Brief Communication: An Incipient Coronal Caries Lesion on a Neandertal Molar Tooth From El Sidrón Cave (Northern Spain)

IF 2 2区 生物学 Q1 ANTHROPOLOGY
Almudena Estalrrich, José Antonio Alarcón, Antonio García Tabernero, Antonio Rosas
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Abstract

Objectives

Here, we present the findings of an incipient caries lesion on a permanent upper left second molar attributed to an adult male Neandertal individual from El Sidrón Cave. This study presents new data regarding the antiquity of human caries lesions, their development, and the possibility of the para-masticatory behavior component as a contributory factor in their origin, at least in Homo neanderthalensis.

Materials and Methods

The tooth was examined using a μCT scan to confirm the lesion and to evaluate its extent. Element chemical analysis was performed to check the decalcification on both the lesion edges and pristine surfaces (as carious lesions often involve demineraization of the tissues) using an environmental scanning electron microscope.

Results

The lesion was located on the occlusal surface on the protocone cusp, a small furrow filled with sediment, 2.6 mm in length and 0.78 mm in width, and mineral loss on the white surrounding area compared to the apparently intact adjacent enamel.

Discussion

This pit lesion resembles the appearance of other Neandertal carious lesions, all from temperate environments. Calcium and phosphorus loss has been documented as has been characterized on dental caries. Regarding the etiology, we propose that an intense masticatory and para-masticatory activity combined with evidence for a mixed diet with a high carbohydrate component, the molar tooth may have developed a crack lesion, which was then colonized by a bacterial biofilm that deepened into the dentine and developed this small channel-shaped caries.

Abstract Image

简短的交流:来自El Sidrón洞穴(西班牙北部)的尼安德特人臼齿的早期冠状龋损伤
在这里,我们介绍了一名来自El Sidrón洞穴的成年男性尼安德特人永久左上第二磨牙的早期龋齿病变的发现。这项研究提供了关于人类龋齿病变的古老、发展以及准咀嚼行为成分作为其起源的一个促成因素的可能性的新数据,至少在尼安德特人中是这样。材料与方法采用μCT扫描确定病变,评估病变程度。使用环境扫描电子显微镜进行元素化学分析以检查病变边缘和原始表面的脱钙(因为龋齿病变通常涉及组织脱矿)。结果病变位于原锥体尖牙合面上,呈长2.6 mm,宽0.78 mm的小沟状充填沉积物,与相邻牙釉质明显完整的牙釉质相比,周围白色区域矿物丢失。这个坑状病变类似于其他穴居人龋齿病变的外观,都来自温带环境。钙和磷的流失已被证明是龋齿的特征。关于病因,我们提出强烈的咀嚼和副咀嚼活动,再加上高碳水化合物成分的混合饮食,磨牙可能已经形成了一个裂纹病变,然后被细菌生物膜定植,深入到牙本质并形成了这个小通道状的龋齿。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
4.80
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