Fauna de Ammonites del tránsito complejo Urgoniano-Flysch negro entre Gernika y DebaAlbiense medio y superior, región Vascocantábrica Septentrional
- Agirrezabala Mundiñano, Luis M.
- Martínez Ribas, Ricard
- García Mondéjar, Joaquín
ISSN: 1130-4995
Year of publication: 1992
Issue: 2
Pages: 143-169
Type: Article
More publications in: Treballs del Museu de Geologia de Barcelona
Abstract
The fauna of ammonites from the Urgonian and Supraurgonian (Black Flysch) complexes, between Gemika and Deba (Bizkaia and Gipuzkoa), is described. The Urgonian consist of limestone horsts and lutite troughs separated by active faults. Limestones are mainly rudist and coral micrites and the adjacent lutites enclose resedimented limestone megabreccias and quartz conglomerates. The Black Flysch is made up of thick sandy turbidites passing laterally to lutites and thin sandy turbidites and to thoroughly bioturbated sandstones. Two ammomle associations are distinguished from these units, corresponding to the Middle Albian (Urgoman complex) and to the early Upper Albian (Black Flysch complex). Species of the following genera are described within the first association (Middle Albian): Phylloceras, Anagaudryceras, Kossmatella, Tetragonites, Puzosia, Desmoceras, Lyeiiceras, Tegoceros, Neophlycticeras, Metahamites and Hamites. The second association (early Upper Albian) includes species of:Kossmatella, Puzosia, Hysteroceras and Mortoniceras. The fauna described is cosmopolitan and its constituent taxa show atlantic as well as tethyan characteristics.