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dc.contributor.authorBógalo Román, Mª Felicidad 
dc.contributor.authorBradák, Balázs 
dc.contributor.authorVillalaín Santamaria, Juan José 
dc.contributor.authorCalvo Rathert, Manuel 
dc.contributor.authorGonzález Martín, Manuel Iván 
dc.contributor.authorHeller, F.
dc.contributor.authorOrtega Martínez, Ana Isabel
dc.contributor.authorParés Casanova, Josep M.
dc.date.accessioned2022-01-25T13:15:09Z
dc.date.available2022-01-25T13:15:09Z
dc.date.issued2021-01
dc.identifier.issn0277-3791
dc.identifier.urihttp://hdl.handle.net/10259/6356
dc.description.abstractThe Galería Complex is a cave sediment succession at the Atapuerca paleoanthropological site (Burgos, Spain) that offers detailed environmental information about the late Middle Pleistocene, especially the period between marine oxygen isotope stages MIS10 and MIS7. Previous studies have reconstructed the chronology and detailed the environmental development of this key succession. We introduce rock magnetic climate proxies from the sedimentary units of the Galería succession that we correlate with the global climate record as represented by the marine oxygen isotope record. The cave sediment sequence consists of five infilling phases, four of which were sampled at high resolution across a 5 m thick composite profile. We propose a novel goethite climate proxy along with a frequently used ultrafine ferrimagnetic mineral proxy for paleoclimate reconstruction and detailed chronostratigraphic correlation with isotope stages and substages MIS10/MIS10-9, MIS9e-a and MIS8. The proxies reveal new paleoenvironmental information about paleoprecipitation and indicate that MIS9e was a humid (∼650 mm/year maximum annual precipitation) and intense interglacial in northern Spain that declined in steps into the globally weak glacial stage MIS8. MIS8 consisted of drier periods with 430–510 mm/year annual precipitation and at least one humid substage (600 mm/year).en
dc.description.sponsorshipJunta de Castilla y León (Spain) and the European Regional Development Fund (ERDF) (BU235P18) and the research projects CGL2016-77560-C2, CGL2018-093925-B-C31, and CGL2017-89603-R of the Spanish Ministry of Science and Innovation and PID2019-108753 GB-C21 and PID2019-105796 GB-I00 of the Spanish State Research Agency (AEI/10.13039/501100011033) and ERDF funding (European Union). B. Bradák acknowledges financial support from project BU235P18 (Junta de Castilla y León, Spain) and the European Regional Development Fund (ERDF). M. Calvo-Rathert acknowledges funding from the Fulbright Commission and the Spanish Ministry of Science Innovation and Universities (PRX19/00148) for a research stay at University of Hawaii at Manoa.en
dc.format.mimetypeapplication/pdf
dc.language.isoengen
dc.publisherElsevieren
dc.relation.ispartofQuaternary Science Reviews. 2021, V. 251, 106721en
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectGalería Complexen
dc.subjectAtapuercaen
dc.subjectWestern europeen
dc.subjectLate Middle Pleistoceneen
dc.subjectPaleoclimatologyen
dc.subjectMIS9en
dc.subjectMIS8en
dc.subjectSediment mineralogyen
dc.subjectEnvironmental magnetismen
dc.subjectGoethite proxyen
dc.subject.otherMagnetismoes
dc.subject.otherMagnetismen
dc.subject.otherArqueología-Burgoses
dc.subject.otherArchaeology-Burgosen
dc.subject.otherCiencias medioambientaleses
dc.subject.otherEnvironmental sciencesen
dc.titleHigh-resolution late Middle Pleistocene paleoclimatic record from the Galería Complex, Atapuerca archaeological site, Spain - An environmental magnetic approachen
dc.typeinfo:eu-repo/semantics/articlees
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.relation.publisherversionhttps://doi.org/10.1016/j.quascirev.2020.106721es
dc.identifier.doi10.1016/j.quascirev.2020.106721
dc.relation.projectIDinfo:eu-repo/grantAgreement/Junta de Castilla y León//BU235P18//Análisis arqueomagnéticos en materiales arqueológicos quemados de edad holocena y pleistocenaes
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-77560-C2-1-P/ES/La remagnetización cretacica del alto Atlas Central como herramienta de reconstrucción geométrica de la estructura Pre-cenozoicaes
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PGC2018-093925-B-C31/ES/EL PLEISTOCENO Y HOLOCENO DE LA SIERRA DE ATAPUERCAes
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2017-89603-R/ES/LA TRANSICION DE AGRADACION A DEGRADACION EN CUENCAS CENOZOICAS IBERICAS: MARCO CRONOESTRATIGRAFICOes
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2019-108753 GB-C21/ES/LA CURVA DE DERIVA POLAR APARENTE DE LA PLACA IBERICA. NUEVOS DATOS PALEOMAGNETICOS SOBRE LA ROTACION DE IBERIA DURANTE EL CRETACICOes
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2019-105796 GB-I00/ES/LAS VARIACIONES DEL REGISTRO ARQUEOMAGNETICO PREHISTORICO EN LA PENINSULA IBERICA Y EL CAUCASOes
dc.relation.projectIDinfo:eu-repo/grantAgreement/MICIU/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PRX19%2F00148es
dc.journal.titleQuaternary Science Reviewsen
dc.volume.number251es
dc.page.initial106721es
dc.type.hasVersioninfo:eu-repo/semantics/acceptedVersiones


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