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从副狒狒及其他化石狒狒属动物的面部亲缘关系推断上新世-更新世南非生物年代学。

Inferring Plio-Pleistocene southern African biochronology from facial affinities in Parapapio and other fossil papionins.

作者信息

Williams F L, Ackermann R R, Leigh S R

机构信息

Department of Anthropology, Georgia State University, Atlanta, GA 30303, USA.

出版信息

Am J Phys Anthropol. 2007 Feb;132(2):163-74. doi: 10.1002/ajpa.20504.

Abstract

Buried in the same South African cave deposits as Australopithecus, fossil papionins have been referred to Parapapio (Pp. whitei, Pp. broomi, Pp. jonesi, Pp. antiquus), Papio (P. izodi, P. angusticeps, P. h. robinsoni), Theropithecus (e.g., T. darti), Gorgopithecus, or Dinopithecus on the basis of postcanine tooth size and descriptive morphology of the muzzle. The morphological patterns of variation that these papionins demonstrate can help to place the Australopithecus fossils into a biochronological context and provide valuable information for reconstructing regional Plio-Pleistocene turnover. To document these patterns of variation across fossil-bearing sites, we explore morphometric affinities within Parapapio, and between Parapapio and other Plio-Pleistocene taxa (Dinopithecus ingens, Papio angusticeps, Papio izodi, and Theropithecus darti) by analyzing a sample of interlandmark distances derived from 3-D coordinate data of the most complete fossil papionin specimens available. Bivariate and multivariate analyses show that Pp. whitei exhibits as much variation between sites and between individuals as Pp. broomi and Pp. whitei combined. Diversity in Parapapio at Makapansgat and Sterkfontein may suggest substantial time depth to the caves. Theropithecus darti, Dinopithecus ingens, Papio angusticeps, Pp. whitei from Bolt's Farm (BF 43), and Pp. jonesi from Sterkfontein (STS 565) differ considerably from one another. Other Parapapio specimens across sites form a separate cluster with P. izodi from Taung, suggesting a Pliocene age for this site.

摘要

与南方古猿一同埋藏在南非同一洞穴沉积物中的化石狒狒,根据犬齿后牙齿大小和口鼻部的描述形态,被归类为副狒狒属(白氏副狒狒、布鲁姆氏副狒狒、琼斯氏副狒狒、古老副狒狒)、狒狒属(伊佐迪狒狒、狭头狒狒、罗宾逊氏狒狒)、草原狒狒属(如达尔蒂草原狒狒)、恐狒属或硕狒属。这些狒狒所展现出的形态变异模式有助于将南方古猿化石置于生物年代学背景中,并为重建区域上新世 - 更新世更替提供有价值的信息。为了记录这些含化石地点间的变异模式,我们通过分析从现有最完整的化石狒狒标本的三维坐标数据得出的地标间距离样本,探究了副狒狒属内部以及副狒狒属与其他上新世 - 更新世分类群(硕狒、狭头狒狒、伊佐迪狒狒和达尔蒂草原狒狒)之间的形态测量亲缘关系。双变量和多变量分析表明,白氏副狒狒在不同地点和个体间展现出的变异程度与布鲁姆氏副狒狒和白氏副狒狒两者的变异程度之和相当。马卡潘斯盖特和斯泰克方丹的副狒狒属多样性可能表明这些洞穴具有相当长的时间深度。达尔蒂草原狒狒、硕狒、狭头狒狒、来自博尔特农场的白氏副狒狒(BF 43)以及来自斯泰克方丹的琼斯氏副狒狒(STS 565)彼此差异很大。不同地点的其他副狒狒标本与来自汤恩的伊佐迪狒狒形成一个单独的聚类,表明该地点为上新世时期。

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