Institute of Human Origins, School of Human Evolution and Social Change, Arizona State University, Tempe, AZ 85287-2402, USA.
J Hum Evol. 2010 Sep-Oct;59(3-4):425-43. doi: 10.1016/j.jhevol.2010.07.011.
Genetic and anatomical evidence suggests that Homo sapiens arose in Africa between 200 and 100ka, and recent evidence suggests that complex cognition may have appeared between ~164 and 75ka. This evidence directs our focus to Marine Isotope Stage (MIS) 6, when from 195-123ka the world was in a fluctuating but predominantly glacial stage, when much of Africa was cooler and drier, and when dated archaeological sites are rare. Previously we have shown that humans had expanded their diet to include marine resources by ~164ka (±12ka) at Pinnacle Point Cave 13B (PP13B) on the south coast of South Africa, perhaps as a response to these harsh environmental conditions. The associated material culture documents an early use and modification of pigment, likely for symbolic behavior, as well as the production of bladelet stone tool technology, and there is now intriguing evidence for heat treatment of lithics. PP13B also includes a later sequence of MIS 5 occupations that document an adaptation that increasingly focuses on coastal resources. A model is developed that suggests that the combined richness of the Cape Floral Region on the south coast of Africa, with its high diversity and density of geophyte plants and the rich coastal ecosystems of the associated Agulhas Current, combined to provide a stable set of carbohydrate and protein resources for early modern humans along the southern coast of South Africa during this crucial but environmentally harsh phase in the evolution of modern humans. Humans structured their mobility around the use of coastal resources and geophyte abundance and focused their occupation at the intersection of the geophyte rich Cape flora and coastline. The evidence for human occupation relative to the distance to the coastline over time at PP13B is consistent with this model.
遗传和解剖学证据表明,智人起源于非洲,时间在 20 万至 10 万年前,最近的证据表明,复杂认知可能出现在约 16.4 万至 7.5 万年前。这些证据将我们的注意力引向海洋同位素阶段(MIS)6,在这个阶段,从 19.5 万至 12.3 万年前,世界处于波动但主要是冰川的阶段,当时非洲的大部分地区更加凉爽和干燥,有日期记载的考古遗址也很少。此前,我们已经表明,人类通过在南非南部海岸的顶点洞 13B(PP13B),将其饮食扩大到包括海洋资源,时间大约在 16.4 万年前(±12 千年前),这可能是对这些恶劣环境条件的一种反应。相关的物质文化记录了早期对颜料的使用和改造,可能是为了象征性行为,以及薄片石器技术的生产,现在还有令人着迷的证据表明石器经过了热处理。PP13B 还包括一个稍晚的 MIS 5 居住序列,记录了一种越来越关注沿海资源的适应。提出了一个模型,该模型表明,非洲南部海岸的开普植物区系的丰富度,加上其球茎植物的多样性和密度以及相关的厄加勒斯洋流的丰富沿海生态系统,共同为南非南部沿海的早期现代人类提供了一套稳定的碳水化合物和蛋白质资源,在现代人类进化的这个关键但环境恶劣的阶段。人类围绕着利用沿海资源和球茎植物的丰富度来组织他们的流动性,并将他们的居住点集中在富含球茎植物的开普植物区系和海岸线的交叉点上。PP13B 上人类居住点相对于海岸线的距离随时间的变化的证据与该模型一致。