<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">García-Alix, A</style></author><author><style face="normal" font="default" size="100%">Minwer-Barakat, R</style></author><author><style face="normal" font="default" size="100%">Martín, J M</style></author><author><style face="normal" font="default" size="100%">Martín Suárez, E</style></author><author><style face="normal" font="default" size="100%">Freudenthal, M</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Biostratigraphy and sedimentary evolution of Late Miocene and Pliocene continental deposits of the Granada Basin (southern Spain)</style></title><secondary-title><style face="normal" font="default" size="100%">Lethaia</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Biostratigraphy</style></keyword><keyword><style  face="normal" font="default" size="100%">fossil small mammals</style></keyword><keyword><style  face="normal" font="default" size="100%">Granada Basin</style></keyword><keyword><style  face="normal" font="default" size="100%">Late Miocene</style></keyword><keyword><style  face="normal" font="default" size="100%">Pliocene</style></keyword><keyword><style  face="normal" font="default" size="100%">sedimentary evolution</style></keyword><keyword><style  face="normal" font="default" size="100%">Turolian–Ruscinian boundary.</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><volume><style face="normal" font="default" size="100%">41</style></volume><pages><style face="normal" font="default" size="100%">431-446</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The Late Miocene and Pliocene continental sediments in the Granada Basin (southern Spain) have yielded large amounts of fossil small mammals in 37 localities from 11 sections. The aim of this paper is to integrate faunistic, stratigraphic, and sedimentary criteria to unravel the geological history of the continental infilling of the basin. The palaeontological study has led to a detailed biozonation on the basis of rodents, which helps to correlate in detail the different sedimentary units found in the basin, and to follow the changes of the different sedimentary systems and their palaeogeographical evolution through time. Combination of the proposed biostratigraphy and the reinterpretation of the magnetostratigraphic analyses of the Barranco del Purcal section allows us to assign an absolute age slightly older than 5.23 Ma to the Turolian–Ruscinian boundary (MN13-MN14)</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">García-Alix, A.</style></author><author><style face="normal" font="default" size="100%">Minwer-Barakat, R.</style></author><author><style face="normal" font="default" size="100%">Martín, J. M.</style></author><author><style face="normal" font="default" size="100%">Martín Suárez, E.</style></author><author><style face="normal" font="default" size="100%">Freudenthal, M.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Biostratigraphy and sedimentary evolution of Late Miocene and Pliocene continental deposits of the Granada Basin (southern Spain)</style></title><secondary-title><style face="normal" font="default" size="100%">Lethaia</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Biostratigraphy</style></keyword><keyword><style  face="normal" font="default" size="100%">fossil small mammals</style></keyword><keyword><style  face="normal" font="default" size="100%">Granada Basin</style></keyword><keyword><style  face="normal" font="default" size="100%">Late Miocene</style></keyword><keyword><style  face="normal" font="default" size="100%">Pliocene</style></keyword><keyword><style  face="normal" font="default" size="100%">sedimentary evolution</style></keyword><keyword><style  face="normal" font="default" size="100%">Turolian–Ruscinian boundary.</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2008</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2008///</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://doi.wiley.com/10.1111/j.1502-3931.2008.00097.x</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">41</style></volume><pages><style face="normal" font="default" size="100%">431 - 446</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The Late Miocene and Pliocene continental sediments in the Granada Basin (southern Spain) have yielded large amounts of fossil small mammals in 37 localities from 11 sections. The aim of this paper is to integrate faunistic, stratigraphic, and sedimentary criteria to unravel the geological history of the continental infilling of the basin. The palaeontological study has led to a detailed biozonation on the basis of rodents, which helps to correlate in detail the different sedimentary units found in the basin, and to follow the changes of the different sedimentary systems and their palaeogeographical evolution through time. Combination of the proposed biostratigraphy and the reinterpretation of the magnetostratigraphic analyses of the Barranco del Purcal section allows us to assign an absolute age slightly older than 5.23 Ma to the Turolian–Ruscinian boundary (MN13-MN14)</style></abstract><issue><style face="normal" font="default" size="100%">4</style></issue></record></records></xml>