School of Earth and Space Sciences, Peking University, Beijing, China.
State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS), Nanjing, China.
J Anat. 2021 Feb;238(2):219-248. doi: 10.1111/joa.13311. Epub 2020 Sep 22.
Hynobiidae are a clade of salamanders that diverged early within the crown radiation and that retain a considerable number of features plesiomorphic for the group. Their evolutionary history is informed by a fossil record that extends to the Middle Jurassic Bathonian time. Our understanding of the evolution within the total group of Hynobiidae has benefited considerably from recent discoveries of stem hynobiids but is constrained by inadequate anatomical knowledge of some extant forms. Pseudohynobius is a derived hynobiid clade consisting of five to seven extant species living endemic to southwestern China. Although this clade has been recognized for over 37 years, osteological details of these extant hynobiids remain elusive, which undoubtedly has contributed to taxonomic controversies over the hynobiid complex Liua-Protohynobius-Pseudohynobius. Here we provide a bone-by-bone study of the cranium in the five extant species of Pseudohynobius (Ps. flavomaculatus, Ps. guizhouensis, Ps. jinfo, Ps. kuankuoshuiensis and Ps. shuichengensis) based on x-ray computer tomography data for 18 specimens. Our results indicate that the cranium in each of these species has a combination of differences in morphology, proportions and articulation patterns in both dermal and endochondral bones. Our study establishes a range of intraspecific differences that will serve as organizing hypotheses for future studies as more extensive collections of these species become available. Morphological features in the cranium for terrestrial ecological adaptation in Hynobiidae are summarized. Based on the results, we also discuss the evolution and development of several potential synapomorphies of Hynobiidae, including features of the orbitosphenoid and articular.
无尾目是一类早期分化的蝾螈,保留了大量的基干特征。它们的进化历史可以通过从中侏罗世巴通期延伸而来的化石记录来了解。我们对无尾目总科内部的进化的理解得益于最近对原始无尾目物种的发现,但由于对一些现存形式的解剖学知识不足,受到了限制。拟小鲵属是一个衍生的小鲵科,由五种到七种现存的物种组成,生活在中国西南部的特有种。尽管这个科已经被认识了 37 年以上,但这些现存小鲵的骨骼细节仍然难以捉摸,这无疑导致了对小鲵属 Liua-Protohynobius-Pseudohynobius 这一复杂分类群的分类争议。在这里,我们根据 18 个标本的 X 射线计算机断层扫描数据,对五种现存的拟小鲵属物种(Ps. flavomaculatus、Ps. guizhouensis、Ps. jinfo、Ps. kuankuoshuiensis 和 Ps. shuichengensis)的颅骨进行了逐一研究。我们的结果表明,这些物种的每一种颅骨都具有形态、比例和真皮和软骨内骨骼的关节模式的差异组合。我们的研究确定了一系列种内差异,这些差异将为未来的研究提供组织假说,随着对这些物种更广泛的收集,未来的研究将更加广泛。总结了无尾目在陆栖生态适应方面的颅骨形态特征。基于这些结果,我们还讨论了几个无尾目潜在的共衍征的进化和发育,包括眶蝶骨和关节的特征。