Research Laboratory for Archaeology and the History of Art, University of Oxford, Dyson Perrins Building, South Parks Road, Oxford OX1 3QY, UK.
Centre for Archaeological Science, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, NSW 2522, Australia.
J Hum Evol. 2014 Jan;66:39-63. doi: 10.1016/j.jhevol.2013.10.001. Epub 2013 Dec 12.
The 1950s excavations by Charles McBurney in the Haua Fteah, a large karstic cave on the coast of northeast Libya, revealed a deep sequence of human occupation. Most subsequent research on North African prehistory refers to his discoveries and interpretations, but the chronology of its archaeological and geological sequences has been based on very early age determinations. This paper reports on the initial results of a comprehensive multi-method dating program undertaken as part of new work at the site, involving radiocarbon dating of charcoal, land snails and marine shell, cryptotephra investigations, optically stimulated luminescence (OSL) dating of sediments, and electron spin resonance (ESR) dating of tooth enamel. The dating samples were collected from the newly exposed and cleaned faces of the upper 7.5 m of the ∼14.0 m-deep McBurney trench, which contain six of the seven major cultural phases that he identified. Despite problems of sediment transport and reworking, using a Bayesian statistical model the new dating program establishes a robust framework for the five major lithostratigraphic units identified in the stratigraphic succession, and for the major cultural units. The age of two anatomically modern human mandibles found by McBurney in Layer XXXIII near the base of his Levalloiso-Mousterian phase can now be estimated to between 73 and 65 ka (thousands of years ago) at the 95.4% confidence level, within Marine Isotope Stage (MIS) 4. McBurney's Layer XXV, associated with Upper Palaeolithic Dabban blade industries, has a clear stratigraphic relationship with Campanian Ignimbrite tephra. Microlithic Oranian technologies developed following the climax of the Last Glacial Maximum and the more microlithic Capsian in the Younger Dryas. Neolithic pottery and perhaps domestic livestock were used in the cave from the mid Holocene but there is no certain evidence for plant cultivation until the Graeco-Roman period.
20 世纪 50 年代,查尔斯·麦克伯尼(Charles McBurney)在利比亚东北部沿海的大型喀斯特洞穴哈瓦法提(Haua Fteah)进行了挖掘,揭示了人类在此深度连续居住的历史。此后,大多数关于北非史前史的研究都参考了他的发现和解释,但该遗址考古和地质序列的年代学一直基于非常早期的年代测定。本文报告了作为该遗址新工作的一部分而开展的一项综合多方法测年计划的初步结果,该计划涉及对木炭、陆生蜗牛和海洋贝壳进行放射性碳测年、隐微喷发物调查、对沉积物进行光释光(OSL)测年以及对牙齿珐琅质进行电子自旋共振(ESR)测年。测年样本取自新暴露和清理过的麦克伯尼深沟(McBurney Trench)上 7.5 米高的表面,深沟深约 14 米,其中包含他确定的七个主要文化阶段中的六个。尽管存在沉积物运移和再作用的问题,但使用贝叶斯统计模型,新的测年计划为在地层序列中确定的五个主要岩石地层单元以及主要的文化单元建立了一个稳健的框架。麦克伯尼在他的勒瓦娄哇-莫斯特文化阶段(Levalloiso-Mousterian phase)底部附近的第 XXXIII 层发现的两块具有解剖学意义的现代人下颌骨的年代现在可以估计在 73 到 65 千年前(几千年前),置信水平为 95.4%,在海洋同位素阶段(MIS)4 内。麦克伯尼的第 XXV 层与上旧石器时代的达班刀片工业有关,与坎帕尼安火山灰层有明确的地层关系。末次冰盛期之后发展起来的细石器奥兰尼技术和在新仙女木期更细的卡普萨。新石器时代的陶器,也许还有家养牲畜,从中石器时代开始就在洞穴中使用,但直到希腊罗马时期才有确凿的证据表明有植物栽培。