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Bedtime for the Middle Stone Age: Land Use, Strategic Foraging, and Lithic Technology at the End of the Pleistocene in the Namib Desert, Namibia

机译:中石器时代的就寝时间:纳米比亚纳米布沙漠更新世末期的土地利用,战略觅食和锂技术

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摘要

Scholars of the Late Pleistocene in Southern Africa have recently sought to develop models explaining long-term variation between Middle Stone Age and Late Stone Age assemblages in terms of variability between "macrolithic" vs. "microlithic" toolmaking systems associated with shifts in hunter-gatherer ecology and land use patterns. While it has often proven extremely difficult to actually test many models, recently developed methods allow us to do so in novel ways. In this dissertation, I use new archaeological data from excavations of two sites in the Namib Desert, as well as new approaches to sourcing lithic artifacts to examine the hypothesis that contrasts between terminal Pleistocene (ca. 15-20 ka BP) and early Holocene (ca. 6-12 ka BP) occupation phases at the two sites represent adaptive responses primarily driven by changes in fluvial regimes and the resource productivity of riparian corridors. Analyzing the lithic assemblage compositions and locating probable source areas for raw materials suggests that terminal Pleistocene groups likely centered land use strategies more toward upland areas east of the study sites and periodically followed broad riparian corridors into the desert itself. Early Holocene groups expanded their ranges and more intensively targeted resources on the open desert plains, dunes, and beaches of the coastal lowlands. My results suggest environmental change may be partially responsible for driving this shift, but new data and methodological tools are needed to address factors like fluctuations in regional population size that may have been driving shifts in the late Pleistocene record of this unique region of Southern Africa.
机译:南部非洲晚更新世的学者们最近寻求开发模型来解释中石器时代和石器时代后期组合之间的长期变化,该模型涉及与猎人-采集者的转变相关的“巨石”与“微石”工具制造系统之间的差异。生态和土地利用方式。尽管事实证明通常很难实际测试许多模型,但是最近开发的方法使我们能够以新颖的方式进行测试。在这篇论文中,我使用了纳米布沙漠两个地点发掘的新考古数据,以及寻找石器物的新方法,以检验晚更新世(约15-20 ka BP)与早期全新世(大约6-12 ka BP)在两个地点的占领阶段代表了适应性反应,主要是由河流形态和河岸走廊资源生产力的变化驱动的。对石块组合物成分进行分析并确定原材料的可能来源区域表明,更新世末期群可能将土地利用策略更多地集中在研究地点以东的高地地区,并定期沿着宽阔的河岸走廊进入沙漠本身。早期全新世组织扩大了范围,将资源更加集中在沿海低地的开阔沙漠平原,沙丘和海滩上。我的研究结果表明,环境变化可能是造成这种转变的部分原因,但是需要新的数据和方法论工具来解决诸如区域人口规模波动等因素,这些因素可能一直在推动这一非洲南部独特地区的晚更新世记录发生变化。

著录项

  • 作者

    Marks, Theodore Pearson.;

  • 作者单位

    The University of Iowa.;

  • 授予单位 The University of Iowa.;
  • 学科 Archaeology.;African history.;South African studies.
  • 学位 Ph.D.
  • 年度 2018
  • 页码 277 p.
  • 总页数 277
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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