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Precisions on the age of the Margas del Forcall Fm in the Oliete sub-basin (NE Iberian Range, Spain) by means of ammonoids and nautiloids

dc.contributor.authorMoreno, J. A.
dc.contributor.authorCompany, M.
dc.contributor.authorDelanoy, G.
dc.contributor.authorGrauges, A.
dc.contributor.authorMartínez, G.
dc.contributor.authorSalas, Ramón
dc.description.abstractAmmonoids and nautiloids from Margas del Forcall Formation, located in the Oliete sub-basin (Iberian Chain), were studied. Taphonomic, sedimentologic and biostratigraphic analyses were carried out. The fossil record of cephalopods is especially abundant in a layer made up of reddish limestone with elongated nodules that are usually covered by a ferruginous-manganese crust. These nodules are embedded in a micritc matrix where infaunal tiering is largely preserved. The biostratigraphic study has allowed recognizing Hambrovi Subzone and proposing a new bioestratigraphic position for this stratigraphic intervalen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherMargas del Forcall Formationen_US
dc.subject.otherIberian Chainen_US
dc.subject.otherHambrovi Subzoneen_US
dc.titlePrecisiones sobre la edad, mediante ammonoideos y nautiloideos, de la Fm. Margas del Forcall en la subcuenca de Oliete (Cadena Ibérica, España)en_US
dc.titlePrecisions on the age of the Margas del Forcall Fm in the Oliete sub-basin (NE Iberian Range, Spain) by means of ammonoids and nautiloidseng

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