This contribution presents the second part of the results of an ongoing systematic revision of the coral fauna from mixed carbonate-siliciclastic sedimentary facies of the Agrio Formation (upper Valanginian–upper Hauterivian) of the Neuquén Basin, west-central Argentina. Columastraeid corals (superfamily Cladocoroidea, that corresponds partly to the suborder Faviina) are represented by six species of the genus Eocolumastrea Löser and Zell, 2015, namely E. gortanii, E. magna, E. neuquensis, E. octaviae, E. cf. octaviae and E. sp. 2. Records of the species are close or match with their first appearances worldwide. The studied corals correspond to mostly ramose and secondarily massive colonies, that are here interpreted as capable of thriving ...
Especies de coral recolectadas en estratos del Cretácico Superior (Maastrichtiano), correspondientes...
El análisis tafonómico y paleoecológico del contenido fosilífero de la Formación Agrio del Cretácico...
Although putative corals of uncertain affinities occur in the early Cambrian, the earliest definite ...
This contribution presents the first results of an ongoing systematic revision of the coral fauna of...
This contribution is the third contribution to the systematic description of the coral fauna recorde...
A coral biostrome from the lower Hauterivian of the Neuquén Basin, west-central Argentina, was exami...
Several beds hosting corals are found within the marine members of the Agrio Formation (Lower Cretac...
The Neuquén back-arc basin is located on the west margin of the South American platform between lati...
One morphotype of sabellids (Sabellida, Sabellidae) and two of serpulids (Sabellida, Serpulidae), fo...
During the Middle Oxfordian, the epicontinental shelf of the Neuquén Basin was a site of major coral...
The small Maastrichtian coral fauna of Ocozocoautla (Chiapas, Mexico) is being taxonomically reviewe...
Silurian and Devonian corals occur abundantly in siliciclastic rocks of the Argentine Precordillera....
Coral carpets are biostromes that form laterally continuous but low-relief (typically less than 1-me...
The gastropod fauna of the Lower Cretaceous of the Argentinian Neuquén Basin contains three aporrhai...
The coral species from the Upper Cretaceous (Maastrichtian) strata of the Ocozocoautla Formation in ...
Especies de coral recolectadas en estratos del Cretácico Superior (Maastrichtiano), correspondientes...
El análisis tafonómico y paleoecológico del contenido fosilífero de la Formación Agrio del Cretácico...
Although putative corals of uncertain affinities occur in the early Cambrian, the earliest definite ...
This contribution presents the first results of an ongoing systematic revision of the coral fauna of...
This contribution is the third contribution to the systematic description of the coral fauna recorde...
A coral biostrome from the lower Hauterivian of the Neuquén Basin, west-central Argentina, was exami...
Several beds hosting corals are found within the marine members of the Agrio Formation (Lower Cretac...
The Neuquén back-arc basin is located on the west margin of the South American platform between lati...
One morphotype of sabellids (Sabellida, Sabellidae) and two of serpulids (Sabellida, Serpulidae), fo...
During the Middle Oxfordian, the epicontinental shelf of the Neuquén Basin was a site of major coral...
The small Maastrichtian coral fauna of Ocozocoautla (Chiapas, Mexico) is being taxonomically reviewe...
Silurian and Devonian corals occur abundantly in siliciclastic rocks of the Argentine Precordillera....
Coral carpets are biostromes that form laterally continuous but low-relief (typically less than 1-me...
The gastropod fauna of the Lower Cretaceous of the Argentinian Neuquén Basin contains three aporrhai...
The coral species from the Upper Cretaceous (Maastrichtian) strata of the Ocozocoautla Formation in ...
Especies de coral recolectadas en estratos del Cretácico Superior (Maastrichtiano), correspondientes...
El análisis tafonómico y paleoecológico del contenido fosilífero de la Formación Agrio del Cretácico...
Although putative corals of uncertain affinities occur in the early Cambrian, the earliest definite ...