Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/42033
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dc.contributor.authorGibert Atienza, Jordi Maria de-
dc.contributor.authorLópez Blanco, Miguel-
dc.contributor.authorRamos Guerrero, Emilio-
dc.date.accessioned2013-05-03T16:35:39Z-
dc.date.available2013-05-03T16:35:39Z-
dc.date.issued2007-
dc.identifier.issn0213-683X-
dc.identifier.urihttp://hdl.handle.net/2445/42033-
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 occurrences.-
dc.format.extent4 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isospa-
dc.publisherSociedad Geológica de España-
dc.relation.ispartofGeogaceta, 2007, vol. 41, p. 91-94-
dc.rights(c) Sociedad Geológica de España, 2007-
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)-
dc.subject.classificationIcnologia-
dc.subject.classificationEocè-
dc.subject.classificationEbre, Conca de l'-
dc.subject.otherIchnology-
dc.subject.otherEocene Epoch-
dc.subject.otherEbro River Watershead-
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).spa
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec551466-
dc.date.updated2013-05-03T16:35:39Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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