首页> 外文期刊>Journal of Human Evolution >Microbial osteolysis in an Early Pleistocene hominin (Paranthropus robustus) from Swartkrans, South Africa
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Microbial osteolysis in an Early Pleistocene hominin (Paranthropus robustus) from Swartkrans, South Africa

机译:来自南非Swartkrans的早期更新世人源素(Paranthropusrobus)中的微生物骨溶解

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Microbiological degradation is one of the most important factors responsible for the destruction of bone in archaeological contexts. Microscopic focal destruction (MFD) is the most prevalent form of microbial tunneling and is encountered very commonly in human bones from archaeological sites, whereas animal bones from these same sites show significantly better preservation if they were deposited in a fragmentary (e.g., butchered) state. Similarly, most fossils show either no evidence or only minor traces of bacterial osteolysis. These observations and experimental evidence point to an endogenous origin for osteolytic bacteria, suggesting that bone bioerosion could potentially aid in reconstructing early taphonomic events. We here report extensive MFD in the mandibular corpus of a small (presumptive female) individual of the hominin Paranthropus robustus from the Early Pleistocene site of Swartkrans, South Africa. The specimen (SKX 5013) derives in situ from the Member 2 deposit, which is dated to ca. 1.5 -1.0 Ma. Examination of sections from the corpus by backscattered electron microscopy reveals numerous small linear longitudinal and budded tunneling cavities, which tend to be concentrated around Haversian canals and are more abundant closer to the endosteal aspect of the section. The taphonomy of Swartkrans has been the subject of intense investigation, and given the possibility that different agents of accumulation may have been responsible for the faunal and hominin fossils in the different members at the site, the observation that a specimen of P. robustus from Member 2 displays significant microbial osteolysis is of potential interest. A study of the prevalence of this process in adequately large samples of the animal bones from these units may yield novel insights and provide refinement of our understanding of their taphonomic histories. Such observations might well reveal differences among the various members that could provide another valuable source of osteoarchaeological information for the site. (C) 2015 Elsevier Ltd. All rights reserved.
机译:微生物降解是在考古环境中破坏骨骼的最重要因素之一。显微聚焦破坏(MFD)是微生物隧穿的最普遍形式,在考古现场的人类骨骼中非常常见,而来自同一地点的动物骨骼如果以零碎(例如,屠宰)状态沉积,则显示出明显更好的保存性。 。同样,大多数化石没有显示出任何迹象,也没有发现细菌溶骨的痕迹。这些观察和实验证据指出溶骨细菌的内源性起源,表明骨生物侵蚀可能潜在地帮助重建早期的染色体异常事件。我们在这里报告了来自南非Swartkrans早期更新世位点的人型Paranthropusrobustus小(假定女性)个体的下颌体广泛的MFD。标本(SKX 5013)是从成员2矿床中原位获得的,该矿床的历史可追溯至大约3年。 1.5 -1.0毫安。通过反向散射电子显微镜检查从sections体切片,发现大量小的线性纵向和萌芽的隧道腔,往往集中在哈弗斯运河周围,并且更靠近切片的骨内膜方面。 Swartkrans的拓朴学一直是深入研究的主题,并且考虑到可能存在不同的积累因子来负责该地点不同成员的动物和人为化石,观察到来自该成员的P.robustus标本2显示出明显的微生物骨溶解是潜在的兴趣。对来自这些单位的足够大的动物骨骼样本中这一过程的普遍性进行研究可能会产生新颖的见解,并进一步完善我们对它们的自相历史的理解。这样的观察结果很可能揭示出各个成员之间的差异,这可能会为该部位提供另一个有价值的骨考古信息。 (C)2015 Elsevier Ltd.保留所有权利。

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