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