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Your path led trough the sea ... The emergence of Neolithic in Sardinia and Corsica

机译:您的路径引领了大海的低谷。新石器时代在撒丁岛和科西嘉岛的出现

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The emergence of Neolithic in Sardinia and Corsica has more and more the aspect of a sharp rupture that led to the first permanent occupation of the islands through a process of diffuse and rapid territorialization. To date, any evidence of contiguity is still lacking between first Neolithic implantations and last Mesolithic frequentations that stretch sporadically over more than two millennia, until the 8.2 kyear cold climatic event. Besides, Mesolithic-Neolithic discontinuity is proved not only archaeologically, on the grounds of stratigraphy, settlement strategies, and technological systems. Indeed, new mitochondrial DNA genome sequences from Mesolithic Sardinia provide evidence of a substantial diversity between the two populations. The earliest stages (scouting phase) of Neolithic colonization of the islands are scarcely documented thus far, even if some clues would place them consistently in the flow of the Neolithic expansion towards the western Mediterranean. Around the central centuries of the 6th millennium cal BC, the following step (consolidation phase) corresponds to the formation and spread of the Cardial impressed ware facies along the coastal belt of the central and north Tyrrhenian shore. Since then, both Sardinia-Corsica and the Tyrrhenian strands opposite to this region reveal an almost symmetrical and synchronous rhythm of evolution. In the last centuries of the 6th millennium cal BC, new influences coming from the North of the Italian mainland, possibly through the mediation of the Tyrrhenian Linear Carved ware facies, acted as a push factor towards the recombination of the shared traditional traits into new original cultures. In the two islands, at the end of this trajectory, the process of neolithization was almost accomplished and the evolution of Neolithic cultures, although interlinked, went on separately afterwards. (C) 2018 Elsevier Ltd and INQUA. All rights reserved.
机译:撒丁岛和科西嘉岛的新石器时代的出现越来越多地出现了急剧破裂的情况,这导致该岛通过扩散和迅速地域化而首次被永久性占领。迄今为止,在新石器时代的首次植入和中石器时代的后遗症散布超过两千年直到8.2 kyear的寒冷气候事件之前,仍缺乏任何连续性证据。此外,不仅从考古学上,根据地层学,沉降策略和技术系统,还证明了中石器—新石器时代的不连续性。实际上,来自中石器撒丁岛的新线粒体DNA基因组序列提供了这两个种群之间实质性多样性的证据。迄今为止,几乎没有文献记载该岛的新石器时代殖民化的最早阶段(侦察阶段),即使有一些线索使它们始终处于新石器时代向地中海西部扩张的过程中。在公元前6世纪的中部世纪左右,接下来的步骤(巩固阶段)对应于沿第勒尼安河中北部和北部沿海地区的Cardial印相相的形成和扩散。从那时起,撒丁岛-科西嘉岛和与该区域相对的第勒尼安链都显示出几乎对称且同步的进化节奏。在公元前六千年的最后几个世纪中,来自意大利大陆北部的新影响,可能是通过第勒尼安线性刻画相的介导,成为将共享的传统特征重组为新的原始特征的推动因素。文化。在这两个岛上,在这条轨迹的尽头,新石器时代的过程几乎完成了,新石器时代的文化虽然相互联系,但是其后分别发展。 (C)2018爱思唯尔有限公司和INQUA。版权所有。

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