首页> 外文期刊>American Museum Novitates >Dyrosaurid (Crocodyliformes: Mesoeucrocodylia) Fossils from the Upper Cretaceous and Paleogene of Mali: Implications for Phylogeny and Survivorship across the K/T Boundary
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Dyrosaurid (Crocodyliformes: Mesoeucrocodylia) Fossils from the Upper Cretaceous and Paleogene of Mali: Implications for Phylogeny and Survivorship across the K/T Boundary

机译:上白垩统和马里古近纪的Dyrosaurid(鳄形目:Mesoeucrocodylia)化石:对跨越K / T边界的系统发育和生存的影响

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We describe new dyrosaurid fossils from three localities in Mali, representing strata of Maastrichtain, Paleocene. and Eocene ages. The fossils significantly extend the temporal and geographic ranges of several known dyrosaurid taxa. Rhabdognathus keiniensis and Chenanisuchus lateroculi are identified for the first time from Maastrichtian sediments. Additional material is referred to Phosphatosaurus gavialoides and, tentatively, the genus Sokotosuchus. These discoveries represent the First occurrence of Chenanisuchus and possibly of Sokotosuchus from Mali. Previously unknown morphological character states are incorporated into existing data matrices, reducing the amount of missing data. Phylogenetic analyses largely corroborate prior hypotheses of dyrosaurid relationships, but indicate a need for new characters to resolve the relationships of certain genera and species. The occurrence of both basal (e.g., Chenanisuchus lateroculi) and highly nested (e.g., Rhabdognathus keiniensis) members of Dyrosauridae on both sides of the K/T boundary indicates that dyrosaurid diversification was well underway by the latest Cretaceous, and that most, if not all dyrosaurid species survived the extinction event. The geology of the Mali's Tilemsi Valley is clarified; some rocks previously assigned to the Iullemmeden Basin actually represent extensions of other basins: the Taoudeni Basin and Gao Trench.
机译:我们描述了来自马里三个地区的新的dyrosaurid化石,它们代表了古新世马斯特里赫丹地层。和始新世时代。这些化石显着地扩展了几种已知的dyrosaurid类群的时间和地理范围。首次从马斯特里赫特沉积物中鉴定出了Rhabdognathus keiniensis和Cheanisuchus Lateroculi。额外的材料被称为磷鳞茎过磷酸杆菌,以及暂定为Sokotosuchus属。这些发现代表了马里最早出现的Chenanisuchus,可能还有Sokotosuchus。以前未知的形态特征状态被合并到现有的数据矩阵中,从而减少了丢失的数据量。系统发育分析很大程度上证实了dyrosaurid关系的先前假设,但表明需要新的特征来解决某些属和种之间的关系。在K / T边界的两侧都存在着Dyrosauridae的基底(例如,Chenanisuchus Lateroculi)和高度嵌套的(例如,Rhabdognathus keiniensis)成员,这表明,dyrosaurid的多样化在最近的白垩纪时期就已经进行得很好,并且大多数(如果没有的话)所有dyrosaurid物种都幸免于难。马里的Tilemsi山谷的地质情况已经阐明;先前分配给Iullemmeden盆地的一些岩石实际上代表了其他盆地的延伸:陶德尼盆地和高沟。

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