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Quibas-Sima: A unique 1 ma-old vertebrate succession in southern Iberian Peninsula

dc.contributor.authorPiñero, Pedro
dc.contributor.authorAgustí, Jordi
dc.contributor.authorLaborda López, Casto
dc.contributor.authorDuval, Mathieu
dc.contributor.authorZhao, Jian-xin
dc.contributor.authorBlain, Hugues-Alexandre
dc.contributor.authorFurió, Marc
dc.contributor.authorLaplana, César
dc.contributor.authorRosas, Antonio
dc.contributor.authorSevilla García, María Paloma
dc.date.accessioned2023-06-22T10:41:53Z
dc.date.available2023-06-22T10:41:53Z
dc.date.issued2022-05-01
dc.description.abstractWith 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.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Ciencia e Innovación (MICINN)/FEDER
dc.description.sponsorshipComunidad Autónoma de la Región de Murcia
dc.description.sponsorshipGeneralitat de Catalunya
dc.description.sponsorshipCentro de Excelencia María de Maeztu
dc.description.sponsorshipPalarq Foundation
dc.description.sponsorshipRamón y Cajal Fellowship
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/71981
dc.identifier.doi10.1016/j.quascirev.2022.107469
dc.identifier.issn0277-3791, ESSN: 1873-457X
dc.identifier.officialurlhttps://doi.org/10.1016/j.quascirev.2022.107469
dc.identifier.urihttps://hdl.handle.net/20.500.14352/71419
dc.issue.number107469
dc.journal.titleQuaternary Science Reviews
dc.language.isoeng
dc.publisherElsevier
dc.relation.projectIDCGL 2016-75109-P; RYC 2018-025221-I.
dc.relation.projectIDARQ115/2018
dc.relation.projectIDAGAUR 2017/SGR/859
dc.relation.projectIDCEX 2019-000945-M
dc.relation.projectIDPID 2020-117289 GB-I00
dc.rights.accessRightsrestricted access
dc.subject.cdu569.32(460.33)
dc.subject.keywordJaramillo subchron
dc.subject.keywordEarly Pleistocene
dc.subject.keywordCombined U-Series/ESR dating
dc.subject.keywordBiostratigraphy
dc.subject.keywordMicromammals
dc.subject.ucmPaleontología
dc.subject.unesco2416 Paleontología
dc.titleQuibas-Sima: A unique 1 ma-old vertebrate succession in southern Iberian Peninsula
dc.typejournal article
dc.volume.number283
dspace.entity.typePublication
relation.isAuthorOfPublication5877a2d3-e5eb-414a-949f-c377cdc5272e
relation.isAuthorOfPublication.latestForDiscovery5877a2d3-e5eb-414a-949f-c377cdc5272e

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