The revision of the radiolitid rudist bivalve Praeradiolites biskraensis (Coquand), including shell morphology and structure, taxonomical status, and palaeogeographical and stratigraphical distribution, was undertaken. We studied Coquand's collection, other specimens from the type locality, Col de Sfa, and other Algerian fossil localities, as well as recently collected material from the Gafsa region in Tunisia. A neotype from Col de Sfa is proposed. The stratigraphical distribution of the species is bracketed in the Upper Cenomanian, using the distribution of co-occurring ammonites in Tunisia and microfossils in Algeria. The palaeogeographical distribution is verified for Algeria and Tunisia based on all records in North Africa. Survey of the taxonomical status and problems of related radiolitid genera has resulted in revised diagnoses of Praeradiolites Douvillé, Eoradiolites Douvillé, Sphaerulites Lamarck and Radiolites Lamarck and revealed problems with Radiolites fleuriaui d'Orbigny, which is being the type species of Praeradiolites. Maghrebites gen. nov. is proposed for the North African radiolitid rudist Praeradiolites biskraensis (Coquand).Key words: Maghrebites gen. nov., Upper Cenomanian, North Africa, radiolitids, taxonomy, biostratigraphy.Upper Cretaceous North African radiolitid rudists have been described or reported since the second half of the 19th century. Earlier records were sometimes based on fossil material collected by field geologists or military amateur collectors and sent to rudists specialists in Europe. Many new taxa were named after these fossil collectors, and selected type material was often insufficient, incomplete or badly preserved. Thus, subsequent proper identification of these taxa was difficult. The stratigraphical or even geographical locations of some types were doubtful. As a consequence, many of the records of the species are in need of confirmation (see relevant references and discussion in Chikhi-Aouimeur, 2010).Originally, Coquand (1880) referred Praeradiolites biskarensis to the genus Sphaerulites, and neither the specimen was figured nor a type specimen was chosen. Thus, most of the subsequent identifications were based on the external views of Tunisian specimens given by Péron (1890), who identified it as Radiolites, and Pervinquière (1912), who identified it as Praeradiolites and corrected the spelling biskarensis to biskraensis. The species was not recognized by Douvillé (1910), who proposed a new species, P. tissoti, for a badly preserved Algerian specimen of P. biskraensis. Many amongst the relatively recently published records of the species lack descriptions or figures of specimens, or the figures are not even useful to show their characteristic external features.In this study, we (1) present a complete description of the external and internal shell features of P. biskraensis based on specimens from the type locality, Col de Sfa, Biskra in Algeria, as well as on specimens from the Gafsa region in Tunisia; (2) propose a neotype; (3) ascribe the species ...