Wood B, Wood C, Konigsberg L
Department of Human Anatomy and Cell Biology, University of Liverpool, UK.
Am J Phys Anthropol. 1994 Oct;95(2):117-36. doi: 10.1002/ajpa.1330950202.
Of the presently recognised early hominid species, Paranthropus boisei is one of the better known from the fossil record and arguably the most distinctive; the latter interpretation rests on the numbers of apparently derived characters it incorporates. The species as traditionally diagnosed is distributed across approximately one million years and is presently confined to samples from East African sites. The hypodigm has been examined for evidence of intraspecific phyletic evolution, with particular emphasis on the areas best represented in the fossil record, namely the teeth and mandible. The results of this examination of 55 mandibular and dental variables which uses the gamma test statistic for the detection of trend, and nonparametric spline regression (Loess regression) for investigating pattern and rate of temporal change, show that within Paranthropus boisei sensu stricto most evidence of temporally related morphological trends relates to the morphology of the P4 crown. There is little or no evidence of any tendency to increase in overall size through time. Fossils from the Omo Shungura Formation and West Turkana which have been recovered from a time period earlier than the P. boisei sensu stricto hypodigm resemble the latter taxon in some features, but differ from it in aspects of cranial morphology. There is insufficient fossil evidence of the earlier taxon to tell whether it changes through time, but when trends of 47 mandibular and dental variables are assessed across the combined East African "robust" australopithecine sample, there is evidence for a relatively abrupt change around 2.2-2.3 Myr in approximately 25% of the dental and mandibular remains. Some of these changes correspond with the temporal trends within P. boisei sensu stricto, but others, such as mandible height, do not. If the earlier material is ancestral to P. boisei sensu stricto, evidence from the teeth and jaws is consistent with a punctuated origin for the latter taxon.
在目前已被认可的早期原始人类物种中,鲍氏傍人是化石记录中较为知名且无疑最具独特性的物种之一;后一种解读基于其包含的明显衍生特征的数量。传统诊断的该物种分布跨越约一百万年,目前仅限于来自东非遗址的样本。已对其模式标本进行检查,以寻找种内系统发育进化的证据,特别关注化石记录中表现最佳的区域,即牙齿和下颌骨。对55个下颌骨和牙齿变量进行检查的结果显示,在严格意义上的鲍氏傍人内部,大多数与时间相关的形态学趋势证据都与P4冠的形态有关。几乎没有证据表明其整体大小随时间有增加的趋势。从奥莫舒古拉组和图尔卡纳西部发现的化石,其年代早于严格意义上的鲍氏傍人模式标本,在某些特征上与后一个分类单元相似,但在颅骨形态方面有所不同。关于早期分类单元是否随时间变化,化石证据不足,但当对东非“粗壮”南方古猿组合样本中的47个下颌骨和牙齿变量趋势进行评估时,约25%的牙齿和下颌骨遗骸显示在约220 - 230万年前有相对突然的变化。其中一些变化与严格意义上的鲍氏傍人内部随时间的趋势相符,但其他一些变化,如下颌骨高度,则不相符。如果早期材料是严格意义上的鲍氏傍人的祖先,那么来自牙齿和颌骨的证据与后一个分类单元的间断起源是一致的。