A multiproxy approach for the reconstruction of ancient continental environments. The case of the Mio-Pliocene deposits of the Granada Basin (southern Iberian Peninsula)

Situation maps and comparison between the temperature reconstruction from isotopic data and that based on the palaeoecology of the small mammal associations in the Granada Basin (García-Alix et al., 2008b), the humidity reconstruction from isotopic data and those based on the palaeoecology of the small mammal associations in the Granada Basin, as well as the sedimentary and environmental evolution of the Granada Basin according to García-Alix et al. (2008b). The estimated absolute age of the studied fossil localities has been taken from García-Alix et al. (2008a, 2008b). Fossil locality acronyms are the same as in Table 1.