Department of Biomedical Sciences, Heritage College of Osteopathic Medicine, Ohio University, Athens, Ohio, United States of America.
Center for Ecology and Evolutionary Studies, Ohio University, Athens, Ohio, United States of America.
PLoS One. 2017 Oct 11;12(10):e0185301. doi: 10.1371/journal.pone.0185301. eCollection 2017.
Throughout the Paleogene, most terrestrial carnivore niches in Afro-Arabia were occupied by Hyaenodonta, an extinct lineage of placental mammals. By the end of the Miocene, terrestrial carnivore niches had shifted to members of Carnivora, a clade with Eurasian origins. The transition from a hyaenodont-carnivore fauna to a carnivoran-carnivore fauna coincides with other ecological changes in Afro-Arabia as tectonic conditions in the African Rift System altered climatic conditions and facilitated faunal exchange with Eurasia. Fossil bearing deposits in the Nsungwe Formation in southwestern Tanzania are precisely dated to ~25.2 Ma (late Oligocene), preserving a late Paleogene Afro-Arabian fauna on the brink of environmental transition, including the earliest fossil evidence of the split between Old World monkeys and apes. Here we describe a new hyaenodont from the Nsungwe Formation, Pakakali rukwaensis gen. et sp. nov., a bobcat-sized taxon known from a portion of the maxilla that preserves a deciduous third premolar and alveoli of dP4 and M1. The crown of dP3 bears an elongate parastyle and metastyle and a small, blade-like metacone. Based on alveolar morphology, the two more distal teeth successively increased in size and had relatively large protocones. Using a hyaenodont character-taxon matrix that includes deciduous dental characters, Bayesian phylogenetic methods resolve Pakakali within the clade Hyainailouroidea. A Bayesian biogeographic analysis of phylogenetic results resolve the Pakakali clade as Afro-Arabian in origin, demonstrating that this small carnivorous mammal was part of an endemic Afro-Arabian lineage that persisted into the Miocene. Notably, Pakakali is in the size range of carnivoran forms that arrived and began to diversify in the region by the early Miocene. The description of Pakakali is important for exploring hyaenodont ontogeny and potential influences of Afro-Arabian tectonic events upon mammalian evolution, providing a deep time perspective on the stability of terrestrial carnivore niches through time.
在整个古近纪时期,非洲-阿拉伯地区的大多数陆地食肉动物生态位都被已灭绝的胎盘哺乳动物——鬣齿兽占据。到中新世末期,陆地食肉动物的生态位已经转移到了食肉目动物身上,而食肉目动物起源于欧亚大陆。从鬣齿兽-食肉动物动物群向食肉目-食肉动物动物群的转变与非洲-阿拉伯地区的其他生态变化同时发生,因为非洲裂谷系统的构造条件改变了气候条件,并促进了与欧亚大陆的动物群交流。坦桑尼亚西南部 Nsungwe 组的含化石沉积物被精确地定年为~2520 万年(晚渐新世),保存了一个处于环境过渡边缘的晚古近纪非洲-阿拉伯动物群,其中包括旧世界猴和猿类分支的最早化石证据。在这里,我们描述了来自 Nsungwe 组的一种新的鬣齿兽,Pakakali rukwaensis gen. et sp. nov.,这是一种体型与山猫相当的分类单元,已知的部分上颌骨保存了一颗脱落的第三前臼齿和 dP4 和 M1 的牙槽。dP3 的牙冠具有长的原尖和后尖以及一个小的、叶片状的次尖。根据牙槽形态,后两个更靠后的牙齿逐渐增大,具有相对较大的原尖。使用包含脱落牙齿特征的鬣齿兽特征-分类单元矩阵,贝叶斯系统发育方法将 Pakakali 归入 Hyainailouroidea 分支中。对系统发育结果的贝叶斯生物地理分析将 Pakakali 分支解析为起源于非洲-阿拉伯地区,表明这种小型食肉哺乳动物是一种特有的非洲-阿拉伯谱系的一部分,该谱系一直持续到中新世。值得注意的是,Pakakali 的体型范围与早中新世到达并开始在该地区多样化的食肉目动物相似。Pakakali 的描述对于探索鬣齿兽的个体发育以及非洲-阿拉伯构造事件对哺乳动物进化的潜在影响具有重要意义,为陆地食肉动物生态位的稳定性提供了一个深入的时间视角。