The Matmor Formation (Middle Jurassic, Callovian, 165-161 mya) in southern Israel contains abundant coral-sponge patch reefs and large crinoids which have been extensively bioeroded by bivalves, worms, barnacles, phoronids, and others producing eight ichnospecies. It is significant for the evolutionary history of bioerosion because this is the first equatorial Middle Jurassic boring ichnofauna to be documented. When compared to contemporaneous ichnofaunas, this assemblage is of average diversity and abundance but has only rare sponge borings and contains abundant specimens of Oichnus paraboloides as shallow pits on crinoid stems. The Matmor Formation surprisingly lacks carbonate hardgrounds, which are otherwise abundant in subtropical and t...
During the Early Jurassic, reefs in the shallow seas of the Atlas Rift experienced substantial chang...
International audienceLate Jurassic coral reefs are present in the Western High Atlas of Morocco alo...
Coral bioherms of the Vršatec Limestone that formed massive, several tens of meters thick complexes ...
Hamakhtesh Hagadol is an erosional cirque (a makhtesh) located in the northern Negev Desert. The Mat...
International audienceThe end of the Triassic and the Early Jurassic are intervals characterised by ...
The Matmor Formation is a set of late Callovian marls and limestones exposed in the Matmor Hills, Ha...
The Djebel Bou Dahar (DBD) carbonate platform (High Atlas, Morocco) developed in an intracratonic ri...
International audienceDuring the Late Jurassic, the Jura platform was the site of major carbonate pr...
The present study investigated traces of bioerosion in parautochthonous associations of oysters from...
A study across the major extinction phase of scleractinians during the Late Triassic/Early Jurassic ...
A diverse sclerozoan assemblages consisting of both encrusting and boring biota are described from t...
Sclerobiont assemblages in the Middle Jurassic Carmel Formation of southwest Utah, USA show paleoeco...
The Mesozoic Marine Revolution (MMR) was a major evolutionary episode involving the large-scale rest...
The Djebel Bou Dahar (DBD) carbonate platform (Early Jurassic, High Atlas, Morocco) was deposited on...
During the Early Jurassic, reefs in the shallow seas of the Atlas Rift experienced substantial chang...
International audienceLate Jurassic coral reefs are present in the Western High Atlas of Morocco alo...
Coral bioherms of the Vršatec Limestone that formed massive, several tens of meters thick complexes ...
Hamakhtesh Hagadol is an erosional cirque (a makhtesh) located in the northern Negev Desert. The Mat...
International audienceThe end of the Triassic and the Early Jurassic are intervals characterised by ...
The Matmor Formation is a set of late Callovian marls and limestones exposed in the Matmor Hills, Ha...
The Djebel Bou Dahar (DBD) carbonate platform (High Atlas, Morocco) developed in an intracratonic ri...
International audienceDuring the Late Jurassic, the Jura platform was the site of major carbonate pr...
The present study investigated traces of bioerosion in parautochthonous associations of oysters from...
A study across the major extinction phase of scleractinians during the Late Triassic/Early Jurassic ...
A diverse sclerozoan assemblages consisting of both encrusting and boring biota are described from t...
Sclerobiont assemblages in the Middle Jurassic Carmel Formation of southwest Utah, USA show paleoeco...
The Mesozoic Marine Revolution (MMR) was a major evolutionary episode involving the large-scale rest...
The Djebel Bou Dahar (DBD) carbonate platform (Early Jurassic, High Atlas, Morocco) was deposited on...
During the Early Jurassic, reefs in the shallow seas of the Atlas Rift experienced substantial chang...
International audienceLate Jurassic coral reefs are present in the Western High Atlas of Morocco alo...
Coral bioherms of the Vršatec Limestone that formed massive, several tens of meters thick complexes ...