The mixed siliciclastic–carbonate Teniet El Klakh Formation (Middle Jurassic, Bajocian)
mainly consists of a monotonous, clay and fine-grained sandstone alternation with some …

The palaeoenvironments of the upper Palaeozoic succession in the eastern foot slopes of
the Northern Galala Plateau, west of the Gulf of Suez, Egypt, are interpreted based on a …

The mixed siliciclastic-carbonate Teferguenite Formation (Pragian-Emsian) occurring in the
Ougarta Range (SW Algeria) is subdivided into two members: the Lower Member consists of …

Early Cretaceous succession of the Oued Fodda Formation in the Ouarsenis Mountains
(northwestern Algeria) is mainly composed of marl–limestone alternations, which are …

The Slama Formation (Upper Pliocene, Lower Chelif Basin, Algeria) displays siliciclastic
deposits distributed in five determined stratigraphic members: Lower Sandstone Member …

The Zoophycos ichnofacies is reported for the first time from the Lower Jurassic (Toarcian)
deposits of Algeria. The trace fossil-bearing strata in the Ksour Mountains, northwestern …

Recent work has focused on erecting new Seilacherian ichnofacies for depositional
environments subject to recurring temporal and spatial variations in physico-chemical stress …

Abstract The Upper Emsian to Frasnian Ia-Ib strata of the Marhouma area (or “km 30”
outcrop), exposed in the Ougarta Range (SW Algeria) belong to the Chefar El Ahmar …

Abstract The Berriasian–Valanginian succession cropping out in the Ouarsenis Range
(northwestern Algeria) consists of ammonite-bearing, marlstone-limestone alternations …

The Messinian shallow marine diatomaceous deposits (Tripoli Diatomite Formation) of the
Lower Chelif basin (northwestern Algeria) display a moderate diversity and high abundance …