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| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Duval, Mathieu | - |
| dc.contributor.author | Grün, Rainer | - |
| dc.contributor.author | Parés, Josep María | - |
| dc.contributor.author | Martín-Francés, Laura | - |
| dc.contributor.author | Campaña Lozano, Isidoro | - |
| dc.contributor.author | Rosell, Jordi | - |
| dc.contributor.author | Shao, Qingfeng | - |
| dc.contributor.author | Arsuaga, Juan Luis | - |
| dc.contributor.author | Carbonell, Eudald | - |
| dc.contributor.author | Bermúdez de Castro, José María | - |
| dc.date.accessioned | 2018-05-22T16:06:51Z | - |
| dc.date.issued | 2018-08 | - |
| dc.identifier.citation | Quaternary Geochronology, 2018, 47, 120-137 | es_ES |
| dc.identifier.issn | 1871-1014 | - |
| dc.identifier.issn | 1878-0350 | - |
| dc.identifier.uri | http://cir.cenieh.es/handle/20.500.12136/353 | - |
| dc.description.abstract | The present study reports the results of the first direct Electron Spin Resonance (ESR) dating study of Homo antecessor, the earliest known hominin species identified in Europe. The analysis of a tooth (ATD6-92) from TD6 unit of Atapuerca Gran Dolina (Spain) following a “semi non-destructive” procedure provides a final age estimate ranging from 624 to 949 ka, which covers all possible uranium uptake scenarios. Last, the additional magnetostratigraphic data collected within TD6 enables to further constrain the initial ESR chronology and to propose an age of between 772 and 949 ka for Homo antecessor, in agreement with previous dating works. Whereas our new results do not refine the existing chronology of stratigraphic unit TD6, they nevertheless support the antiquity of H. antecessor, which pre-dates the estimated divergence age of modern and archaic human lineages based on genetic evidence. This work illustrates the challenges of dating human teeth by means of the ESR method, with the main pitfalls that are sometimes inherent to this specific application (e.g., systematic μCT-scanning of fossil hominin teeth; limited knowledge about the original sedimentary environment for teeth coming from old excavations; heterogeneous spatial distribution or the U-series elements in dental tissues). We identified several sources of uncertainty that may directly impact the accuracy of the age result. In particular, a slight contamination of dentine (<6%) in the enamel fragment measured by ESR was found to induce a significant age underestimation (33%) if not taken into consideration. It indeed caused not only a DE underestimation (by about 8%), but also produced a massive internal dose rate overestimation (by a factor of about 3.5). In contrast, other sources of uncertainty, such as the heterogeneity of the sedimentary environment, the variability of the water content over time, the previous μCT-scanning of the tooth or the potential preferential creation of unstable NOCORs in the ESR signal, showed here a limited impact on the final age result. | es_ES |
| dc.description.sponsorship | We would like to thank V. Guilarte, D. Martínez Asturias, B. Notario Collado, C. Saiz and M.I. Sarro from CENIEH for their help some aspects of the analytical procedure, and M. Modesto-Mata (CENIEH) for providing the pictures used in Fig. 2. We are also thankful to Ken Kodama for letting us use the Paleomagnetic Laboratory at Lehigh University, where some measurements were done, and to María Martinón-Torres (CENIEH) for her support and useful comments on the manuscript. The constructive comments made by two anonymous reviewers contributed to improve the quality of the paper. The research leading to these results has received funding from the People Programme (Marie Curie Actions) of the European Union's Seventh Framework Programme (FP7/2007–2013) under REA Grant Agreement nº PIOF-GA-2013-626474, and the Australian Research Council Future Fellowship grant FT150100215. Aspects of this study have received financial support from the French State in the frame of the “Investments for the future” Programme IdEx Bordeaux, reference ANR-10-IDEX-03-02. Atapuerca Research Project is supported by the project number CGL2015-65387-C3-3-P of the MINECO (FEDER, UE), The Consejería de Cultura y Turismo of the Junta de Castilla y León, and the Fundación Atapuerca. I.C. was the recipient of a pre-doctoral FPI Scholarship from the Spanish MINECO. Finally, we give our special thanks to all members of the Atapuerca Research and Excavation Team for their hard work during many years. | es_ES |
| dc.language.iso | en | es_ES |
| dc.publisher | Elsevier | es_ES |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América | * |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/us/ | * |
| dc.title | The first direct ESR dating of a hominin tooth from Atapuerca Gran Dolina TD-6 (Spain) supports the antiquity of Homo antecessor | es_ES |
| dc.type | Article | es_ES |
| dc.identifier.doi | 10.1016/j.quageo.2018.05.001 | - |
| dc.relation.publisherversion | https://doi.org/10.1016/j.quageo.2018.05.001 | es_ES |
| dc.date.available | 2020-08-22 | - |
| Appears in Collections: | Geocronología y Geología Paleobiología | |
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|---|---|---|---|---|
| The first direct ESR dating of a hominin tooth from Atapuerca Gran Dolina TD-6 (Spain) supports the antiquity of Homo antecessor_Duval_et_al_2018.pdf | 4.21 MB | Adobe PDF | ![]() View/Open |
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