Comparative morphology and morphometric assessment of the Neandertal occipital remains from the El Sidrón site (Asturias, Spain: years 2000–2008)

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• 作者：Markus Bastir ; Antonio Rosas ; Antonio Garcí ; a Tabernero ; Angel Peñ ; a-Meliá ; n ; Almudena Estalrrich ; Marco de la Rasilla ; Javier Fortea
• 关键词：Fossils ; Intraspecific variation ; Middle Pleistocene human evolution ; Geometric morphometrics ; Virtual anthropology
• 刊名：Journal of Human Evolution
• 出版年：2010
• 出版时间：January 2010
• 年：2010
• 卷：58
• 期：1
• 页码：68-78
• 全文大小：1020 K

文摘

This paper analyses the occipital remains recovered from the El Sidrón (Asturias, Spain) Neandertal site between the years of 2000–2008. The sample is represented by three specimens, SD-1219, SD-1149, and SD-370a. Descriptive morphology, linear measurements, 3D geometric morphometrics, and virtual anthropological methods were employed to address the morphological, morphometric, and phylogenetic affinities of these fossils. The fossils display Neandertal autapomorphies (e.g., bilaterally protruding transverse occipital torus, suprainiac fossa). SD-1219 also preserves a strongly projecting juxtamastoid eminence and shows occipital bunning. In linear distances, the El Sidrón occipitals are similar to each other and close to the Neandertal mean. The centroid size of SD-1219 is slightly larger than the Neandertal average. All of the evidence taken together points to the hypothesis that SD-1219 belongs to a smaller Neandertal male. Linear measurements and the vault thickness of SD-1149 also suggest a robust male individual. The gracility of SD-370a points towards an immature individual. Virtual anthropological methods were used to reconstruct a 3D model of the SD-1219 occipital for geometric morphometrics, which reveals that SD-1219 shows relatively broad and low occipital plane proportions. Within the European Pleistocene lineage sample, this fossil falls geometrically closer to primitive rather than to derived morphologies because of its increased width, and a lower, anterior position of inion relative to the biasterionic axis. These results may imply that cranial sphericity could be an important feature of intraspecific Neandertal variability. Our findings open the way for further studies of intraspecific variation in Neandertal populations, in which the El Sidrón sample may play a significant role.