Lower Aptian rudist faunas from Croatia consist of Requienia? zlatarskii PAQUIER, Toucasia sp., Agriopleura sp., Glossomyophorus costatus MASSE, SKELTON & SLISKOVIC, Himeraelites sp. and Offneria sp. This assemblage has a clear Southern Tethyan (Arabo–African) significance and typifies the Early Aptian. Faunas from the interior of the Adriatic Carbonate Platform in Istria are dominated by Requieniidae while those from the northeastern area in the vicinity of Tounj–Ogulin, close to the platform margin, exhibit a higher diversity and include, beside requieniids, Caprinidae, Caprotinidae and Monopleuridae, in conjunction with evidence of open marine conditions
Abstract: The lithological and faunal succession cropping out close to the famous palaeontological l...
Upper Cretaceous to Lower Palaeogene shallow marine carbonates are the youngest deposits on the Brač...
Upper Cretaceous carbonate sediments characterized by rudist bivalves are extensively distributed in...
Lower Aptian rudist faunas from Croatia consist of Requienia? zlatarskii PAQUIER, Toucasia sp., Agri...
Rudist bivalves are abundant in Upper Cretaceous Adriatic carbonate platform deposits in biostromes ...
Rudist bivalves thrived commonly in the shallow carbonate platforms of the Cretaceous Tethyan realm....
The shallow marine carbonate deposits on the island of Cres, overlying deeper-water Cenomanian–Turon...
Rudists, especially members of the family Hippuritidae, were common dwellers on the Adriatic Carbona...
The larger benthic foraminifera Cretaciclavulina gusici n. gen., n. sp. is described from the lower ...
The Upper Cretaceous (Middle Cenomanian-Coniacian) successions of the Bey Daglari Carbonate Platform...
Lower Cretaceous (Aptian) shallow-marine limestones with intercalated polymictic conglomerates were ...
In the western Black Sea region of Turkey (Zonguldak area), Late Aptian rudist-bearing carbonates (t...
Synsedimentary tectonics caused significant differentiation of sedimentary environments of the Adria...
Chondrodonta joannae (Choffat) is a morphologically variable oyster-like bivalve with a predominatel...
To the present knowlege according to DERCOURT et al. (1985) the following Upper Cretaceous rudist su...
Abstract: The lithological and faunal succession cropping out close to the famous palaeontological l...
Upper Cretaceous to Lower Palaeogene shallow marine carbonates are the youngest deposits on the Brač...
Upper Cretaceous carbonate sediments characterized by rudist bivalves are extensively distributed in...
Lower Aptian rudist faunas from Croatia consist of Requienia? zlatarskii PAQUIER, Toucasia sp., Agri...
Rudist bivalves are abundant in Upper Cretaceous Adriatic carbonate platform deposits in biostromes ...
Rudist bivalves thrived commonly in the shallow carbonate platforms of the Cretaceous Tethyan realm....
The shallow marine carbonate deposits on the island of Cres, overlying deeper-water Cenomanian–Turon...
Rudists, especially members of the family Hippuritidae, were common dwellers on the Adriatic Carbona...
The larger benthic foraminifera Cretaciclavulina gusici n. gen., n. sp. is described from the lower ...
The Upper Cretaceous (Middle Cenomanian-Coniacian) successions of the Bey Daglari Carbonate Platform...
Lower Cretaceous (Aptian) shallow-marine limestones with intercalated polymictic conglomerates were ...
In the western Black Sea region of Turkey (Zonguldak area), Late Aptian rudist-bearing carbonates (t...
Synsedimentary tectonics caused significant differentiation of sedimentary environments of the Adria...
Chondrodonta joannae (Choffat) is a morphologically variable oyster-like bivalve with a predominatel...
To the present knowlege according to DERCOURT et al. (1985) the following Upper Cretaceous rudist su...
Abstract: The lithological and faunal succession cropping out close to the famous palaeontological l...
Upper Cretaceous to Lower Palaeogene shallow marine carbonates are the youngest deposits on the Brač...
Upper Cretaceous carbonate sediments characterized by rudist bivalves are extensively distributed in...