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Vertebrate fossil remains in the Paleogene of the Conca de Barbera and Ulldemolins areas, (Ebro Basin, Tarragona): stratigraphic Implications

dc.contributor.authorColombo Piñol, Ferrán
dc.contributor.authorMoya, S.
dc.contributor.authorCheca, L.
dc.contributor.authorAgustí, J.
dc.contributor.authorKöhler, M.
dc.description.abstractThe Ulldemolins Complex, which is characterized by different lithotypes, contains several types of fossil remains such as ostracoda, gastropoda, charophyta and micromammalia. This fossil association suggests that the Complex was deposited during the Culsian-Bartonlan time span. The outcrops located near the Ulldemolins village, which are characterized by mammalian remains, suggest that lower levels of Ulldemolins Complex were deposited during the Culslan time span. The outcrops located in the Conca d e Barberà area Indicate that the levels of the Montblanc Formation were deposited during the Bartonian-Pnabonian time span. The outcrops located near Vimbodi area suggest that the levels of Biancafort Fm were deposited during Lower Oligocene timesen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherMarine fossil remainsen_US
dc.subject.otherEbro basinen_US
dc.titleYacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräficoen_US
dc.titleVertebrate fossil remains in the Paleogene of the Conca de Barbera and Ulldemolins areas, (Ebro Basin, Tarragona): stratigraphic Implicationseng

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