PaleoAnthropology Group, Department of Paleobiology, Museo Nacional de Ciencias Naturales, CSIC, Calle José Gutiérrez Abascal 2, Madrid, Spain.
Am J Phys Anthropol. 2011 Jan;144(1):154-61. doi: 10.1002/ajpa.21359.
The distribution of subvertical grooves on interproximal wear dental facets from the El Sidrón (Asturias, Spain) Neandertals is described and analyzed. Out of 93 teeth, 64.5% present subvertical grooves, including a high frequency (50%) on the anterior dentition. Contrary to some studies, subvertical grooves from adjacent facets perfectly overlap each other and do not interdigitate, probably forming small channels. Both the facet and the groove surface share the same polished appearance, suggesting a common origin. Statistical analyses reveal that the number of grooves is neither dependent on the degree of occlusal wear, nor on the position on the tooth or the individual's age. However, facet width is an important factor determining the number of subvertical grooves. The etiology of subvertical grooves formation on Neandertal teeth remains unclear.
本文描述和分析了来自西班牙阿斯图里亚斯的埃尔西德龙(El Sidrón)尼安德特人近中磨面牙小尖嵴上的亚垂直沟的分布情况。93 颗牙齿中,64.5%有亚垂直沟,其中前牙的出现频率较高(50%)。与一些研究不同,相邻小尖嵴上的亚垂直沟完全重叠而不交错,可能形成了小的沟道。小尖嵴和沟表面具有相同的抛光外观,表明它们具有共同的起源。统计分析表明,沟的数量既不取决于咬合磨损的程度,也不取决于牙齿的位置或个体的年龄。然而,小尖嵴的宽度是决定亚垂直沟数量的一个重要因素。尼安德特人牙齿上亚垂直沟形成的病因仍不清楚。