2026-06-29T20:09:29Zhttps://riubu.ubu.es/oai/requestoai:riubu.ubu.es:10259/63562023-01-01T23:42:05Zcom_10259.4_2526com_10259.4_2525com_10259.4_106com_10259_2604com_10259.4_2560com_10259_5086col_10259_4164col_10259.4_2561
High-resolution late Middle Pleistocene paleoclimatic record from the Galería Complex, Atapuerca archaeological site, Spain - An environmental magnetic approach
Bógalo Román, Mª Felicidad
Bradák, Balázs
Villalaín Santamaria, Juan José
Calvo Rathert, Manuel
González Martín, Manuel Iván
Heller, F.
Ortega Martínez, Ana Isabel
Parés Casanova, Josep M.
Galería Complex
Atapuerca
Western europe
Late Middle Pleistocene
Paleoclimatology
MIS9
MIS8
Sediment mineralogy
Environmental magnetism
Goethite proxy
The 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).
2022-01-25T13:15:09Z
2022-01-25T13:15:09Z
2021-01
info:eu-repo/semantics/article
0277-3791
http://hdl.handle.net/10259/6356
10.1016/j.quascirev.2020.106721
eng
Quaternary Science Reviews. 2021, V. 251, 106721
https://doi.org/10.1016/j.quascirev.2020.106721
info:eu-repo/grantAgreement/Junta de Castilla y León//BU235P18//Análisis arqueomagnéticos en materiales arqueológicos quemados de edad holocena y pleistocena
info: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-cenozoica
info: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 ATAPUERCA
info: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 CRONOESTRATIGRAFICO
info: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 CRETACICO
info: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 CAUCASO
info:eu-repo/grantAgreement/MICIU/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PRX19%2F00148
http://creativecommons.org/licenses/by-nc-nd/4.0/
info:eu-repo/semantics/openAccess
Attribution-NonCommercial-NoDerivatives 4.0 Internacional
Elsevier