000097832 001__ 97832
000097832 005__ 20210118122856.0
000097832 037__ $$aTAZ-TFG-2020-3720
000097832 041__ $$aspa
000097832 1001_ $$aMarí Navarro, Óscar
000097832 24200 $$aPaleoecological and paleoenvironmental study of the Mas de les Clapises (Mirambel Fm, Barremian, Castellon)
000097832 24500 $$aEstudio paleoecológico y paleoambiental de la sección de Mas de les Clapises (Fm. Mirambel, Barremiense, Castellón)
000097832 260__ $$aZaragoza$$bUniversidad de Zaragoza$$c2020
000097832 506__ $$aby-nc-sa$$bCreative Commons$$c3.0$$uhttp://creativecommons.org/licenses/by-nc-sa/3.0/
000097832 520__ $$aWeald Facies from the Iberian Lower Cretaceous are represented by several formations like Camarillas Fm, Galve Fm, Cantaperdius Fm and others. In the case of Mirambel Formation, most of the studies were carried out in the 20th century being the recent ones mainly focused on vertebrate findings.<br />Mas de Clapises I site (Portell de Morella, Castellon, Spain) has a high amount of dinosaur and other vertebrate findings out of geological context due to the lack of previous studies. In order to identify to which formation Mas de Clapises I belongs, a multidisciplinary study was carried out (stratigraphy, mineralogy and micropaleontology).<br />According to the results obtained, Mas de Clapises I was a barrier island system in the Mirambel Formation (in the lowermost part of the Lower Barremian attributed by charophyte associations and stratigraphical correlation) that suffered a transgressive event. Lagoon/lacustrine environments with charophytes (Atopochara trivolvis var. triquetra, Favargerella aquavivae, etc.), ostracodes (Cypridea) and also washover fans, tidal flats and emersion events with development of lateritic soils, evolved progressively to coastal facies (foreshore and shoreface) and final offshore facies with Chondrichthyes (Hybodus indet.), Osteichthyes (Pycnodontiformes and Amiidae), crocodylomorphs (Bernissatiidae), and benthic agglutinated foraminifera (Choffatella and Pseudocyclammina). The stratigraphic section ends at the beginning of a thick carbonate deposit that outcrops extensively in the area from the Artoles Formation (Upper Barremian).<br /><br />
000097832 521__ $$aGraduado en Geología
000097832 540__ $$aDerechos regulados por licencia Creative Commons
000097832 700__ $$aCanudo Sanagustín, José Ignacio$$edir.
000097832 700__ $$aBauluz Lázaro, Blanca$$edir.
000097832 7102_ $$aUniversidad de Zaragoza$$bCiencias de la Tierra$$cPaleontología
000097832 8560_ $$f693717@unizar.es
000097832 8564_ $$s3213110$$uhttps://zaguan.unizar.es/record/97832/files/TAZ-TFG-2020-3720.pdf$$yMemoria (spa)
000097832 909CO $$ooai:zaguan.unizar.es:97832$$pdriver$$ptrabajos-fin-grado
000097832 950__ $$a
000097832 951__ $$adeposita:2021-01-18
000097832 980__ $$aTAZ$$bTFG$$cCIEN
000097832 999__ $$a20200914092210.CREATION_DATE