Department of Anthropology, University at Albany, Albany, New York, United States.
Museum für Naturkunde, Berlin, Germany.
PeerJ. 2022 Apr 6;10:e13210. doi: 10.7717/peerj.13210. eCollection 2022.
The Early Pleistocene was a critical time period in the evolution of eastern African mammal faunas, but fossil assemblages sampling this interval are poorly known from Ethiopia's Afar Depression. Field work by the Hadar Research Project in the Busidima Formation exposures (~2.7-0.8 Ma) of Hadar in the lower Awash Valley, resulted in the recovery of an early maxilla (A.L. 666-1) with associated stone tools and fauna from the Maka'amitalu basin in the 1990s. These assemblages are dated to ~2.35 Ma by the Bouroukie Tuff 3 (BKT-3). Continued work by the Hadar Research Project over the last two decades has greatly expanded the faunal collection. Here, we provide a comprehensive account of the Maka'amitalu large mammals (Artiodactyla, Carnivora, Perissodactyla, Primates, and Proboscidea) and discuss their paleoecological and biochronological significance. The size of the Maka'amitalu assemblage is small compared to those from the Hadar Formation (3.45-2.95 Ma) and Ledi-Geraru (2.8-2.6 Ma) but includes at least 20 taxa. Bovids, suids, and are common in terms of both species richness and abundance, whereas carnivorans, equids, and megaherbivores are rare. While the taxonomic composition of the Maka'amitalu fauna indicates significant species turnover from the Hadar Formation and Ledi-Geraru deposits, turnover seems to have occurred at a constant rate through time as taxonomic dissimilarity between adjacent fossil assemblages is strongly predicted by their age difference. A similar pattern characterizes functional ecological turnover, with only subtle changes in dietary proportions, body size proportions, and bovid abundances across the composite lower Awash sequence. Biochronological comparisons with other sites in eastern Africa suggest that the taxa recovered from the Maka'amitalu are broadly consistent with the reported age of the BKT-3 tuff. Considering the age of BKT-3 and biochronology, a range of 2.4-1.9 Ma is most likely for the faunal assemblage.
早更新世是东非哺乳动物区系进化的关键时期,但埃塞俄比亚阿法尔洼地的化石组合在这一时期的采样情况知之甚少。Hadar 研究项目在 Awash 河谷较低处的 Busidima 组(2.7-0.8 Ma)进行实地考察,在 20 世纪 90 年代从 Maka'amitalu 盆地回收了一个带有石器和动物群的早期上颌骨(A.L. 666-1)。这些组合的年代由 Bouroukie Tuff 3(BKT-3)确定为2.35 Ma。Had ar 研究项目在过去二十年的持续工作极大地扩展了动物群的收集。在这里,我们全面描述了 Maka'amitalu 大型哺乳动物(偶蹄目、食肉目、奇蹄目、灵长目和长鼻目),并讨论了它们的古生态和生物年代学意义。与 Hadar 组(3.45-2.95 Ma)和 Ledi-Geraru 组(2.8-2.6 Ma)相比,Maka'amitalu 组合的规模较小,但至少包括 20 个分类群。有蹄类、猪科和 是最丰富和丰富的,而食肉目、马科和大型食草动物则很少。虽然 Maka'amitalu 动物群的分类组成表明与 Hadar 组和 Ledi-Geraru 沉积物有显著的物种更替,但随着时间的推移,更替似乎以恒定的速度发生,因为相邻化石组合之间的分类差异强烈预测了它们的年龄差异。功能生态的更替也呈现出类似的模式,只有在整个下 Awash 序列中,饮食比例、体型比例和有蹄类动物的丰度发生了细微的变化。与东非其他地点的生物年代学比较表明,从 Maka'amitalu 回收的分类群与报道的 BKT-3 凝灰岩年龄大致一致。考虑到 BKT-3 的年龄和生物年代学,该动物群最有可能的年龄范围是 2.4-1.9 Ma。