2026-04-13T11:26:00Zhttps://recercat.cat/oai/request

oai:recercat.cat:2445/420332025-12-05T17:10:26Zcom_2072_1057col_2072_478804col_2072_478917

urn:hdl:2445/42033 Presencia de la icnoespecie Dactyloidites Ottoi en el complejo de abanico costero de Sant Llorenç del Munt (Eoceno, Cuenca del Ebro, NE de España). Gibert Atienza, Jordi Maria de López Blanco, Miguel Ramos Guerrero, Emilio Icnologia Eocè Ebre, Conca de l' Ichnology Eocene Epoch Ebro River Watershead 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. 2013-05-03T16:35:39Z 2013-05-03T16:35:39Z 2007 2013-05-03T16:35:39Z info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Geogaceta, 2007, vol. 41, p. 91-94 (c) Sociedad Geológica de España, 2007 info:eu-repo/semantics/openAccess Sociedad Geológica de España Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)