Add to ORKGFollowing the end of Permian mass extinction, primitive groups of microbial communities emerged from stressed palaeoenvironments to recolonize the normal marine area of the Tethys. The prolific upper Paleozoic skeletal carbonate factory was abruptly replaced by a nonskeletal carbonate factor
The nature of Phanerozoic carbonate factories is strongly controlled by the composition of carbonate...
© 2017. A new Permian-Triassic boundary microbialite (PTBM) is described from the Xiajiacao section ...
International audienceThe extinction of most heavy calcifiers, such as corals, calcareous algae and ...
Following the end of Permian mass extinction, primitive groups of microbial communities emerged from...
During the first step of the very rapid and large scale lowest Triassic transgression , we note in d...
23 pagesInternational audiencePermian-Triassic boundary microbialites (PTBMs) are thin (0.05-15 m) c...
The end-Permian mass extinction was the most severe biotic crisis in Earth's history. In its direct ...
Shallow marine carbonate sediments that formed after the end-Permian mass extinction are rich in a t...
40 pagesInternational audienceThe Lower Triassic Mineral Mountains area (Utah, USA) preserves divers...
The Transcaucasia area (central Armenia) offers the opportunity to study a distinctive sponge-microb...
This paper can be accessed through the doi link below.Earliest Triassic microbialites (ETMs) and ino...
Early Triassic microbialites are distributed widely in the shallow marine facies of the Tethys Regio...
Stromatolites just after the end-Permian extinction are exceptionally well developed in the Chongyan...
The end-Permian mass extinction was the most severe biotic crisis in Earth’s history. In its direct ...
The nature of Phanerozoic carbonate factories is strongly controlled by the composition of carbonate...
© 2017. A new Permian-Triassic boundary microbialite (PTBM) is described from the Xiajiacao section ...
International audienceThe extinction of most heavy calcifiers, such as corals, calcareous algae and ...
Following the end of Permian mass extinction, primitive groups of microbial communities emerged from...
During the first step of the very rapid and large scale lowest Triassic transgression , we note in d...
23 pagesInternational audiencePermian-Triassic boundary microbialites (PTBMs) are thin (0.05-15 m) c...
The end-Permian mass extinction was the most severe biotic crisis in Earth's history. In its direct ...
Shallow marine carbonate sediments that formed after the end-Permian mass extinction are rich in a t...
40 pagesInternational audienceThe Lower Triassic Mineral Mountains area (Utah, USA) preserves divers...
The Transcaucasia area (central Armenia) offers the opportunity to study a distinctive sponge-microb...
This paper can be accessed through the doi link below.Earliest Triassic microbialites (ETMs) and ino...
Early Triassic microbialites are distributed widely in the shallow marine facies of the Tethys Regio...
Stromatolites just after the end-Permian extinction are exceptionally well developed in the Chongyan...
The end-Permian mass extinction was the most severe biotic crisis in Earth’s history. In its direct ...
The nature of Phanerozoic carbonate factories is strongly controlled by the composition of carbonate...
© 2017. A new Permian-Triassic boundary microbialite (PTBM) is described from the Xiajiacao section ...
International audienceThe extinction of most heavy calcifiers, such as corals, calcareous algae and ...