Análisis de la producción científica de los arquitectos técnicos docentes universitarios en España. 1980-2015. Estudio de revistas indizadas en WOS-SCOPUS-CSIC (ICYT-ISOC)

Se estudia la producción científica de los Arquitectos Técnicos docentes universitarios en España en los últimos 35 años ya que el cambio del título académico al de Grado, el aumento del número de doctores y el desarrollo de una política académica que ha convertido en parámetro especial para medir la calidad de la Universidad la cantidad y calidad de los artículos publicados han propiciado un cambio sustancial en esta área del conocimiento. Se determina la investigación producida a través del análisis de las bases de datos WOS-SCOPUS-CSIC(ICYT-ISOC) y las revistas más utilizadas por esta disciplina y se analiza el número de publicaciones de este colectivo por Universidades y revistas. El estudio llevado a cabo evidencia un cambio sustancial en la producción científica de los arquitectos técnicos en España.

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.