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南非阿马齐斯泉地区 1 号的一个海洋同位素阶段 11 沿海阿舍利手工作坊,以及与之相关的木材。

A marine isotope stage 11 coastal Acheulian workshop with associated wood at Amanzi Springs Area 1, South Africa.

机构信息

Palaeoscience, Dept. Archaeology and History, La Trobe University, Melbourne Campus, Bundoora, Victoria, Australia.

The Palaeo-Research Institute, University of Johannesburg, Auckland Park, South Africa.

出版信息

PLoS One. 2022 Oct 20;17(10):e0273714. doi: 10.1371/journal.pone.0273714. eCollection 2022.

Abstract

Amanzi Springs is a series of inactive thermal springs located near Kariega in the Eastern Cape of South Africa. Excavations in the 1960s exposed rare, stratified Acheulian-bearing deposits that were not further investigated over the next 50 years. Reanalysis of the site and its legacy collection has led to a redefined stratigraphic context for the archaeology, a confirmed direct association between Acheulian artefacts and wood, as well as the first reliable age estimates for the site. Thermally transferred optically stimulated luminescence and post-infrared infrared stimulated luminescence dating indicates that the Acheulian deposits from the Amanzi Springs Area 1 spring eye formed during Marine Isotope Stage (MIS) 11 at ~ 404-390 ka. At this time, higher sea levels of ~13-14m would have placed Amanzi Springs around 7 km from a ria that would have formed along what is today the Swartkops River, and which likely led to spring reactivation. This makes the Amanzi Springs Area 1 assemblage an unusual occurrence of a verified late occurring, seaward, open-air Acheulian occupation. The Acheulian levels do not contain any Middle Stone Age (MSA) elements such as blades and points that have been documented in the interior of South Africa at this time. However, a small number of stone tools from the upper layers of the artefact zone, and originally thought of as intrusive, have been dated to ~190 ka, at the transition between MIS 7 to 6, and represent the first potential MSA identified at the site.

摘要

阿玛兹温泉是一系列位于南非东开普省卡里埃加附近的休眠热泉。20 世纪 60 年代的挖掘工作暴露了罕见的、分层的阿舍利石器层,但在接下来的 50 年里,这些地层并没有得到进一步的研究。对该遗址及其遗留物的重新分析导致了对考古学的地层背景的重新定义,确认了阿舍利石器与木材之间的直接联系,以及对该遗址的第一个可靠年代估计。热转移光激发发光和后红外光激发发光测年表明,来自阿玛兹温泉区 1 号泉眼的阿舍利石器层形成于约 40.4-39 万年前的海洋同位素阶段 11(MIS 11)。当时,较高的海平面约为 13-14 米,阿玛兹温泉距离一个可能形成于今天斯沃特科普斯河的河口湾约 7 公里,这可能导致了泉水的重新活跃。这使得阿玛兹温泉区 1 号组合成为一个罕见的验证发生在较晚时期、朝向海洋、露天阿舍利石器时代的遗址。阿舍利石器层没有包含当时在南非内陆已经有记录的中石器时代(MSA)元素,如刀片和尖状器。然而,来自石器层上层的少量石器工具,最初被认为是侵入性的,其年代可以追溯到约 19 万年前,处于 MIS 7 到 6 的过渡期,代表了该遗址首次确定的潜在 MSA 时期。

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