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斯泰克方丹5号成员的地层学、人工制品工业与人类关联

Stratigraphy, artefact industries and hominid associations for Sterkfontein, member 5.

作者信息

Kuman K, Clarke R J

机构信息

Department of Archaeology, University of the Witwatersrand, Johannesburg, Wits 2050, South Africa.

出版信息

J Hum Evol. 2000 Jun;38(6):827-47. doi: 10.1006/jhev.1999.0392.

Abstract

A revised stratigraphy for the early hominid site of Sterkfontein (Gauteng Province, South Africa) reveals a complex distribution of infills in the main excavation area between 2.8 and 1.4 m.y.a, as well as deposits dating to the mid to late Pleistocene. New research now shows that the Member 4 australopithecine breccia (2.8-2.6 Ma) extends further west than was previously thought, while a late phase of Member 4 is recognized in a southern area. The artefact-bearing breccias were defined sedimentologically as Member 5, but one supposed part of these younger breccias, the StW 53 infill, lacks in situ stone tools, although it does appear to post-date 2.6 Ma when artefacts first appear in the archaeological record. The StW 53 hominid, previously referred to Homo habilis, is here argued to be Australopithecus. The first artefact-bearing breccia of Member 5 is the Oldowan Infill, estimated at 2-1.7 Ma. It occupies a restricted distribution in Member 5 east and contains an expedient, flake-based tool industry associated with a few fossils of Paranthropos robustus. An enlarged cave opening subsequently admitted one or more Early Acheulean infills associated in Member 5 west with Homo ergaster. The artefacts attest to a larger site accumulation between ca. 1.7 and 1.4 Ma, with more intensive use of quartzite over quartz and a subtle but important shift to large flakes and heavier-duty tools. The available information on palaeoenvironments is summarized, showing an overall change from tropical to sub-tropical gallery forest, forest fringe and woodland conditions in Member 4 to more open woodland and grassland habitats in the later units, but with suggestions of a wet localized topography in the Paranthropus -bearing Oldowan Infill.

摘要

斯泰克方丹早期人类遗址(南非豪登省)的地层修订显示,在280万至140万年前的主要挖掘区域内,填充物分布复杂,同时还有可追溯到更新世中晚期的沉积物。新研究表明,4号成员南方古猿角砾岩(280 - 260万年前)向西延伸的范围比之前认为的更远,同时在南部区域识别出了4号成员的晚期阶段。含有人工制品的角砾岩在沉积学上被定义为5号成员,但这些较年轻角砾岩的一个假定部分,即斯泰克方丹53号填充物,缺乏原地石器工具,尽管它似乎确实晚于260万年前,而人工制品首次出现在考古记录中的时间是260万年前。此前被归类为能人(Homo habilis)的斯泰克方丹53号人类,在这里被论证为南方古猿。5号成员的首个含有人工制品的角砾岩是奥杜威填充物,估计年代为200 - 170万年前。它在5号成员东部的分布范围有限,包含一种权宜性的、以石片为基础的工具工业,与一些粗壮傍人(Paranthropos robustus)化石相关。随后一个扩大的洞穴开口容纳了一个或多个与5号成员西部的匠人(Homo ergaster)相关的早期阿舍利文化填充物。这些人工制品证明在约170万至140万年前有一个更大的遗址堆积,与石英相比,石英岩的使用更加密集,并且有一个微妙但重要的转变,即转向大型石片和更重型的工具。对古环境的现有信息进行了总结,显示从4号成员的热带到亚热带长廊森林、森林边缘和林地环境总体上转变为后期单元中更开阔的林地和草原栖息地,但在含有傍人的奥杜威填充物中有局部潮湿地形的迹象。

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