Prang Thomas C
Center for the Study of Human Origins, Department of Anthropology, New York University, New York, NY 10003, USA.
J Hum Evol. 2015 Mar;80:135-46. doi: 10.1016/j.jhevol.2014.09.001. Epub 2014 Oct 18.
A key pedal adaptation to bipedality is a relatively large, weight-bearing calcaneus. The earliest evidence for a human-like, robust calcaneus is at 3.2 Ma in Australopithecus afarensis (A.L. 333-8, A.L. 333-55, A.L. 333-37) from Hadar, Ethiopia. Australopithecus sediba at 1.98 Ma from Malapa, South Africa displays a unique combination of primitive australopith features and more derived Homo-like features, but surprisingly is characterized by a gracile, chimpanzee-like calcaneus. The differences in calcaneal morphology suggest that these taxa differed in the frequency of arboreality and in the manner of foot function during terrestrial bipedal locomotion. This study examines calcaneal morphology in extant hominids (i.e., great apes and humans; N = 95) and fossil hominins (N = 5) to better understand the evolutionary development of calcaneal robusticity in early hominins. In particular, this study focuses on two additional fossil hominin calcanei that have not figured prominently in previous discussions of calcaneal robusticity: StW 352 and Omo 33-74-896. A measure of calcaneal robusticity was quantified as the ratio of calcaneal tuber cross-sectional area to calcaneal tuber length, which significantly differs between humans and non-humans using a sequential Bonferroni alpha adjustment for multiple comparisons. Additional multivariate analyses using Mosimann shape variables show that StW 352 and Omo 33-74-896 are more similar to Au. sediba in calcaneal tuber morphology than to Au. afarensis, suggesting that the latter taxon is better adapted for terrestrial bipedalism than at least some later species of Australopithecus. This finding implies the possibility of several complex evolutionary scenarios involving either multiple reversals in postcranial morphology in Australopithecus or the independent acquisition of adaptations to terrestrial bipedalism in Au. afarensis and Homo.
对两足行走的一个关键足部适应性变化是相对较大的、承重的跟骨。最早的类似人类的粗壮跟骨证据来自埃塞俄比亚哈达尔的320万年前的阿法南方古猿(A.L. 333 - 8、A.L. 333 - 55、A.L. 333 - 37)。来自南非马拉帕的198万年前的南方古猿源泉种展现出原始南方古猿特征和更具衍生性的类人特征的独特组合,但令人惊讶的是其特征是纤细的、类似黑猩猩的跟骨。跟骨形态的差异表明这些分类群在树栖频率和陆地两足行走时的足部功能方式上有所不同。本研究检查了现存人科动物(即大猩猩和人类;N = 95)和化石人族(N = 5)的跟骨形态,以更好地理解早期人族跟骨粗壮度的进化发展。特别是,本研究聚焦于另外两块在之前关于跟骨粗壮度的讨论中未占据显著地位的化石人族跟骨:StW 352和奥莫33 - 74 - 896。跟骨粗壮度的一个衡量指标被量化为跟骨结节横截面积与跟骨结节长度的比值,使用顺序邦费罗尼α调整进行多重比较时,该比值在人类和非人类之间有显著差异。使用莫西曼形状变量的额外多变量分析表明,StW 352和奥莫33 - 74 - 896在跟骨结节形态上与南方古猿源泉种比与阿法南方古猿更相似,这表明后一个分类群比至少一些后来的南方古猿物种更适应陆地两足行走。这一发现意味着几种复杂进化情景的可能性,涉及南方古猿颅后形态中的多次逆转,或者阿法南方古猿和人属对陆地两足行走适应性的独立获得。