Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/3355
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dc.contributor.authorSantamaría Barragán, A.-
dc.contributor.authorParés, Josep María-
dc.contributor.authorColino García, S.-
dc.contributor.authorChurruca Clemente, A.-
dc.contributor.authorFujioka, Toshiyuki-
dc.contributor.authorSerrano-Ramos, A.-
dc.contributor.authorToffolo, Michael B.-
dc.contributor.authorÁlvaro Gallo, Ana-
dc.contributor.authorVal Blanco, Miren del-
dc.contributor.authorIglesias Cibanal, Javier-
dc.contributor.authorJáimez, J.-
dc.contributor.authorMiguens Rodríguez, Leticia-
dc.contributor.authorPla-Pueyo, S.-
dc.contributor.authorRevilla Cob, J.-
dc.contributor.authorSáiz Dominguez, Carlos-
dc.contributor.authorSolano García, J.-
dc.contributor.authorJiménez-Arenas, J. M.-
dc.contributor.authorViseras, C.-
dc.contributor.authorDuval, Mathieu-
dc.date.accessioned2024-09-25-
dc.date.accessioned2024-11-25T11:39:36Z-
dc.date.issued2024-11-
dc.identifier.citationJournal of Iberian Geology, 2024, (0), 1-24es_ES
dc.identifier.issn1698-6180-
dc.identifier.issn1886-7995-
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/3355-
dc.description.abstractWe report the first continuous core-based sedimentary record obtained at Barranco León, Spain, based on two boreholes drilled on the western and eastern margins of the ravine. The sediment cores cover an 80 m-thick succession belonging to the Baza Formation, which includes the lithic artefact- and fossil-bearing deposits documenting one of the earliest evidence of hominin presence in western Europe. Based on a series of observations performed at macroscopic (core description) and microscopic (grain size, fabric, thin sections) scales combined with the results obtained from the high- resolution multi-technique analysis of the natural radioactivity, magnetic susceptibility and carbonate content along the sediment cores, we identified six main lithostratigraphic units (named LU1 to LU6 from top to bottom) showing distinct compositions, textures and petrophysical properties. While our results are overall consistent with those from previous works based on outcropping sediment, we nevertheless provide here an unprecedented, detailed and continuous characterization of the 80-m thick sedimentary sequence at Barranco León. In particular, this is the first time that the deposits located > 15 m below the archaeological level can be accessed and thoroughly described in this area. Consequently, the present work offers a robust lithostratigraphic framework for future chronological and paleoenvironmental studies. From a methodological point of view, we observe a good consistency between the various data sets collected, independently of whether they were obtained from in situ or laboratory analyses, or using non-invasive or more destructive approaches. In particular, the magnetic susceptibility records obtained from the direct measurement of the core with a multi-sensor core logger, and from discrete samples collected from that same core, are in excellent agreement.es_ES
dc.description.sponsorshipInvestigations in the Orce Archaeo-paleontological Zone (OAZ) are performed within the framework of the Regional Research Project (PGI) ‘Evolución humana y paleoecología a partir de los yacimientos de la zona arqueológica `Cuenca de Orce´. Retos y desafíos. ReDes-ORCE’ funded by Andalusia. Drilling activities at Barranco León were been carried out under the umbrella of the poject ‘Actividad arqueológica puntual de excavación mediante sondeos geológicos en el entorno de Barranco León (Orce, Granada) 2022’. This work is part of Grant PID2021-123092NB-C22 funded by MCIN/AEI/ https://doi.org/10.13 039/5 01100011033/’ERDF A way of making Europe’, and of PID2021-122355NB-C33. Mathieu Duval’s investigation is currently supported by the Spanish Ramón y Cajal Fellowship RYC2018-025221-I, which is funded by MCIN/ AEI/ https://doi.org/10.13 039/5 01100011033 and by ‘ESF Investing in your future’. Michael Toffolo is supported by Grant RYC2021-030917-I funded by the MCIN/AEI/https://doi.org/10.13 039/5 01100011033 and by the “European Union NextGenerationEU/PRTR”. Alexia Serrano-Ramos and Juan Manuel Jiménez-Arenas are supported by project PID 2021.125098NB.I00 funded by M C I N / A E I /ht t p s: // d o i . o rg / 1 0 . 1 3 0 3 9 / 5 0 11 0 0 0 11 0 3 3 / F E D E R Una manera de hacer Europa, and ProyExcel_00274 funded by ‘Dirección General de Planificación de la Investigación (Consejería de Universidad, Investigación e Innovación, Junta de Andalucía)’. Aspects of the work received support from Grant PID2022-140850OB-C21 funded by MICIU/AEI/10.13039/501100011033/ and by “ERDF/EU”, and from Research Group RNM 369 (P.A.I.). We thank Santiago Padilla Domínguez for his help with the preparation of the cores before the MSCL-S analyseses_ES
dc.language.isoenes_ES
dc.publisherSpringer Science and Business Media LLCes_ES
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_ES
dc.subjectGuadix-Baza Basines_ES
dc.subjectBetic rangees_ES
dc.subjectOrcees_ES
dc.subjectBarranco Leónes_ES
dc.subjectMulti-sensor core loggeres_ES
dc.subjectMagnetic susceptibilityes_ES
dc.subjectDrillinges_ES
dc.titleHigh-resolution multi-technique analysis of a continuoussediment core of the Baza Formation at Barranco León (Guadix-Baza) Basin, Granada): First petrophysical resultses_ES
dc.typeArticlees_ES
dc.identifier.doi10.1007/s41513-024-00264-8-
dc.relation.publisherversionhttps://doi.org/10.1007/s41513-024-00264-8es_ES
dc.date.available2024-11-25T11:39:36Z-
Appears in Collections:Geocronología y Geología



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