Department of Geosciences, Prehistory and Archaeological Sciences Research Unit, Eberhard Karls University of Tübingen, Tübingen, Germany.
Dipartimento di Beni Culturali, Università di Bologna, Via degli Ariani 1, 48121, Ravenna, Italy.
Sci Rep. 2024 Jun 4;14(1):12783. doi: 10.1038/s41598-024-59896-6.
The Aurignacian is the first European technocomplex assigned to Homo sapiens recognized across a wide geographic extent. Although archaeologists have identified marked chrono-cultural shifts within the Aurignacian mostly by examining the techno-typological variations of stone and osseous tools, unraveling the underlying processes driving these changes remains a significant scientific challenge. Scholars have, for instance, hypothesized that the Campanian Ignimbrite (CI) super-eruption and the climatic deterioration associated with the onset of Heinrich Event 4 had a substantial impact on European foraging groups. The technological shift from the Protoaurignacian to the Early Aurignacian is regarded as an archaeological manifestation of adaptation to changing environments. However, some of the most crucial regions and stratigraphic sequences for testing these scenarios have been overlooked. In this study, we delve into the high-resolution stratigraphic sequence of Grotta di Castelcivita in southern Italy. Here, the Uluzzian is followed by three Aurignacian layers, sealed by the eruptive units of the CI. Employing a comprehensive range of quantitative methods-encompassing attribute analysis, 3D model analysis, and geometric morphometrics-we demonstrate that the key technological feature commonly associated with the Early Aurignacian developed well before the deposition of the CI tephra. Our study provides thus the first direct evidence that the volcanic super-eruption played no role in this cultural process. Furthermore, we show that local paleo-environmental proxies do not correlate with the identified patterns of cultural continuity and discontinuity. Consequently, we propose alternative research paths to explore the role of demography and regional trajectories in the development of the Upper Paleolithic.
阿舍利技术期是第一个在广泛地理范围内被认定为智人物种所拥有的欧洲技术复合体。尽管考古学家已经通过研究石器和骨制工具的技术类型变化识别出阿舍利技术期内的显著的年代文化转变,但解开驱动这些变化的潜在过程仍然是一个重大的科学挑战。例如,学者们假设坎帕尼亚火山灰(CI)超级喷发以及与海因里希事件 4 开始相关的气候恶化对欧洲觅食群体产生了重大影响。从原始阿舍利技术期到早期阿舍利技术期的技术转变被认为是适应不断变化的环境的考古学表现。然而,一些对于检验这些假说最为关键的地区和地层序列却被忽视了。在这项研究中,我们深入研究了意大利南部 Grotta di Castelcivita 的高分辨率地层序列。在这里,乌利赞文化之后是三个阿舍利技术层,被 CI 的喷发单元所封闭。我们采用了一系列全面的定量方法,包括属性分析、3D 模型分析和几何形态测量学,证明了与早期阿舍利技术期通常相关的关键技术特征是在 CI 火山灰沉积之前就已经发展起来的。因此,我们的研究提供了第一个直接证据,表明火山超级喷发在此文化过程中没有发挥作用。此外,我们还表明,当地古环境指标与所确定的文化连续性和不连续性模式没有相关性。因此,我们提出了替代研究路径,以探索人口统计学和区域轨迹在旧石器时代晚期发展中的作用。