Virginia Museum of Natural History, Martinsville, Virginia, USA.
Natural History Museum of Utah and Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah, USA.
Anat Rec (Hoboken). 2023 Aug;306(8):2102-2118. doi: 10.1002/ar.25160. Epub 2023 Feb 27.
The femora of diapsids have undergone morphological changes related to shifts in postural and locomotor modes, such as the transition from plesiomorphic amniote and diapsid taxa to the apomorphic conditions related to a more erect posture within Archosauriformes. One remarkable clade of Triassic diapsids is the chameleon-like Drepanosauromorpha. This group is known from numerous articulated but heavily compressed skeletons that have the potential to further inform early reptile femoral evolution. For the first time, we describe the three-dimensional osteology of the femora of Drepanosauromorpha, based on undistorted fossils from the Upper Triassic Chinle Formation and Dockum Group of North America. We identify apomorphies and a combination of character states that link these femora to those in crushed specimens of drepanosauromorphs and compare our sample with a range of amniote taxa. Several characteristics of drepanosauromorph femora, including a hemispherical proximal articular surface, prominent asymmetry in the proximodistal length of the tibial condyles, and a deep intercondylar sulcus, are plesiomorphies shared with early diapsids. The femora contrast with those of most diapsids in lacking a crest-like, distally tapering internal trochanter. They bear a ventrolaterally positioned tuberosity on the femoral shaft, resembling the fourth trochanter in Archosauriformes. The reduction of an internal trochanter parallels independent reductions in therapsids and archosauriforms. The presence of a ventrolaterally positioned trochanter is also similar to that of chameleonid squamates. Collectively, these features demonstrate a unique femoral morphology for drepanosauromorphs, and suggest an increased capacity for femoral adduction and protraction relative to most other Permo-Triassic diapsids.
晰脚类恐龙的股骨经历了与姿势和运动模式转变相关的形态变化,例如从原始的羊膜动物和晰脚类过渡到更直立姿势的主龙形类的特化条件。三叠纪晰脚类恐龙的一个显著分支是变色龙样的美颌龙类。该类群有大量完整但严重压缩的骨骼,这些骨骼有可能进一步揭示早期爬行动物股骨的演化情况。我们首次基于来自北美上三叠统钦迪组和多克组的未变形化石,描述了美颌龙类的股骨的三维骨骼结构。我们确定了这些股骨的特化特征和特征组合,将其与美颌龙类破碎标本的股骨联系起来,并将我们的样本与一系列羊膜动物类群进行了比较。美颌龙类股骨的几个特征,包括近端关节面呈半球形、胫骨髁的近-远侧长度明显不对称以及深的髁间沟,都是与早期双孔类共享的原始特征。与大多数双孔类恐龙的股骨不同,美颌龙类的股骨没有一个像喙突一样、远端逐渐变细的内转子。它们在股骨体上有一个位于腹外侧的结节,类似于主龙形类的第四转子。内转子的缺失与兽脚类和主龙形类的独立缺失相平行。腹外侧转子的存在也与变色龙科蜥蜴相似。这些特征共同表明了美颌龙类独特的股骨形态,表明它们相对于大多数其他二叠纪-三叠纪双孔类恐龙具有更大的股骨内收和前伸能力。