MICROFAUNAS, MICROFLORAS AND SUCCESSIVE P ALEOENVIRONMENTS FROM THE EL-MERS FORMATION BATHONIAN-QUESTIONABLE CALLAVIAN) IN THE SKOURA SYNCLINE (MIDDLE-ATLAS, MOROCCO)

Citation
A. Charriere et al., MICROFAUNAS, MICROFLORAS AND SUCCESSIVE P ALEOENVIRONMENTS FROM THE EL-MERS FORMATION BATHONIAN-QUESTIONABLE CALLAVIAN) IN THE SKOURA SYNCLINE (MIDDLE-ATLAS, MOROCCO), Geobios, 27(2), 1994, pp. 157-174
Citations number
NO
Categorie Soggetti
Paleontology
Journal title
ISSN journal
00166995
Volume
27
Issue
2
Year of publication
1994
Pages
157 - 174
Database
ISI
SICI code
0016-6995(1994)27:2<157:MMASPA>2.0.ZU;2-X
Abstract
In the Middle-Atlas (Morocco), the lower part of the ''Red beds'' (El Mers Formation), Middle Jurassic in age, contains various microfossils which permit to reconstruct the palaeoenvironmental evolution of this area for this period. Populations of abundant charophytes, collected at the base of the formation, are assigned to a new species : Porochar a hians FEIST & GRAMBAST-FESSARD. Species of ostracods are generally d ifferent than the European synchronous ones. The first ostracods appea ring at the base of the formation are monospecific and euryhaline (con tinental or brackish). They are more diversified above and correspond to a typical marine depositional environment.