A stratigraphic framework for the Pliocene-Pleistocene continental sediments of the Guadix Basin (Betic Cordillera, S. Spain)
Metadatos
Mostrar el registro completo del ítemAutor
Pla Pueyo, Sila; Viseras Alarcón, César; Soria, Jesús M.; Tent-Manclús, José E.; Arribas Herrera, AlfonsoEditorial
Elsevier
Fecha
2011-02-01Referencia bibliográfica
S. Pla-Pueyo, C. Viseras, J.M. Soria, J.E. Tent-Manclús, A. Arribas. 2011. A stratigraphic framework for the Pliocene-Pleistocene continental sediments of the Guadix Basin (Betic Cordillera, S. Spain). Quaternary International, 243, 16-32.
Patrocinador
RNM369Resumen
The central sector of the Guadix Basin (Betic Cordillera, S. Spain) hosts some of the most significant
Pleistocene large-mammal sites in Europe. The basin infill is divided into six genetic units, the three
lower with marine sediments and the remainder mainly continental. As the environmental characterization
of the sediments is crucial to understand the ecologic and geologic processes leading to the
formation of these sites, a stratigraphic, sedimentologic and petrologic study is presented. Combining
a lithologic correlation with previous biostratigraphic data and new magnetostratigraphic data,
a detailed litho-, bio- and magnetostratigraphic scheme has been developed for the study area. It shows
the stratigraphic architecture of the central sector of the Guadix Basin, together with the age and the
relative spatial position of the most important mammal sites. As well, it has been also helpful to identify
several isochronous surfaces, to establish the exact position and the age of the boundary between the
two last units of the continental infill in the Guadix Basin and to calculate sedimentation rates.