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A context for the last Neandertals of interior Iberia: Los Casares cave revisited.

Manuel Alcaraz-CastañoJavier Alcolea-GonzálezMartin KehlRosa-María AlbertJavier Baena-PreyslerRodrigo de Balbín-BehrmannFelipe CuarteroGloria Cuenca-BescósFernando Jiménez-BarredoJosé-Antonio López-SáezRaquel PiquéDavid Rodríguez-AntónJosé YravedraGerd-Christian Weniger
Published in: PloS one (2017)
The sediment sequence reveals a mostly in situ archeological deposit containing evidence of both Neandertal activity and carnivore action in level c, dated to 44,899-42,175 calendar years ago. This occupation occurred during a warm and humid interval of Marine Isotopic Stage 3, probably correlating with Greenland Interstadial 11, representing one of the latest occurrences of Neandertals in the Iberian interior. However, overlying layer b records a deterioration of local environments, thus providing a plausible explanation for the abandonment of the site, and perhaps for the total disappearance of Neandertals of the highlands of inland Iberia during subsequent Greenland Stadials 11 or 10, or even Heinrich Stadial 4. Since layer b provided very few signs of human activity and no reliable chronometric results, and given the scarce chronostratigrapic evidence recorded so far for this period in interior Iberia, this can only be taken as a working hypothesis to be tested with future research. Meanwhile, 42,000 calendar years ago remains the most plausible date for the abandonment of interior Iberia by Neandertals, possibly due to climate deterioration. Currently, a later survival of this human species in Iberia is limited to the southern coasts.
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