Abstract The Cretaceous Period is a vital time interval in deciphering the evolutionary history
of the Neo-Tethys Ocean and the convergence of different plates and blocks across the …

Marine carbonate source rocks are ubiquitous worldwide and many of these can act as self-
sourced unconventional reservoirs. This work focuses on the Lower Turonian Abu Roash-F …

Lithostratigraphic, biostratigraphic and microfacies studies of two Cenomanian-Turonian
shallow-marine, siliciclastic-carbonate successions at Gebel Ekma plateau (southwestern …

Abstract The Ocean Anoxic Event (OAE2) at the Cenomanian-Turonian boundary presents a
unique record of gradual global warming and its effects on benthic organisms. The present …

In the Batna area of Algeria, the Cenomanian is represented by the Smail Marls Formation, a
highly fossiliferous unit with a diverse benthic macrofauna (mainly of ostreid bivalves). A …

The systematic study of bivalves collected from the Cenomanian-Turonian succession of the
Bellezma-Batna Mountains (northeastern Algeria) led identification of nine species …

The Coniacian strata of the Tébessa Mountains in northern Algeria are predominantly marly
facies that have received few studies. The present study is the first one to be carried out at …

Abstract Well-exposed fossiliferous Upper Cenomanian–Lower Turonian marine
sedimentary rocks are present in west-central Jordan. Ammonites serve as an important …

Palaeontological investigation of four lithostratigraphic sections documenting the upper
Cenomanian shallow marine carbonates of three palaeogeographic domains of southern …

ABSTRACT The Cenomanian/Turonian strata of the Kasserine area: Tunisia exhibit a
unique sedimentological and palaeontological pattern. Five lithological units have been …