Foth Christian, Ezcurra Martín D, Sookias Roland B, Brusatte Stephen L, Butler Richard J
Department of Geosciences, University of Fribourg/Freiburg, Fribourg, Switzerland.
SNSB, Bayerische Staatssammlung für Paläontologie und Geologie, München, Germany.
BMC Evol Biol. 2016 Sep 15;16:188. doi: 10.1186/s12862-016-0761-6.
Archosauromorpha originated in the middle-late Permian, radiated during the Triassic, and gave rise to the crown group Archosauria, a highly successful clade of reptiles in terrestrial ecosystems over the last 250 million years. However, scientific attention has mainly focused on the diversification of archosaurs, while their stem lineage (i.e. non-archosaurian archosauromorphs) has often been overlooked in discussions of the evolutionary success of Archosauria. Here, we analyse the cranial disparity of late Permian to Early Jurassic archosauromorphs and make comparisons between non-archosaurian archosauromorphs and archosaurs (including Pseudosuchia and Ornithodira) on the basis of two-dimensional geometric morphometrics.
Our analysis recovers previously unappreciated high morphological disparity for non-archosaurian archosauromorphs, especially during the Middle Triassic, which abruptly declined during the early Late Triassic (Carnian). By contrast, cranial disparity of archosaurs increased from the Middle Triassic into the Late Triassic, declined during the end-Triassic extinction, but re-expanded towards the end of the Early Jurassic.
Our study indicates that non-archosaurian archosauromorphs were highly diverse components of terrestrial ecosystems prior to the major radiation of archosaurs, including dinosaurs, while disparity patterns of the Ladinian and Carnian indicate a gradual faunal replacement of stem archosaurs by the crown group, including a short interval of partial overlap in morphospace during the Ladinian.
主龙形下纲起源于二叠纪中晚期,在三叠纪辐射演化,并产生了冠群主龙类,这是在过去2.5亿年陆地生态系统中非常成功的爬行动物类群。然而,科学关注主要集中在主龙类的多样化上,而在关于主龙类进化成功的讨论中,它们的干群谱系(即非主龙类主龙形下纲)常常被忽视。在此,我们基于二维几何形态测量学分析了晚二叠世至早侏罗世主龙形下纲的颅骨差异,并对非主龙类主龙形下纲和主龙类(包括伪鳄类和鸟颈类)进行了比较。
我们的分析发现非主龙类主龙形下纲具有此前未被认识到的高形态差异,尤其是在中三叠世,这种差异在晚三叠世早期(卡尼期)突然下降。相比之下,主龙类的颅骨差异从中三叠世到晚三叠世增加,在三叠纪末大灭绝期间下降,但在早侏罗世末期重新扩大。
我们的研究表明,在包括恐龙在内的主龙类主要辐射演化之前,非主龙类主龙形下纲是陆地生态系统中高度多样化的组成部分,而拉丁期和卡尼期的差异模式表明干群主龙类逐渐被冠群取代,包括在拉丁期形态空间中有一段短暂的部分重叠期。