Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/321
Item metadata
Title: Neandertal roots: cranial and chronological evidence from Sima de los Huesos
Authors: Arsuaga, Juan Luis
Martínez, Ignacio
Arnold, Lee J.
Aranburu Artano, Arantza
Gracia-Téllez, Ana
Sharp, Warren D.
Quam, Rolf M.
Falguères, Christophe
Pantoja-Pérez, Ana
Bischoff, James L.
Poza-Rey, Eva María
Parés, Josep María
Carretero Díaz, José Miguel
Demuro, Martina
Lorenzo Merino, Carlos
Sala, Nohemi
Martinón-Torres, María
García García, Nuria
Alcázar de Velasco, Almudena
Cuenca Bescós, Gloria
Gómez-Olivencia, Azier
Moreno García, Davinia
Pablos Fernández, Adrián
Shen, Chuan-Chou
Rodríguez, Laura
Ortega Martínez, Ana Isabel
García-González, Rebeca
Bonmatí, Alejandro
Bermúdez de Castro, José María
Carbonell, Eudald
Issue Date: Jun-2014
Publisher: American Association for the Advancement of Science
Citation: Science, 2014, 344 (6190), 1358-1363
Abstract: Seventeen Middle Pleistocene crania from the Sima de los Huesos site (Atapuerca, Spain) are analyzed, including seven new specimens. This sample makes it possible to thoroughly characterize a Middle Pleistocene hominin paleodeme and to address hypotheses about the origin and evolution of the Neandertals. Using a variety of techniques, the hominin-bearing layer could be reassigned to a period around 430,000 years ago. The sample shows a consistent morphological pattern with derived Neandertal features present in the face and anterior vault, many of which are related to the masticatory apparatus. This suggests that facial modification was the first step in the evolution of the Neandertal lineage, pointing to a mosaic pattern of evolution, with different anatomical and functional modules evolving at different rates.
URI: http://hdl.handle.net/20.500.12136/321
ISSN: 0036-8075
1095-9203
DOI: 10.1126/science.1253958
metadata.dc.relation.publisherversion: https://doi.org/10.1126/science.1253958
Type: Article
Appears in Collections:Paleobiología
Geocronología y Geología



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