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伊朗中扎格罗斯西部的尼安德特人。Wezmeh 1 上颌前磨牙的结构再评估。

A Neanderthal from the Central Western Zagros, Iran. Structural reassessment of the Wezmeh 1 maxillary premolar.

机构信息

Laboratoire PACEA, UMR 5199 CNRS, Université de Bordeaux, Ministère de La Culture, Bordeaux, France.

Paleolithic Department, National Museum of Iran, Tehran, Iran.

出版信息

J Hum Evol. 2019 Oct;135:102643. doi: 10.1016/j.jhevol.2019.102643. Epub 2019 Aug 13.

Abstract

Wezmeh Cave, in the Kermanshah region of Central Western Zagros, Iran, produced a Late Pleistocene faunal assemblage rich in carnivorans along with a human right maxillary premolar, Wezmeh 1, an unerupted tooth from an 8 ± 2 year-old individual. Uranium-series analyses of the fauna by alpha spectrometry provided age estimates between 70 and 11 ka. Crown dimensions place the tooth specimen at the upper limits of Late Pleistocene human ranges of variation. Wezmeh 1 metameric position (most likely a P) remains uncertain and only its surficial morphology has been described so far. Accordingly, we used microfocus X-ray tomography (12.5 μm isotropic voxel size) to reassess the metameric position and taxonomic attribution of this specimen. We investigated its endostructural features and quantified crown tissue proportions. Topographic maps of enamel thickness (ET) distribution were also generated, and semilandmark-based geometric morphometric analyses of the enamel-dentine junction (EDJ) were performed. We compared Wezmeh 1 with unworn/slightly-moderately worn P and P of European Neanderthals, Middle Paleolithic modern humans from Qafzeh, an Upper Paleolithic premolar, and Holocene humans. The results confirm that Wezmeh 1 represents a P. Based on its internal conformation and especially EDJ shape, Wezmeh 1 aligns closely with Neanderthals and is distinct from the fossil and extant modern human pattern of our comparative samples. Wezmeh 1 is thus the first direct evidence of Neanderthal presence on the western margin of the Iranian Plateau.

摘要

我们在伊朗中扎格罗斯西部的克尔曼沙赫地区的 Wezmeh 洞穴发现了一个晚更新世的动物群,其中富含食肉动物,还有一个人类右上颌前磨牙,Wezmeh 1,这是一颗来自 8±2 岁个体的未萌出牙。对动物群的铀系分析通过阿尔法谱仪提供了 70 到 11 ka 的年龄估计。牙冠尺寸将牙齿标本置于晚更新世人类变异范围的上限。牙齿标本的 Wezmeh 1 分节位置(很可能是 P)仍然不确定,到目前为止,只描述了其表面形态。因此,我们使用微焦点 X 射线断层扫描(12.5 μm 各向同性体素大小)重新评估了该标本的分节位置和分类归属。我们研究了它的内结构特征,并量化了牙冠组织的比例。还生成了釉质厚度(ET)分布的地形地图,并对牙本质-釉质交界处(EDJ)进行了基于半标志的几何形态测量分析。我们将 Wezmeh 1 与未磨损/轻度磨损的 P 和 P 进行了比较,包括欧洲尼安德特人、卡法泽的中更新世现代人、上更新世的前磨牙和全新世的人类。结果证实 Wezmeh 1 代表 P。基于其内部形态和特别是 EDJ 形状,Wezmeh 1 与尼安德特人非常接近,与我们比较样本中的化石和现生现代人模式明显不同。因此,Wezmeh 1 是尼安德特人在伊朗高原西缘存在的第一个直接证据。

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