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	Universitat de Barcelona
dc.contributor.author	Gibert Atienza, Jordi Maria de
dc.contributor.author	López Blanco, Miguel
dc.contributor.author	Ramos Guerrero, Emilio
dc.date	2007
dc.identifier.citation	0213-683X
dc.identifier.uri	http://hdl.handle.net/2445/42033
dc.format	4 p.
dc.format	application/pdf
dc.language.iso	spa
dc.publisher	Sociedad Geológica de España
dc.relation	Geogaceta, 2007, vol. 41, p. 91-94
dc.rights	(c) Sociedad Geológica de España, 2007
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Icnologia
dc.subject	Eocè
dc.subject	Ebre, Conca de l'
dc.subject	Ichnology
dc.subject	Eocene Epoch
dc.subject	Ebro River Watershead
dc.title	Presencia de la icnoespecie Dactyloidites Ottoi en el complejo de abanico costero de Sant Llorenç del Munt (Eoceno, Cuenca del Ebro, NE de España).
dc.type	info:eu-repo/semantics/article
dc.type	info:eu-repo/semantics/publishedVersion
dc.description.abstract	The 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.