纳米比亚纳米布沙海纳拉贝布更新世晚期考古遗址的地貌演变和水文特征

IF 2.9 Q2 GEOGRAPHY, PHYSICAL Quaternary Science Advances Pub Date : 2024-04-28 DOI:10.1016/j.qsa.2024.100190
Abi Stone , George Leader , Dominic Stratford , Theodore Marks , Kaarina Efraim , Rachel Bynoe , Rachel Smedley , Andrew Gunn , Eugene Marais
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引用次数: 0

摘要

众所周知,纳米比亚的纳米布沙海(Namib Sand Sea,NSS)保存着种类繁多的更新世考古遗址。然而,该地区的中石器时代(MSA)遗址很少受到系统调查,有关年代学和技术组织的基本问题仍未解决。在此,我们考察了纳拉贝(Narabeb),这是一处露天的中石器时代地表遗址,暴露在距北部南沙群岛北部 30 千米的沙丘间平原上。20 世纪 70 年代首次对 Narabeb 进行了记录,随后本团队成员于 2021 年和 2022 年对其进行了重新考察。石器技术分析结合遗址的地貌描述、细粒度水成沉积物的古环境解释,以及纳拉贝岩盘北部和南部地点的发光年龄,使我们首次了解了人类与环境的相互作用,并估算了北高亚地区晚中新世和晚更新世的年代。此外,我们还对风化线性沙丘的堆积和延伸采用了定量方法,以探索该地点景观发展的可能情景,从而更好地了解影响该地区的前水道。新的年代学表明,该地点在MIS 7/6过渡期或其后,以及在MIS 6末期至MIS 5早期或其后,都有积水。我们的研究结果为在南部非洲这一独特的环境中对早期人类的适应策略进行更大规模的区域性分析奠定了基础。
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Landscape evolution and hydrology at the Late Pleistocene archaeological site of Narabeb in the Namib Sand Sea, Namibia

The Namib Sand Sea (NSS) in Namibia is known to preserve a wide variety of Pleistocene-age archaeological sites. However, few Middle Stone Age (MSA) sites in this region have been systematically investigated and basic questions around chronology and technological organization remain open. Here we examine Narabeb, an open air MSA surface site exposed in an interdune pan, ∼30 km into the northern NSS. Narabeb was first documented in the 1970s, and then re-examined in 2021 and 2022 by members of this team. Lithic technological analysis combined with a geomorphological description of the site, palaeoenvironmental interpretation of fine-grain water-lain sediments, and luminescence ages from northern and southern locations on the Narabeb pan provide some of the first understanding of human-environmental interactions and estimates of chronology from the later-Middle and Late Pleistocene in the NSS. In addition, we apply a quantitative approach to aeolian linear dune accumulation and extension to explore possible scenarios for landscape development at this site, in order to better understand the former water course(s) affecting the area. The new chronology suggests this site contained standing water at, or just after, the MIS 7/6 transition, and again at, or just after, the end of MIS 6 into early MIS 5. The timing of greater phases of water availability have some overlap with the speleothem growth record at Rössing Cave, situated ∼90 km north of the NSS (and ∼135 km north of Narabeb). Our results provide the foundation for larger, regional-scale analyses of early human adaptive strategies in this unique environment within Southern Africa.

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来源期刊
Quaternary Science Advances
Quaternary Science Advances Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
4.00
自引率
13.30%
发文量
16
审稿时长
61 days
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