UMR 7194 HNHP MNHN-CNRS-UPVD, Département Homme et Environnement du Muséum national d'Histoire Naturelle, Institut de Paléontologie Humaine, 1 rue René Panhard, 75013 Paris, France.
UMR 5060 IRAMAT CNRS-Université de Bordeaux, Centre de Recherche en Physique Appliquée à l'Archéologie, Maison de l'archéologie, 33607 Pessac cedex, France.
J Hum Evol. 2022 Jan;162:103092. doi: 10.1016/j.jhevol.2021.103092. Epub 2021 Nov 25.
Previous studies have suggested that the Lower-to-Middle Paleolithic transition was associated with the earliest Neanderthals, but recent research has established that the oldest Neanderthal fossils and the first signs of their technologies and behavior appear from MIS 11 or possibly earlier. To understand these changes, re-evaluation of the evidence is necessary to determine if this transition corresponds to a progressive evolution rather than abrupt change. Orgnac 3 is a key and appropriate site to study this research context. Located in southern France, it yields a long stratigraphic sequence testifying the evolution of technical and subsistence behaviors of pre-Neanderthal human groups during a Middle Pleistocene interglacial-glacial cycle. In this article, a new chronological framework is provided for the sequence based on results of dating methods applied to various types of geological materials. Speleothems and volcanic minerals, dated in previous studies by U-series and Ar/Ar, respectively, show periods of calcitic crystallization and regional volcanic activity. Other materials, such as heated flints and herbivore teeth, are directly related to evidence of anthropogenic activities and are analyzed in the present work by trapped-charge dating methods such as thermoluminescence and electron spin resonance combined with uranium series (ESR/U-series). The new thermoluminescence and ESR/U-series dates confirm the attribution of the Orgnac 3 stratigraphic sequence to the MIS 10-MIS 8 period and are discussed in relation to paleoenvironmental data derived from bioarchaeological studies. The paleoanthropological levels, including the emergence of Levallois technology, are dated to ca. 275 ka (early MIS 8) and appear coeval to a wet and temperate period recorded locally, the Amargiers interstadial, defined in the regional palynological records. The implications of this reassessed chronology for the archaeological assemblages are discussed in the wider context of behavioral innovations from MIS 11 onward and their establishment in subsequent periods.
先前的研究表明,下-中更新世过渡与最早的尼安德特人有关,但最近的研究已经确定,最古老的尼安德特人化石以及他们的技术和行为的最初迹象出现在 MIS 11 或更早。为了了解这些变化,有必要重新评估证据,以确定这种过渡是否对应于渐进的进化,而不是突然的变化。奥格纳德 3 号遗址是研究这一研究背景的关键和合适地点。该遗址位于法国南部,提供了一个长的地层序列,证明了前尼安德特人类群体在中更新世间冰期-冰期旋回期间技术和生存行为的演变。在本文中,根据应用于各种地质材料的测年方法的结果,为该序列提供了一个新的年代框架。在之前的研究中,分别通过铀系和氩/氩测年方法对洞穴中的矿物质和火山矿物质进行了定年,这些结果显示了方解石结晶和区域性火山活动的时期。其他材料,如加热的燧石和食草动物牙齿,与人类活动的证据直接相关,在本工作中,通过热释光和电子自旋共振与铀系(ESR/U 系列)相结合的俘获电荷测年方法进行了分析。新的热释光和 ESR/U 系列测年结果证实了奥格纳德 3 号地层序列的归属,即 MIS 10-MIS 8 时期,并与生物考古学研究得出的古环境数据进行了讨论。古人类学层,包括勒瓦卢瓦技术的出现,可追溯到约 27.5 万年(早 MIS 8),与当地记录的湿润和温和时期——阿马吉尔斯间冰期同时出现,该时期在区域花粉记录中得到了定义。在更广泛的 MIS 11 及以后的行为创新及其在随后时期的建立的背景下,讨论了重新评估的年代学对考古组合的影响。