Autor según el artículo: Campaña I; Benito-Calvo A; Pérez-González A; Ortega AI; Álvaro-Gallo A; Miguens-Rodríguez L; Iglesias-Cibanal J; de Castro JMB; Carbonell E
Departamento: Història i Història de l'Art
Autor/es de la URV: Carbonell Roura, Eudald
Palabras clave: Sedimentary facies Interior facies Gran dolina Early pleistocene Cave sedimentation Atapuerca sedimentary facies pleistocene sites paleoanthropological site karst interior facies gravity flow de-atapuerca clastic sediments cave sedimentation burgos atapuerca archaeological sites
Resumen: This work showed that cave sediments are useful for geomorphologic studies and for reconstructing depositional environments. While the cave entrance facies have been extensively studied for their relationship with the fossil and archaeological record, the cave interior facies have received much less attention, although they can provide much information on the geomorphological evolution of the karst. This work presents the stratigraphic and sedimentological study of a section >6 m thick and 10 m long of cave interior sediments of Galería Complex (Sierra de Atapuerca, Spain). Galería Complex is a cavity infill of the Sierra de Atapuerca (Spain), composed of three sections filled by at least 30 m of Pleistocene sediments. This sequence is divided into 5 lithostratigraphic units named from bottom to top: GI – GV. GI unit is 19 m thick of interior facies in the base of the Galería Complex, divided into two sub-unit, GIa and GIb, by the Matuyama-Bruhnes paleomagnetic boundary. GI unit shows an issue with the chronology since has uncoherent between TT-OSL and ESR/U-series and paleomagnetism dates. This work has been done by combining field observation with laboratory sedimentary analysis to characterize the texture and structure of the sediments. Based on these studies, 12 layers and 9 sedimentary facies have been identified. The facies associations indicate a clear separation between GIa and GIb sub-units. GIa sub-unit is dominated by epiphreatic conditions and represents continuous relativity sedimentation during the Early Pleistocene; meanwhile, GIb shows important erosion events and facies with reworked materials that indicate vadose conditions during the Middle Pleistocene. This environmental change is related to the geomorphological evolution of the Arlanzón River. In addition, soft-sediment deformation structures have been described, including faults and low-angle folds. An important leaching process has been identified by the presence of phosphates that could explain the underestimated ages obtained in other works.
Áreas temáticas: Interdisciplinar Historia Geosciences, multidisciplinary Geosciences, interdisciplinary Geology Geography, physical Geography Geografia i urbanisme Geografía Geociências Engenharias iii Engenharias i Earth-surface processes Ciências biológicas i Ciências ambientais Ciências agrárias i Biodiversidade Astronomia / física Antropologia / arqueologia
Acceso a la licencia de uso: https://creativecommons.org/licenses/by/3.0/es/
Direcció de correo del autor: eudald.carbonell@urv.cat
Identificador del autor: 0000-0001-6306-3621
Fecha de alta del registro: 2024-08-03
Versión del articulo depositado: info:eu-repo/semantics/publishedVersion
URL Documento de licencia: https://repositori.urv.cat/ca/proteccio-de-dades/
Referencia al articulo segun fuente origial: Geomorphology. 440
Referencia de l'ítem segons les normes APA: Campaña I; Benito-Calvo A; Pérez-González A; Ortega AI; Álvaro-Gallo A; Miguens-Rodríguez L; Iglesias-Cibanal J; de Castro JMB; Carbonell E (2023). Reconstructing depositional environments through cave interior facies: The case of Galería Complex (Sierra de Atapuerca, Spain). Geomorphology, 440(), -. DOI: 10.1016/j.geomorph.2023.108864
Entidad: Universitat Rovira i Virgili
Año de publicación de la revista: 2023
Tipo de publicación: Journal Publications
Repositori URV