@article{10272/8427,
year = {2007},
url = {http://hdl.handle.net/10272/8427},
abstract = {Ammonoids 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 interval},
keywords = {Ammonoids},
keywords = {Nautiloids},
keywords = {Margas del Forcall Formation},
keywords = {Oliete},
keywords = {Iberian Chain},
keywords = {Hambrovi Subzone},
title = {Precisiones sobre la edad, mediante ammonoideos y nautiloideos, de la Fm. Margas del Forcall en la subcuenca de Oliete (Cadena Ibérica, España)},
title = {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},
author = {Moreno, J. A. and Company, M. and Delanoy, G. and Grauges, A. and Martínez, G. and Salas, Ramón},
}