Cenomanian and lower Turonian relative chronology and palaeoenvironmental framework of the Nouader site (Aures Basin, Northeastern Algeria)

Abstract

AbstractThe lower–upper Cenomanian boundaries interval of the Nouader site in the Aures Basin (NE Algeria) has been studied for the first time using the association of two particularly effective taxonomic groups, one macrofossil (ammonites), and the other microfossil (foraminifera). The study section is divided into two formations (Fahdene and Bahloul) and one member (Annaba). Biostratigraphicaly, six ammonite biozones and five foraminiferan biozones were identified and calibrated. The ammonite fauna allows recognition of the lower CenomanianMantelliceras mantelliZone, the upper lower CenomanianMantelliceras dixoniZone, the succeeding lower middle CenomanianCunningtoniceras inermeZone, theAcanthoceras rhotomagenseZone and its subzones ofTurrilites costatusandTurrilites acutus, followed by the upper middle CenomanianAcanthoceras amphibolumZone, the lower upper CenomanianEucalycoceras pentagonumZone and finally the lower TuronianPseudaspidoceras flexuosumZone. The foraminiferan biozones are respectively:Thalmanninella brotzeniZone,Thalmanninella reicheliZone,Rotalipora cushmaniZone,Whiteinella archaeocretaceaZone andHelvetoglobotruncana helveticaZone. Among 14 ammonite zones in the Tethyan domain versus 11 in the Boreal domain, seven are common to both domains. For the planktonic foraminifera the Tethyan domain has five zones, the Boreal domain also has five, with five in common. The succession of index species occurs in the same order in both Tethyan (NE Algeria and Central Tunisia) and Boreal realms (East and NW Europe). Furthermore, the supposed depositional setting is interpreted as a calm and relatively deep environment which can be located around the middle to the external platform.