Presencia de la icnoespecie Dactyloidites ottoi en el complejo de abanico costero de Sant Llorenç del Munt (Eoceno, Cuenca del Ebro, NE de España)

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dc.contributor.authorGibert, J. M. de
dc.contributor.authorLópez Blanco, Miguel
dc.contributor.authorRamos Guerrero, Emilio
dc.date.accessioned2014-07-11T09:58:24Z
dc.date.available2014-07-11T09:58:24Z
dc.date.issued2006
dc.description.abstractThe presence of Dactyloidites ottoi is first recorded in the Eocene Sant Llorenç del Munt fan-delta complex. This constitutes the first citation for the Paleogene. The ichnospecies occurs in the lower part of a prograding fan-delta front sequence, associated to other traces produced by sediment-feeders. This association is substituted in the upper part of the sequence by abundant vertical Ophiomorpha indicating an increase of energetic conditions. The paleoenvironmental setting interpreted for Dactyloidites is consistent with that of previous described occurrencesen_US
dc.identifier.urihttp://hdl.handle.net/10272/8508
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherFan-deltaen_US
dc.subject.otherDelta-fronten_US
dc.subject.otherIchnologyen_US
dc.subject.otherDactyloidites ottoien_US
dc.subject.otherEoceneen_US
dc.titlePresencia de la icnoespecie Dactyloidites ottoi en el complejo de abanico costero de Sant Llorenç del Munt (Eoceno, Cuenca del Ebro, NE de España)en_US
dc.titlePresence of the ichnospecies Dactyloidites ottoi in the Sant Llorenç del Munt fan delta (Eocene, Ebro Basin, NE Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 41, (2006)