A coral biostrome from the lower Hauterivian of the Neuquén Basin, west-central Argentina, was examined in detail. Taxonomic analysis established it as a monospecific assemblage of the scleractinian colonial coral Stereocaenia triboleti (Koby). Palaeoecological analysis of the species allows us to infer that it was an opportunistic species, capable of thriving in mixed carbonatesiliciclatic environments, on a soft substrate under a moderate to low sedimentation rate showing great regenerative capacity. Taphonomic analysis, together with lithofacies and microfacies analysis, allowed us to establish that the coral biostrome was deposited in a middle ramp setting under open marine and well-oxygenated conditions. Corals colonized a soft substra...
Coral reefs represent one of the main carbonate factories that contributed to the control of the str...
During the Early Miocene, coincident with the Sardinia-Corsica block rotation, mixed carbonate-silic...
During the Early Miocene, coincident with the Sardinia–Corsica block rotation, mixed carbonate–silic...
During the Middle Oxfordian, the epicontinental shelf of the Neuquén Basin was a site of major coral...
The Neuquén back-arc basin is located on the west margin of the South American platform between lati...
This contribution is the third contribution to the systematic description of the coral fauna recorde...
Several beds hosting corals are found within the marine members of the Agrio Formation (Lower Cretac...
This contribution presents the second part of the results of an ongoing systematic revision of the c...
Coral bioconstructions associated with mixed carbonate-siliciclastic settings are known to be strong...
Coral carpets are biostromes that form laterally continuous but low-relief (typically less than 1-me...
Coral-rich deposits and coral bioconstructions characterize the mixed carbonate-siliciclastic system...
23 pagesInternational audienceDuring the Miocene, Mediterranean shallow-water carbonates were rich i...
International audienceVery large amount of microbialites, up to 70% of the reef volume takes part in...
During the Miocene, Mediterranean shallow-water carbonates were rich in scleractinian corals, which ...
We describe a small microbial reef and associated limestones occurring in a Maastrichtian transgress...
Coral reefs represent one of the main carbonate factories that contributed to the control of the str...
During the Early Miocene, coincident with the Sardinia-Corsica block rotation, mixed carbonate-silic...
During the Early Miocene, coincident with the Sardinia–Corsica block rotation, mixed carbonate–silic...
During the Middle Oxfordian, the epicontinental shelf of the Neuquén Basin was a site of major coral...
The Neuquén back-arc basin is located on the west margin of the South American platform between lati...
This contribution is the third contribution to the systematic description of the coral fauna recorde...
Several beds hosting corals are found within the marine members of the Agrio Formation (Lower Cretac...
This contribution presents the second part of the results of an ongoing systematic revision of the c...
Coral bioconstructions associated with mixed carbonate-siliciclastic settings are known to be strong...
Coral carpets are biostromes that form laterally continuous but low-relief (typically less than 1-me...
Coral-rich deposits and coral bioconstructions characterize the mixed carbonate-siliciclastic system...
23 pagesInternational audienceDuring the Miocene, Mediterranean shallow-water carbonates were rich i...
International audienceVery large amount of microbialites, up to 70% of the reef volume takes part in...
During the Miocene, Mediterranean shallow-water carbonates were rich in scleractinian corals, which ...
We describe a small microbial reef and associated limestones occurring in a Maastrichtian transgress...
Coral reefs represent one of the main carbonate factories that contributed to the control of the str...
During the Early Miocene, coincident with the Sardinia-Corsica block rotation, mixed carbonate-silic...
During the Early Miocene, coincident with the Sardinia–Corsica block rotation, mixed carbonate–silic...