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This work received financial support from the research projects CGL2015–68333-P (MINECO/FEDER, UE), Research Group BSCHUCM 910607 and Consolidated Research Group EO5 (Aragón Government). Referencias bibliográficas: • Adrover R (1986) Nuevas faunas de roedores en el Mio-Plioceno continental de la región de Teruel (España). Interés bioestratigráfico y paleoecológico. Instituto de Estudios Turolenses, Teruel • Adrover R, Feist M, Hugueney M, Mein P, Moissenet E (1982) L'áge et la mise en relief de la formation détritique culminante de la Sierra Pelarda (Province de Teruel, Espagne). C R Acad Sci Paris 295:231–236 • Aguirre E (1973) Conservación e historia de la Naturaleza. Boletín Estación Central. Ecología 2:89–97 • Aguirre E, Morales J, Soria D (1981) Accumulated bones in a Pliocene cave in Cerro Pelado, Spain. Natl Res Rep 13:69–81 • Agustí J, Santos-Cubero A, Furió M, De Marfa R, Blain H-A, Oms O, Sevilla P (2011) The late Neogene-early quaternary small vertebrate succession from the Almenara-Casablanca karst complex (Castellón, Eastern Spain): chronologic and paleoclimatic context. Quat Int 243:183–191 • Calvo JP, Daams R, Morales J, López-Martínez N, Agustí J, Anadón P, Armenteros I, Cabrera L, Civis J, Corrochano A, Díaz-Molina M, Elizaga E, Hoyos M, Martín-Suárez E, Martínez J, Moissenet E, Muñoz A, Pérez-García A, Pérez-González A, Portero JM, Robles F, Santisteban C, Torres T, van der Meulen J, Vera JA, Mein P (1993) Up-to-date Spanish continental Neogene synthesis and paleoclimatic interpretation. Rev Soc Geol Esp 6:29–40 • Daams R, Meulen A, Van Der Peláez-Campomanes P, Álvarez-Sierra MA (1999) Trends in rodent assemblages from the Aragonian (early-middle Miocene) of the Calatayud-Daroca Basin, Aragón, Spain. In: Agustí J, Rook L, Andrews P (eds) Hominoid evolution and climatic change in Europe (the evolution of Neogene terrestrial ecosystems in Europe), vol 1. Cambridge University Press, Cambridge, pp 390–412 • Hilgen FJ, Lourens LJ, Dam JA Van, with Contr, Corral de Lobato, a karstic site in the area of Molina de Aragón has been studied in a preliminary way. Even though there are not many Neogene karstic sites in the Iberian Chain, they occur in four clusters, with ages ranging from latest middle Miocene (MN7/8) to early Pleistocene (MN17). Correlations between these clusters and the reference stratigraphical units of the Tagus Basin, as well as with local and global events, are proposed. These karstic sites provide a complementary source of fossil vertebrate remains to that of the stratified sites formed lowland. The Heritage significance of such sites arises from the enhanced preservation of rare taxa or associations, and the operation of biotic concentrative processes., Gobierno de Aragón, Depto. de Didáctica de las Ciencias Experimentales , Sociales y Matemáticas, Fac. de Educación, TRUE, pub