来自南非西开普省顶峰点PP5-6N岩石庇护所的晚更新世人类脚踏板方阵

IF 1.7 2区 生物学 Q1 ANTHROPOLOGY
Adrián Pablos, Frederick E. Grine, Naomi Cleghorn, Katherine Elmes, Carrie S. Mongle, Curtis W. Marean
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引用次数: 0

摘要

目的对Pinnacle Point PP5-6N岩洞LBSR地层砾岩底部附近出土的非虚构远端脚趾骨(PP 654270)进行描述和形态计量学比较分析。它来源于两个主要地层集合接触处的薄燃烧特征(可能是原位炉底),其过渡的模拟年龄范围为91.9-86.0 ka,这将该化石置于MIS 5b。材料和方法该指骨(PP 654270)被评估为可能来自射线II或III右侧的远端指骨。这块骨头补充了来自非洲南部晚更新世的极少量足跖骨样本。我们将这个方阵的度量变量与几个化石和最近的人类样本进行了比较。结果骨皮层较薄,近端尤其是远端有弥漫性骨小梁网。与尼安德特人的同类相比,他们的指骨又长又窄,而且相对纤细。PP 654270密集阵显示出与准同时期欧亚中旧石器时代和近代现代人的相似性,尽管这些样品中的射线II和III同源物往往相对较长。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

A Late Pleistocene Human Pedal Phalanx From the Pinnacle Point PP5-6N Rock-Shelter, Western Cape Province, South Africa

A Late Pleistocene Human Pedal Phalanx From the Pinnacle Point PP5-6N Rock-Shelter, Western Cape Province, South Africa

Objectives

This study provides the description and comparative morphometric analysis of a non-hallucial distal pedal phalanx (PP 654270) excavated from near the base of the LBSR Stratigraphic Aggregate in the Pinnacle Point PP5-6N rock-shelter. It derives from a thin combustion feature (probably an in situ hearth) at the contact of two major stratigraphic aggregates, the transition of which has a modeled age range of 91.9–86.0 ka, which places this fossil in MIS 5b.

Material and Method

This phalanx (PP 654270) is assessed as representing a distal phalanx probably from the right side of Ray II or III. This bone adds to the very meager sample of pedal phalanges from the late Pleistocene of southern Africa. We compared the metric variables of this phalanx to several fossil and recent Homo samples.

Results

The bone has a comparatively thin cortex and a diffuse trabecular network in the proximal and especially the distal ends. The phalanx is long, narrow, and relatively gracile in comparison to Neandertal homologues.

Discussion

The phalanx PP 654270 displays similarities with penecontemporaneous Eurasian Middle Paleolithic and recent modern humans, although it tends to be comparatively long for Ray II and III homologues in these samples.

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