Aureli Daniele, Contardi Antonio, Giaccio Biagio, Jicha Brian, Lemorini Cristina, Madonna Sergio, Magri Donatella, Marano Federica, Milli Salvatore, Modesti Valerio, Palombo Maria Rita, Rocca Roxane
Dipartimento di Scienze Fisiche, della Terra e dell'Ambiente, U.R. Preistoria e Antropologia, Università di Siena, Via Laterina 8, 53100, Siena, Italy; UMR 7041- ArScAn équipe AnTET, 21 allée de l'Université F-92023, Nanterre, Paris, France.
Museo Civico A. Klitsche De la Grange, Palazzo Camerale, Piazza della Repubblica, 29, 00051, Allumiere, Roma, Italy.
PLoS One. 2015 Apr 21;10(4):e0124498. doi: 10.1371/journal.pone.0124498. eCollection 2015.
The Ficoncella site in northern Latium (Italy) represents a unique opportunity to investigate the modalities of a short occupation in an alluvial setting during the Lower Palaeolithic. The small excavation area yielded a lithic assemblage, a carcass of Palaeoloxodon antiquus, and some other faunal remains. The main objectives of the study are to better characterize the depositional context where the Palaeoloxodon and the lithic assemblage occur, and to evaluate with greater precision the occupation dynamics. A 25 m-long well was drilled just above the top of the terrace of the Ficoncella site and faunal and lithic remains were analyzed with current and innovative techniques. The archaeological site contains floodplain deposits as it is located next to a small incised valley that feeds into a larger valley of the Mignone River. A tephra layer capping the site is 40Ar/39Ar dated to 441± 8 ka. Collectively, the geochronologic, tephrochronologic and geologic data, suggest the site was occupied during MIS 13. The new results should prompt further research at Ficoncella in order to improve our understanding of the dynamics of human settlement in Europe during the Early to Middle Pleistocene.
意大利拉齐奥北部的菲孔切拉遗址为研究旧石器时代早期冲积环境中的短期居住模式提供了一个独特的机会。这片小发掘区域出土了一批石器、一具古老象的遗骸以及其他一些动物化石。该研究的主要目的是更全面地描述古老象和石器组合所处的沉积环境,并更精确地评估居住动态。在菲孔切拉遗址阶地顶部上方钻了一口25米深的竖井,并运用现有及创新技术对动物化石和石器进行了分析。该考古遗址包含洪泛平原沉积物,因为它位于一条流入米尼奥内河较大河谷的小深切谷旁。覆盖该遗址的一层火山灰经40Ar/39Ar测年,年代为441±8 ka。综合来看,地质年代学、火山灰年代学和地质数据表明该遗址在海洋同位素阶段13期间有人居住。这些新结果应促使对菲孔切拉进行进一步研究,以增进我们对欧洲早更新世至中更新世人类定居动态的理解。