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Last Interglacial (MIS 5) ungulate assemblage from the Central Iberian Peninsula The Camino Cave (Pinilla del Valle, Madrid, Spain)》.pdf
Palaeogeography, Palaeoclimatology, Palaeoecology 374 (2013) 327–337 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.el /l oc ate/ pal aeo Last Interglacial (MIS 5) ungulate assemblage from the Central Iberian Peninsula: The Camino Cave (Pinilla del Valle, Madrid, Spain) Diego J. Álvarez-Lao a,⁎, Juan L. Arsuaga b, c, Enrique Baquedano d, Alfredo Pérez-González e a Área de Paleontología, Departamento de Geología, Universidad de Oviedo, C/Jesús Arias de Velasco, s/n, 33005 Oviedo, Spain b Centro Mixto UCM-ISCIII de Evolución y Comportamiento Humanos, C/Sinesio Delgado, 4, 28029 Madrid, Spain c Departamento de Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, Ciudad Universitaria, 28040 Madrid, Spain d Museo Arqueológico Regional de la Comunidad de Madrid, Plaza de las Bernardas, s/n, 28801-Alcalá de Henares, Madrid, Spain e Centro Nacional de Investigación sobre la Evolución Humana (CENIEH), Paseo Sierra de Atapuerca, s/n, 09002 Burgos, Spain a r t i c l e i n f o a b s t r a c t Article history: The fossil assemblage from the Camino Cave, corresponding to the late MIS 5, constitutes a key record to un- Received 2 November 2012 derstand the faunal composition of Central Iberia during the last Interglacial. Moreover, the largest Iberian Received in revised form 21 January 2013 fallow deer fossil population was recovered here. Other ungulate species present at this assemblage include Accepted 31 January 2013 red deer, roe deer, aurochs, chamois, wild boar, horse and steppe rhinoceros; carnivores and Neanderthals Available o
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