UMR5608 TRACES, CNRS, Toulouse Jean-Jaurès University, Toulouse, France.
PLoS One. 2021 Mar 3;16(3):e0246964. doi: 10.1371/journal.pone.0246964. eCollection 2021.
In the Western Mediterranean, the Neolithic mainly developed and expanded during the sixth millennium BCE. In these early phases, it generally spread through the displacement of human groups, sometimes over long distances, as shown, for example, by the Impressa sites documented on the northern shores. These groups then settled new territories which they gradually appropriated and exploited. The question of their potential interaction with groups of Late Mesolithic hunter-gatherers living in the area prior to their arrival is therefore crucial. Were their encounters based on conflict and resistance or, on the contrary, on exchange and reciprocity? Many hypotheses have been put forward on this matter and many papers written. Before we can consider these potential interactions however, we must first ascertain that these different human groups really did meet-an implicit assumption in all these studies, which is, in reality, much less certain than one might think. The population density of the Late Mesolithic groups varied greatly throughout the Mediterranean, and it is possible that some areas were relatively devoid of human presence. Before any Neolithization scenarios can be considered, we must therefore first determine exactly which human groups were present in a given territory at a given time. The precise mapping of sites and the chronological modeling of their occupation enriches our understanding of the Neolithization process by allowing high-resolution regional models to be developed, which alone can determine the timing of potential interactions between Mesolithic and Neolithic groups. Various international research programs have recently produced several hundred new radiocarbon dates, based on selected samples from controlled contexts. The geochronological modelling of these data at the scale of the Western Mediterranean shows contrasting situations, probably related to different social and environmental processes. These results suggest that we should consider a varied range of Neolithization mechanisms, rather than uniform or even binary models.
在地中海西部,新石器时代主要在公元前 6000 年发展和扩张。在这些早期阶段,它通常通过人类群体的迁移传播,有时距离很远,例如在 Impressa 遗址的记录中就可以看到,这些遗址位于北部海岸。这些群体随后在新的领土上定居,并逐渐占有和开发这些领土。因此,他们与在这些群体到达之前居住在该地区的晚期旧石器时代狩猎采集者群体之间是否存在潜在的互动,是至关重要的。他们的相遇是基于冲突和抵制,还是相反,基于交流和互惠?关于这个问题已经提出了许多假设,并写了很多论文。然而,在我们能够考虑这些潜在的相互作用之前,我们必须首先确定这些不同的人类群体确实相遇了——这是所有这些研究中隐含的假设,而实际上,这一假设远不如人们想象的那么确定。地中海地区晚期旧石器时代群体的人口密度差异很大,有些地区可能相对缺乏人类的存在。在考虑任何新石器化方案之前,我们必须首先确定在特定时间特定地区存在哪些人类群体。通过对遗址进行精确的绘制,并对其居住情况进行年代建模,我们可以更好地了解新石器化过程,因为这可以开发出高分辨率的区域模型,从而确定旧石器时代和新石器时代群体之间潜在相互作用的时间。最近,各种国际研究计划根据选定的受控环境样本,产生了数百个新的放射性碳日期。对这些数据在地中海西部的地质年代建模显示出对比的情况,这可能与不同的社会和环境过程有关。这些结果表明,我们应该考虑各种不同的新石器化机制,而不是单一的或甚至是二元的模型。