Laboratory of Archaeology and Population in Africa, Anthropology Unit, Department of Genetics and Evolution, University of Geneva, Quai Ernest-Ansermet 30, 1205 Genève, Switzerland.
Laboratory of Physical Geography (LGP), CNRS-UMR 8591, Department of Geography, University Paris-Est Creteil, 1 Place Aristide Briand, 920195 Meudon, France.
J Hum Evol. 2021 May;154:102952. doi: 10.1016/j.jhevol.2021.102952. Epub 2021 Mar 19.
The Ravin Blanc I archaeological occurrence, dated to MIS 5, provides unprecedented data on the Middle Stone Age (MSA) of West Africa since well-contextualized archaeological sites pre-dating MIS 4/3 are extremely rare for this region. The combined approach on geomorphology, phytolith analysis, and OSL date estimations offers a solid framework for the MSA industry comprised in the Ravin Blanc I sedimentary sequence. The paleoenvironmental reconstruction further emphasizes on the local effects of the global increase in moisture characterizing the beginning of the Upper Pleistocene as well as the later shift to more arid conditions. The lithic industry, comprised in the lower part of the sequence and dated to MIS 5e, shows core reduction sequences among which Levallois methods are minor, as well as an original tool-kit composition, among which pieces with single wide abrupt notches, side-scrapers made by inverse retouch, and a few large crudely shaped bifacial tools. The Ravin Blanc I assemblage has neither a chronologically equivalent site to serve comparisons nor a clear techno-typological correspondent in West Africa. However, the industry represents an early MSA technology that could either retain influences from the southern West African 'Sangoan' or show reminiscences of the preceding local Acheulean. A larger-scale assessment of behavioral dynamics at work at the transition period between the Middle to Upper Pleistocene is discussed in view of integrating this new site to the global perception of this important period in the MSA evolutionary trajectories.
拉文布兰克 I 考古遗址的年代可追溯到 MIS5 期,为非洲西部中石器时代(MSA)提供了前所未有的数据,因为在该地区,MIS4/3 之前的史前考古遗址极为罕见。地貌学、植硅石分析和 OSL 日期估计的综合方法为拉文布兰克 I 沉积序列中的 MSA 工业提供了一个坚实的框架。古环境重建进一步强调了全球增湿对当地的影响,这种增湿特征标志着更新世上部的开始,随后又转向更为干旱的条件。石器工业位于序列的下部,年代为 MIS5e,显示出核心减少序列,其中勒瓦娄哇技术较少,工具套件组成也较为原始,包括具有单个宽而突然的缺口的石器、通过反向锐化制成的侧刮器,以及少量大型粗糙的双面工具。拉文布兰克 I 组合既没有与年代相当的遗址可供比较,也没有在西非找到明确的技术类型对应物。然而,该工业代表了一种早期的 MSA 技术,它可能保留了来自西非南部“桑戈安”的影响,或者显示了对前一个本地阿舍利的回忆。在中更新世到上更新世过渡时期的行为动态的更大规模评估是基于将这个新遗址纳入对 MSA 进化轨迹中这个重要时期的全球认知来讨论的。