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来自埃塞俄比亚高地梅尔卡昆图雷加尔巴四号早期更新世遗址的一个直立人幼年下颌骨的结构组织与牙齿发育情况

Structural organization and tooth development in a Homo aff. erectus juvenile mandible from the Early Pleistocene site of Garba IV at Melka Kunture, Ethiopian highlands.

作者信息

Zanolli Clément, Dean M Christopher, Assefa Yared, Bayle Priscilla, Braga José, Condemi Silvana, Endalamaw Metasebia, Engda Redae Blade, Macchiarelli Roberto

机构信息

Laboratoire AMIS, UMR 5288 CNRS, Université Toulouse III Paul Sabatier, Toulouse, France.

Department of Cell and Developmental Biology, University College, London, United Kingdom.

出版信息

Am J Phys Anthropol. 2017 Mar;162(3):533-549. doi: 10.1002/ajpa.23135. Epub 2016 Nov 24.

DOI:10.1002/ajpa.23135
PMID:27883188
Abstract

OBJECTIVES

The immature partial mandible GAR IVE from the c. 1.7 Ma old Garba IV site at Melka Kunture (Upper Awash Basin, Ethiopia), the earliest human representative from a mountain-like environment, represents one of the oldest early Homo specimens bearing a mixed dentition. Following its first description (Condemi, ), we extended the analytical and comparative record of this specimen by providing unreported details about its inner morphology, tooth maturational pattern and age at death, crown size, and tooth tissue proportions.

MATERIALS AND METHODS

The new body of quantitative structural information and virtual imaging derives from a medical CT record performed in 2013.

RESULTS

Compared to the extant human condition and to some fossil representatives of comparable individual age, the GAR IVE mandible reveals absolutely and relatively thick cortical bone. Crown size of the permanent lateral incisor and the canine fit the estimates of H. erectus s.l., while the dm2 and the M1 more closely approach those of H. habilis-rudolfensis. Molar crown pulp volumes are lower than reported in other fossil specimens and in extant humans. The mineralization sequence of the permanent tooth elements is represented four times in our reference sample of extant immature individuals (N = 795).

CONCLUSIONS

The tooth developmental pattern displayed by the immature individual from Garba IV falls within the range of variation of extant human populations and is also comparable with that of other very young early fossil hominins. Taken together, the evidence presented here for mandibular morphology and dental development suggest GAR IVE is a robust 2.5- to 3.5-year old early Homo specimen.

摘要

目的

来自埃塞俄比亚上阿瓦什盆地梅尔卡昆图雷约170万年前的加尔巴四世遗址的不成熟部分下颌骨GAR IVE,是来自类似山区环境的最早人类代表,是带有混合牙列的最古老早期人类标本之一。在首次描述之后(孔德米,),我们通过提供有关其内部形态、牙齿成熟模式和死亡年龄、牙冠大小以及牙齿组织比例的未报告细节,扩展了该标本的分析和比较记录。

材料与方法

新的定量结构信息和虚拟成像来自于2013年进行的医学CT记录。

结果

与现存人类状况以及一些年龄相当的化石代表相比,GAR IVE下颌骨显示出绝对和相对较厚的皮质骨。恒侧切牙和犬齿的牙冠大小符合直立人广义的估计,而乳磨牙dm2和第一恒磨牙M1更接近能人-鲁道夫猿人的牙冠大小。磨牙牙冠髓腔体积低于其他化石标本和现存人类的报告值。在我们现存未成熟个体的参考样本(N = 795)中,恒牙元素的矿化序列出现了四次。

结论

来自加尔巴四世的未成熟个体所显示的牙齿发育模式落在现存人类种群的变异范围内,也与其他非常年轻的早期化石人类的发育模式相当。综合来看,这里提供的下颌形态和牙齿发育证据表明GAR IVE是一个健壮的2.5至3.5岁的早期人类标本。

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