Garralda María Dolores, Le Cabec Adeline, Maíllo Fernández José Manuel, Maureille Bruno, Gunz Philipp, Neira Ana, Hublin Jean Jacques, Bernaldo de Quirós Federico
Departamento de Biodiversidad, Ecología y Evolución. Facultad de CC. Biológicas, Universidad Complutense de Madrid, Ciudad Universitaria, 28040 Madrid, Spain,
Univ. Bordeaux, CNRS, MC, PACEA, UMR 5199, F-33600 Pessac, France.
J Anthropol Sci. 2023 Oct 20;100:123-142. doi: 10.4436/JASS.10021. Epub 2023 Aug 9.
El Castillo cave is a well-known site because of its Paleolithic archaeology and parietal rock art. This paper is focused on the human remains found by V. Cabrera in the Mousterian Unit XX assigned to MIS 4 and early MIS 3. The fossils consist of one upper left second premolar (ULP4), one incomplete proximal hand phalanx, and one partial femoral head. The tooth and the phalanx were assigned to adults, whereas the femoral head belonged to an immature individual due to the absence of fusion traces to the metaphyseal surface. The external morphology and metrical characterization of the Castillo-1466 (ULP4) tooth crown was quantified and compared to the variability of other Neanderthal dental remains and a sample of modern human populations. We also quantified its 3D enamel thickness distribution, its roots morphology, as well as the presence of chipping, and their possible relation to masticatory or paramasticatory activities. Castillo-1466 shows crown dimensions compatible with middle-sized Neanderthal teeth, but with a remarkably thicker enamel than other Neanderthal premolars, such as Marillac 13. The femoral head and the hand phalanx fragment are compared to published values for Neanderthals, although both partial fossils lack diagnostic features precluding any clear taxonomic diagnostic. Therefore, their attribution to Neanderthals is assumed based on the dating of the layers in which they were discovered. El Castillo cave Mousterian fossils represent another contribution to the knowledge of the Middle Paleolithic populations of Northern Spain, where different sites along the Cantabrian mountains yielded several human remains assigned to MIS 4 and early MIS 3.
埃尔卡斯蒂略洞穴因其旧石器时代考古学和岩壁岩石艺术而闻名。本文聚焦于V. 卡布雷拉在莫斯特阶第XX单元发现的人类遗骸,该单元被认定为海洋同位素阶段(MIS)4和MIS 3早期。化石包括一颗左上第二前磨牙(ULP4)、一根不完整的近端手趾骨和一个部分股骨头。牙齿和指骨被认定为成年人的,而股骨头属于一个未成熟个体,因为其与干骺端表面没有融合痕迹。对卡斯蒂略 - 1466(ULP4)牙冠的外部形态和测量特征进行了量化,并与其他尼安德特人牙齿遗骸的变异性以及现代人类群体样本进行了比较。我们还量化了其三维牙釉质厚度分布、牙根形态以及是否存在缺口,及其与咀嚼或准咀嚼活动的可能关系。卡斯蒂略 - 1466显示出与中型尼安德特人牙齿相符的牙冠尺寸,但牙釉质比其他尼安德特人前磨牙(如马里亚克13)厚得多。将股骨头和手趾骨碎片与已公布的尼安德特人数据进行了比较,尽管这两块部分化石缺乏诊断特征,无法进行明确的分类诊断。因此,基于它们被发现的地层年代,假定它们属于尼安德特人。埃尔卡斯蒂略洞穴的莫斯特阶化石为了解西班牙北部旧石器时代中期的人群做出了另一贡献,在坎塔布里亚山脉沿线的不同遗址出土了几具被认定为MIS 4和MIS 3早期的人类遗骸。