In the Cenomanian of northern Tunisia, 5 divisions are based on the phylogeny of planktonic Foraminifera ; the upper part of the Rotundina stephani zone is the oldest one, the boundaries of the following ones coincide with the first appearance of Thalmanninella brotzeni, Th. appenninica gandolfii, Rotalipora cushmani montsalvensis, Ro. cushmani cushmani.La phylogénie des Foraminifères planctoniques permet de distinguer 5 subdivisions dans le Cénomanien de Tunisie septentrionale ; la plus ancienne correspond à la partie supérieure, datée par macrofaune, de la zone à Rotundina stephani, les limites inférieures des suivantes coïncident avec l'apparition de Thalmanninella brotzeni, Th. appenninica gandolfii, Rotalipora cushmani montsalvensis, R...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
In the Cenomanian of northern Tunisia, 5 divisions are based on the phylogeny of planktonic Foramini...
Planktonic foraminifera were quantitatively analyzed across the Upper Coniacian - Lower Campanian su...
The Upper Senonian rudist carbonate complex which makes up the Merfeg formation at Jebel el Kebar in...
Planktonic foraminifera were quantitatively analyzed across the Upper Coniacian - Lower Campanian su...
The study of Cenomanian planktonic Foraminifera can be performed in great details in the subalpine c...
The study of Cenomanian planktonic Foraminifera can be performed in great details in the subalpine c...
The foraminiferous wealth of the deposits of the Maastrichtian-Ypresian interval, in the northern an...
The planktonic foraminifera assemblage across the Global Boundary Stratotype Section and Point (GSSP...
Biostratigraphy of the AJbian of Koudiat el Beida (North of J. Mrhila, Central Tunisia). Biostratigr...
Biostratigraphy of the AJbian of Koudiat el Beida (North of J. Mrhila, Central Tunisia). Biostratigr...
El Amri Zaineb, Zaghbib-Turki Dalila, Karoui-Yaakoub Narjess. Biostratigraphie des foraminifères pla...
Planktonic foraminifera from sections in predominantly pelagic and hemipelagic sediments of Late Al...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
In the Cenomanian of northern Tunisia, 5 divisions are based on the phylogeny of planktonic Foramini...
Planktonic foraminifera were quantitatively analyzed across the Upper Coniacian - Lower Campanian su...
The Upper Senonian rudist carbonate complex which makes up the Merfeg formation at Jebel el Kebar in...
Planktonic foraminifera were quantitatively analyzed across the Upper Coniacian - Lower Campanian su...
The study of Cenomanian planktonic Foraminifera can be performed in great details in the subalpine c...
The study of Cenomanian planktonic Foraminifera can be performed in great details in the subalpine c...
The foraminiferous wealth of the deposits of the Maastrichtian-Ypresian interval, in the northern an...
The planktonic foraminifera assemblage across the Global Boundary Stratotype Section and Point (GSSP...
Biostratigraphy of the AJbian of Koudiat el Beida (North of J. Mrhila, Central Tunisia). Biostratigr...
Biostratigraphy of the AJbian of Koudiat el Beida (North of J. Mrhila, Central Tunisia). Biostratigr...
El Amri Zaineb, Zaghbib-Turki Dalila, Karoui-Yaakoub Narjess. Biostratigraphie des foraminifères pla...
Planktonic foraminifera from sections in predominantly pelagic and hemipelagic sediments of Late Al...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...
International audienceSince the end of the 19th century the interval comprising the uppermost Upper ...