Pla Pueyo, SilaViseras, CésarSoria, Jesús M.Arribas, A.2014-06-252014-06-252007http://hdl.handle.net/10272/8354In this work we develop an up-to-date stratigraphical scheme of a determinate zone within the western sector of the Guadix Basin (Betic Cordillera, South of Spain), where most of the main large-mammal sites are concentrated. The stratigraphical architecture is highly influenced in this sector by the tectonic evolution of the basin. The boundary between the two main genetic units represents a change in the rate of creation of new accommodation space. This change can be assumed as a consequence of the slow down of the tectonic subsidence in the area through the Pliocene and the PleistocenespaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Guadix BasinStratigraphyPliocene-PleistoceneContinental sedimentationSubsidencejournal articleopen access