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| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Piñero, Pedro | - |
| dc.contributor.author | Agustí, Jordi | - |
| dc.contributor.author | Laborda, Casto | - |
| dc.contributor.author | Duval, Mathieu | - |
| dc.contributor.author | Zhao, Jian-xin | - |
| dc.contributor.author | Blain, Hugues-Alexandre | - |
| dc.contributor.author | Furió, Marc | - |
| dc.contributor.author | Laplana, César | - |
| dc.contributor.author | Rosas, Antonio | - |
| dc.contributor.author | Sevilla, Paloma | - |
| dc.date.accessioned | 2022-06-30T14:22:46Z | - |
| dc.date.issued | 2022-05 | - |
| dc.identifier.citation | Quaternary Science Reviews, 2022, 283, 107469 | es_ES |
| dc.identifier.issn | 0277-3791 | - |
| dc.identifier.uri | http://cir.cenieh.es/handle/20.500.12136/2701 | - |
| dc.description.abstract | With the identification of the Jaramillo geomagnetic subchron, the late Early Pleistocene vertebrate succession of the Quibas-Sima section (Quibas karstic complex, southern Spain) represents a time span scarcely recorded in Europe. To complete the existing chronostratigraphic framework published earlier by Piñero et al. (2020), we provide here additional new information about the lithostratigraphy and micromammal succession along the sedimentary sequence. Seven lithostratigraphic units have been differentiated (QS-1 to QS-7) at Quibas-Sima, documenting an almost continuous small mammal record, including representatives of the families Soricidae, Erinaceidae, Rhinolophidae, Vespertilionidae, Arvicolidae, Muridae, Gliridae, Sciuridae, Leporidae and Ochotonidae. The small mammal association indicates that units QS-1 to QS-4 have an intermediate biostratigraphic position between the sites of Fuente Nueva 3 (ca. 1.2 Ma) and Cueva Victoria (ca. 0.9 Ma). New numerical age result from the combined U-series/ESR dating of one equid tooth from QS-3 consistently support the general chronostratigraphic framework based on magnetostratigraphy and biostratigraphic inferences by confirming a post-Olduvai age. Based on an estimation of the sedimentation rate during the Jaramillo subchron, these broad chronological constraints may be confidently refined to approx. 1.1–0.9 Ma for the whole sequence. While we acknowledge the existing uncertainty associated to this age range, it is nevertheless consistent with biostratigraphic evidence indicating that all stratigraphic units most likely do not significantly differ from a chronological point of view. Both independent proxies (biostratigraphy and the sedimentation rate) strongly suggest that the sedimentary sequence covers a relatively short time interval (<200 kyr). These results place the Quibas-Sima sequence as one of the longest and most complete pre-Jaramillo (QS-1) to Jaramillo (QS-2 to QS-5) continental vertebrate succession in Europe. | es_ES |
| dc.description.sponsorship | This work was supported by the the Comunidad Autónoma de la Región de Murcia (ARQ115/2018, Subvención para la Investigación e Intervención en el Patrimonio Arqueológico y Paleontológico de la Región de Murcia), the Palarq Foundation, the Spanish Agencia Estatal de Investigación and the European Regional Development Fund of the European Union (AEI/FEDER EU, PID 2020-117289 GB-I00), the Spanish Ministry of Science and Innovation (MICINN/FEDER, CGL 2016-75109-P), and Generalitat de Catalunya (AGAUR 2017/SGR/859). The Institut Català de Paleoecologia Humana i Evolució Social (IPHES-CERCA) has received financial support from the Spanish Ministry of Science and Innovation through the “María de Maeztu” program for Units of Excellence (CEX 2019-000945-M). PP was beneficiary of a postdoctoral contract from the “María de Maeztu” program. The U-series and ESR dating analyses have been funded by the Spanish Ramón y Cajal Fellowship RYC 2018-025221-I. We are grateful to María Jesús Alonso Escarza and Javier Iglesias Cibanal, CENIEH, technical support associated to the ESR dating analytical procedure. The solution U-series dating analyses were carried out within the framework of the existing Brisbane Geochronology Alliance between Griffith University, University of Queensland and Queensland University of Technology. We gratefully acknowledge support of this work by Gregorio Romero and the Servicio de Patrimonio Histórico de la Dirección General de Bienes Culturales de la Región de Murcia. We would like to express our thanks to the Quibas excavation team, who helped with the extraction, sieving, and washing of sediments. The authors wish to thank the Town Hall of Abanilla for their support and facilities in conducting research at the Quibas site. We thank Dr. Raef Minwer-Barakat and one anonymous reviewer for constructive comments on an earlier version of the manuscript. | es_ES |
| dc.language.iso | en | es_ES |
| dc.publisher | Elsevier | es_ES |
| dc.rights | info:eu-repo/semantics/embargoedAccess | es_ES |
| dc.rights | Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) | - |
| dc.rights.uri | https://creativecommons.org/licenses/by-nc-nd/4.0/ | - |
| dc.subject | Jaramillo subchron | es_ES |
| dc.subject | Early Pleistocene | es_ES |
| dc.subject | Combined U-Series/ESR dating | es_ES |
| dc.subject | Biostratigraphy | es_ES |
| dc.subject | Micromammals | es_ES |
| dc.title | Quibas-Sima: A unique 1 ma-old vertebrate succession in southern Iberian Peninsula | es_ES |
| dc.type | Article | es_ES |
| dc.identifier.doi | 10.1016/j.quascirev.2022.107469 | - |
| dc.relation.publisherversion | https://doi.org/10.1016/j.quascirev.2022.107469 | es_ES |
| dc.date.available | 2022-06-30T14:22:46Z | - |
| Appears in Collections: | Datación por Resonancia Paramagnética Electrónica Geocronología y Geología | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| Quibas-Sima A unique 1 ma-old vertebrate succession in southern Iberian Peninsula_Piñero et al_2022.pdf | 2.06 MB | Adobe PDF | ![]() View/Open |
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