<?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><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><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%">Van Der Wiel, A M</style></author><author><style face="normal" font="default" size="100%">Wijmstra, T A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Palynology of the 112.8–197.8 m interval of the core Tenaghi Philippon III, Middle Pleistocene of Macedonia</style></title><secondary-title><style face="normal" font="default" size="100%">Review of Palaeobotany and Palynology</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Biostratigraphy</style></keyword><keyword><style  face="normal" font="default" size="100%">Chronostratigraphy</style></keyword><keyword><style  face="normal" font="default" size="100%">palynology</style></keyword><keyword><style  face="normal" font="default" size="100%">vegetation history (PG)</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1987</style></year></dates><volume><style face="normal" font="default" size="100%">52</style></volume><pages><style face="normal" font="default" size="100%">89-117</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">In this article the palynological record of the Tenaghi Philippon III core (112.8–197.8 m) from the Philippi Plain in Greece is discussed. The arboreal pollen diagrams show an alteration of steppe phases (representing glacial periods) and oak forest phases (coinciding with interglacial periods). A proposal for a local biostratigraphy is given and a preliminary correlation is suggested with the Northwest European subdivision of the Middle Pleistocene. From the AP diagrams it appears that the flora is gradually impoverished in Arcto-Tertiary elements and obtains a more mediterranean character. In this section, however, the real mediterranean forest, rich in Quercus ilex/coccifera type is not yet present, which implies that a warm humid climate dominated with rainfall throughout the year. The presence of a great number of Tertiary pollen, two sterile intervals and clastic sediment in the lower part of the core, while from 181.6 m upwards organic sediment is found, indicates a change in sedimentation regime around a depth of 182 m. The sedimentation regime changed from fluvatile to lacustrine as a result of the aftermath of tectonic events. Chronostratigraphy of the diagrams is based on radiocarbon dates from the TF2 core, paleomagnetic polarity determinations in the TF3 core as well as interpolations between the two. In this way the core was dated at 900,000-approx. 600,000 yr B.P. A correlation with deep-sea Core V28–239 is proposed. From this correlation it appears that both in the diagrams and in the oxygen isotope curve the glacial and interglacial periods of the Middle Pleistocene are of a different wavelength and amplitude as compared to the ones of the Upper Pleistocene.</style></abstract></record></records></xml>