成,髂骨的前部有向前延伸、拉长和远端中空的髂骨叶片。这些髂骨的特征,包括缺乏明显的背突和比髋臼区域长得多的轴,表明它们与冠群无尾目有更密切的亲缘关系,而不是来自马达加斯加的早三叠世茎蛙 Triadobatrachus 和来自波兰的 Czatkobatrachus,这两个都是高纬度地区的化石记录。新化石表明,冠群无尾目可能在晚三叠世泛古陆的赤道地区就已经存在。此外,同一地层序列中存在早侏罗世无尾目(来自凯岩组的 Prosalirus bitis)表明,无尾目在中生代早期该地区气候干旱化时期幸存了下来。这些化石强调了有针对性地采集微化石的重要性,并进一步证明了在晚三叠世灭绝之前,陆地脊椎动物的冠群代表就已经存在。

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