Major sea-level cycles occurred in the Cenomanian-early Turonian greenhouse world and
impacted depositional conditions and ecosystems across the paleo-shelf seas. These sea …

Abstract The Cenomanian 'Marnes de Smail'Formation in Djebel Sabaoune (Batna, Algeria)
contains many fossil ostracods with 73 species taxa that are identified for the first time from …

Abstract The Abu Qada Formation is a reference interval for the Cenomanian–Turonian
boundary event in the northeastern margin of Africa. In this paper, geochemical …

The current investigation provides further insight into the petroliferous characteristics of the
Abu Roash “G” Member, which is regarded as an important rock unit for the Egyptian oil …

Quantitative palynological, sedimentological, and geophysical data analyses of the
Cretaceous Abu Tunis 1X well from the Matruh Basin, northwestern Egypt indicate …

Abstract The ostracode Family Brachycytheridae is one of the most common taxa of Late
Cretaceous shallow marine microfossils, and occurs in the marginal basins of Africa …

This study deals with the integration between geochemical data (carbon isotope and, total
organic carbon) and foraminiferal turnover to track the Oceanic Anoxic Event 2 (OAE2) from …

Microfacies, fossil macroinvertebrates and microfossil assemblages (foraminifera and
ostracods) and δ 13 C from the Rhoundjaïa Formation (Ksour Mountains, Western Saharan …

Abstract During the Cenomanian and Turonian, high eustatic sea levels combined with
subsidence of North Africa resulted in widespread marine inundation and the evolution of an …

Despite their potential for providing important information for paleobiogeography, studies
using ostracod assemblages compiled from global datasets have been scarce so far. In this …