RT Journal Article
T1 Particularidades de los macroforaminiferos del Cenomaniense de la Cordillera Ibérica: implicaciones paleobiogeográficas
T1 Some peculiarities of the Cenomanian Larger Foraminifera of Iberian Range: paleobiogeographic implications
A1 Calonge, Amelia
A1 Caus, E.
AB The distribution of Larger Foraminifera in the Iberian Range during the Cenomanian is being studied. The occurrence of Ovalveolina maccagnoae, Sellialveolina viallii and Pseudedomia drorimensis on the shelves of the lower depositional cycle (Upper Albian-Middle Cenomanian) implies a Tethysian origin of the sediments. In contrast, during the upper depositional cycle (Upper Cenomanian) the Larger Foraminifera assemblages are related to the Pyrenean Culf with the exception of Cisalveolina. Us occurrence in the north-eastern part of the Iberian Range, however, indicates a communication with the Tethys realm. The Cenomanian age attributed to the uppermost shallow platform facies implies that carbonate sedimentation stopped before the deposition of Middle Turonian hemipelagic sediments
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/11421
UL http://hdl.handle.net/10272/11421
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026