2014
DOI: 10.1016/j.jhevol.2013.12.017
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The chronology of the earliest Upper Palaeolithic in northern Iberia: New insights from L'Arbreda, Labeko Koba and La Viña

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Cited by 142 publications
(94 citation statements)
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“…Recently some of the late dates of Mousterian assemblages in this region have been discussed (Wood et al, 2013) but, roughly, it can be said that there is some persistence of Neandertal groups after ca. 40 ka BP, after the first Upper Paleolithic assemblages in the northern Iberian Peninsula (Martínez-Moreno et al, 2010;Wood et al, 2014).…”
Section: Iberian Peninsula Late Middle Paleolithicmentioning
confidence: 99%
“…Recently some of the late dates of Mousterian assemblages in this region have been discussed (Wood et al, 2013) but, roughly, it can be said that there is some persistence of Neandertal groups after ca. 40 ka BP, after the first Upper Paleolithic assemblages in the northern Iberian Peninsula (Martínez-Moreno et al, 2010;Wood et al, 2014).…”
Section: Iberian Peninsula Late Middle Paleolithicmentioning
confidence: 99%
“…In contrast to the high number of sites, the chronological framework for the Middle Palaeolithic is, at least in parts, fragile. Indeed, the latest/ transitional phase towards the Upper Palaeolithic has been increasingly studied within the last years (Zilhão, 2006;Wood et al, 2013;Wood et al, 2014). The time before though has gained only minor interest.…”
Section: Southern Iberiamentioning
confidence: 99%
“…En el contexto más inmediato, el extremo occidental cantábrico, tenemos cuatro dataciones radiocarbónicas asignables, sin dudas, al Gravetiense procedentes de La Viña, Sopeña y Cueto de la Mina. El paralelo entre la del nivel IX de La Viña, 24640±190 BP (Wood et al 2014), y las obtenidas en el nivel Co.B.6 de Coímbre debe matizarse, dado que la primera se realizó a través del método de ultrafiltración, donde el tratamiento previo de la muestra y el propio método difieren de los empleados en las dataciones de Coímbre. La fecha del nivel II de Sopeña, 24300±170 BP, procede de un contexto estratigráfico alterado (Pinto et al 2012) mientras la de su nivel X, 23550±180 BP, tiene una correspondencia similar, aunque ligeramente más alejada en el tiempo.…”
Section: Dataciones C14 Ams Y Posición Cronoestratigráficaunclassified