Identifier: imarina:6386849
Authors:
Chacón Navarro, María Gema / FERNANDEZ LASO, M.CRISTINA / García-Antón Trassierra, Ma. Dolores / Rivals, Florent Joseph Louis
Abstract:
© Springer Science+Business Media B.V. 2011. The Abric Romaní site is located in the northeast Iberian Peninsula, 50 km from Barcelona 317 m above sea level, in a travertine cliff on the right bank of the Anoia river, which is a tributary of the Llobregat river. This river passes by the Capellades locality, forming a narrow gorge known as “Cinglera del Capelló”. This corridor crosses the mountain range “Cordillera Prelitoral”, and is considered as a natural passage between the inland and coastal Catalonia regions. This situation provides the possibility to exploit a great variety of biotopes. The site yielded an important and complete stratigraphic sequence of European Middle Paleolithic. Fifteen archeological levels have been excavated until today, which appear as thin layers between sterile travertine platforms. This sequence has been dated by U-series between 70 and 40 ka BP, except for the uppermost level, which is attributed to the Early Upper Paleolithic. Pollen analyses have revealed five climatic phases, ranging from the milder conditions at the bottom to an interstadial climate at the top, correlated with the Hengelo interstadial. It is, consequently, a key site for human behavioral studies among Neanderthal groups. This paper presents the results of studies on resource procurements, lithics and animals and on the territory used by Neanderthal groups, through the example of level M dated around 55 ka BP. The results of the lithic analysis and faunal assemblages suggest that the resource procurement and management is focused on a local and semi-local exploitation in a geographic area of about 20 km around the rock-shelter.