Examination of samples from eight outcrops from Albian and Cenomanian of Estremadura, induced to take a census of sixty-two species and subspecies of Ostracodes among which fifteen are new and described here. Their associations pennited - first, to characterize three faunistic sets: a lower and middle Albian set with a mediolittoral and infralittoral (shallow marine} sedimentation; an upper Albian s.l. (near formations of Rudists}; a lagoonal lower Cenomanian; - on the other hand, to state local comparisons with the middle Cretaceous of Southern France, of the South-pyrenean Zone (Sierra d' Aulet: district of Sopeira), of the district of Oviedo (Northwestern Spain), and of the Aragonese Iberian Range (Aragon and Maestrazgo), placing in a...
Découverte au Portugal (Cabo Espichel), dans le sud-est de la France (Bouches-du RhBne: Crau, Var: e...
The evolution of the Portuguese Acanthopleuroceratinae is similar to the celto-souabe succession suc...
Glauconite K-Ar ages (6.88±0.4; 7.03±0.4 MY) confirm earlier reports to Upper Tortonian of silt beds...
Examination of samples from eight outcrops from Albian and Cenomanian of Estremadura, induced to tak...
The Domerian sections from the Lusitanian Basin of São Pedro de Muel, Rabaçal and Tomar have provide...
Forty-five species of ostracoda from the Aquitanian of the Lisbon area, belonging in thirty-two gene...
This paper presents a resume of the results achieved by researchers of the Centro de Estratigrafia e...
The biozonation of the portuguese Domerian is presented. This biozonation is based essentially on fa...
Some land and freshwater mollusks (Gastropoda, Pelecypoda) from three middle Miocene localities: Pêr...
The palynological study of sediments from lower levels of Lousã basin (Lomba do Alveite Arkoses), is...
The presence of Craspedochelys (Plesiochelys s.l.) at Romão, Portugal, indicates that, in that count...
The geological sections studied at the São Gião sector (Cantanhede region) have allowed the establis...
Les marnes de la partie supérieure de la Formation du Tigri du Crétacé supérieur des Hauts Plateaux ...
This study on middle Miocene Charophytes from the Tagus' basin indicates the presence of two species...
The Mid Miocene marine formations of Salles area (former "Sallomacian" stage) have been studied agai...
Découverte au Portugal (Cabo Espichel), dans le sud-est de la France (Bouches-du RhBne: Crau, Var: e...
The evolution of the Portuguese Acanthopleuroceratinae is similar to the celto-souabe succession suc...
Glauconite K-Ar ages (6.88±0.4; 7.03±0.4 MY) confirm earlier reports to Upper Tortonian of silt beds...
Examination of samples from eight outcrops from Albian and Cenomanian of Estremadura, induced to tak...
The Domerian sections from the Lusitanian Basin of São Pedro de Muel, Rabaçal and Tomar have provide...
Forty-five species of ostracoda from the Aquitanian of the Lisbon area, belonging in thirty-two gene...
This paper presents a resume of the results achieved by researchers of the Centro de Estratigrafia e...
The biozonation of the portuguese Domerian is presented. This biozonation is based essentially on fa...
Some land and freshwater mollusks (Gastropoda, Pelecypoda) from three middle Miocene localities: Pêr...
The palynological study of sediments from lower levels of Lousã basin (Lomba do Alveite Arkoses), is...
The presence of Craspedochelys (Plesiochelys s.l.) at Romão, Portugal, indicates that, in that count...
The geological sections studied at the São Gião sector (Cantanhede region) have allowed the establis...
Les marnes de la partie supérieure de la Formation du Tigri du Crétacé supérieur des Hauts Plateaux ...
This study on middle Miocene Charophytes from the Tagus' basin indicates the presence of two species...
The Mid Miocene marine formations of Salles area (former "Sallomacian" stage) have been studied agai...
Découverte au Portugal (Cabo Espichel), dans le sud-est de la France (Bouches-du RhBne: Crau, Var: e...
The evolution of the Portuguese Acanthopleuroceratinae is similar to the celto-souabe succession suc...
Glauconite K-Ar ages (6.88±0.4; 7.03±0.4 MY) confirm earlier reports to Upper Tortonian of silt beds...