A new early Visean coral assemblage from Azrou-Khenifra Basin, central Morocco and palaeobiogeographic implications
| Autor: | Javier Sanz-López, Pedro Cózar, Sergio Rodríguez, Mohamed El Houicha, Ian D. Somerville, Ismael Coronado, Ismail Said, Felipe González |
|---|---|
| Přispěvatelé: | Ministerio de Ciencia, Innovación y Universidades (España) |
| Rok vydání: | 2020 |
| Předmět: |
010506 paleontology
Coral 010502 geochemistry & geophysics 01 natural sciences Visean Paleontología Palaeobiogeography Paleontology Foraminifers Viséan Sedimentology lcsh:QE701-760 0105 earth and related environmental sciences biology Conodonts biology.organism_classification Morocco lcsh:Paleontology Corals Facies Geología estratigráfica Carbonate rock Syncline Conodont Mississippian Geology Marine transgression |
| Zdroj: | E-Prints Complutense: Archivo Institucional de la UCM Universidad Complutense de Madrid Digital.CSIC. Repositorio Institucional del CSIC instname Arias Montano. Repositorio Institucional de la Universidad de Huelva Scopus RUO. Repositorio Institucional de la Universidad de Oviedo E-Prints Complutense. Archivo Institucional de la UCM RUO: Repositorio Institucional de la Universidad de Oviedo Universidad de Oviedo (UNIOVI) Journal of Palaeogeography, Vol 9, Iss 1, Pp 1-20 (2020) |
| Popis: | A new early Visean coral assemblage has been recorded from turbidite facies in the southern part of the Azrou-Khenifra Basin, northwest of Khenifra, central Morocco. The newly discovered Ba Moussa West (BMW) coral fauna includesSiphonophyllia khenifrensesp. nov.,Sychnoelasma urbanowitschi,Cravenia lamellata,Cravenia tela,Cravenia rhytoides,Turnacipora megastomaandPleurosiphonella crustosa. The early Visean age of the coral assemblage is supported by foraminiferal and conodont data, with the recognition of the basal Visean MFZ9 Zone. This confirms that the first transgression in the Azrou-Khenifra Basin was during the earliest Visean. The allochthonous coral assemblage was recovered from coarse-grained proximal limestone debris flow and turbidite beds within a fault-bounded unit, lying to the west of a thrust syncline containing upper Visean limestones. No evidence exists of the former early Visean shallow-water platform from which the corals were derived. All other in situ platform carbonate rocks around the southern margin of the Azrou-Khenifra Basin are probably of late Visean (Asbian–Brigantian) age. The early Visean Ba Moussa West coral fauna can be compared with that at Tafilalt in eastern Morocco, as well as in other Saharian basins of Algeria. Many of the genera and species in the Ba Moussa West assemblage are identical to those in NW Europe, with which it must have had marine connections. The new rugose species described,Siphonophyllia khenifrense,is probably endemic to North Africa. Its ecological niche in NW Europe was occupied byS. cylindricaorS.aff.garwoodi. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|