4.2 Article

ESR/U-series chronology of the Neanderthal occupation layers at Galeria de las Estatuas (Sierra de Atapuerca, Spain)

Journal

QUATERNARY GEOCHRONOLOGY
Volume 72, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.quageo.2022.101342

Keywords

ESR/U-series dating; Neanderthal; Late pleistocene; Atapuerca site complex; Iberian peninsula

Funding

  1. Ministerio de Ciencia e Innovacion - Agencia Estatal de Investigacion [NSFC 41877430, PGC 2018-093925-B-C31, PGC 2018-093925-B-C32]
  2. Junta de Castilla y Le on
  3. Fundacion Atapuerca
  4. Jose Castillejo Mobility Fellowship [PGC 2018-093925-B-C33]
  5. MNHN
  6. Normal Nanjing University [CAS18/00404]

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The Galeria de las Estatuas is a Mousterian site located in the karstic system of Sierra de Atapuerca, Spain. It has yielded a large number of lithic artefacts, faunal remains, Neanderthal foot phalanx, and mitochondrial and nuclear DNA. With various dating methods, the site has been dated to approximately 45ka cal BP, and the sediment containing Mousterian lithic artefacts, faunal, and human remains is estimated to have been deposited during the second part of MIS5.
The Galeria de las Estatuas is a Mousterian site located within the Cueva Mayor-Cueva del Silo karstic system at the Sierra de Atapuerca (Burgos, Spain). This site is characterised by an important Upper Pleistocene strati graphic sequence in which a large number of lithic artefacts exhibiting clear Mousterian affinities and a rich assemblage of faunal remains have been found. Additionally, this site has yielded a foot phalanx of a clear Neanderthal affinities and its sediment has yielded Neanderthal mitochondrial and nuclear DNA.Two test pits, GE-I and GE-II, have been excavated since 2008 which have been divided in 5 and 2 lithostratigraphical units, respectively. A minimum age of 45 ka cal BP for this site was obtained by radiocarbon dating in GE-II. This chronology was refined using single-grain Optically Stimulated Luminescence (OSL: 80-112 ka in GE-I and 70-79 ka in GE-II) and single-grain thermally transferred OSL (TT-OSL). Although in all case TT-OSL ages were systematically older than their single-grain counterparts. The detrital sequence is sealed by a flow stone whose base is dated to 53.7 +/- 3.5 ka cal BP using U-series dating.In order to better constrain the age of this site, nine herbivorous teeth were collected from the whole sedimentary sequence to be dated by the ESR/U-series dating method though only seven provided modelled ages. Six of them were collected from levels 2 to 5 of the GE-I test pit while the last tooth was taken from level 2 of the GE II test pit. Our results, ranging between 80 and 110 ka, are in agreement with those obtained by single grain TTOSL and suggest that the sedimentological levels containing Mousterian lithic artefacts and faunal and human remains began to be deposited during the second part of the MIS5. These results fill a temporal gap in the chronology of the Atapuerca sites for which no contemporary MIS5 date was obtained until recently.

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