The name Frasnian, which comes from the locality of Frasnes near Couvin in Belgium, was introduced by Gosselet in 1879 and was formally retained for the lower stage of the Upper Devonian by the Subcommission on Devonian Stratigraphy in 1981. The modern definition of the Frasnian is based on conodonts and the historical background of the stage is developed in detail herein. Data about the lithostratigraphy, sedimentology, biostratigraphy, chronostratigraphy and absolute age of the Frasnian can also been found in this contribution
The Devonian Coumiac carbonate series is well known since it is the point reference in time for the ...
About 2,450 carapaces, valves and fragments of ostracods have been extracted from 94 samples collect...
The Givetian Stage in the Givet area is represented by the main part of the Hanonet Fm, the Trois-Fo...
Eighty-nine samples have been collected for ostracods, from the stratotypes for the upper part of th...
Frechastraea coeni n. sp. is widely distributed at the base of the Late Frasnian from the Philippevi...
Frechastraea pentagona (Goldfuss, 1826), type species of Frechastraea Scrutton, 1968, F. minima (Roz...
The name of the Famennian stage originated in the 19th century from the Famenne region in southern B...
Samples from the Upper Frasnian (Devonian) of Lompret Quarry and Nismes railway section in Dinant Sy...
Abstract: Recent opening of the La Thure quarry in Western Belgium allowed the collection of new dat...
Above Givetian and Frasnian continental deposits, the Upper Frasnian transgression starts in the Boo...
A high-resolution correlation of 10 Frasnian sections in the Belgian Ardennes is made using the grap...
This paper focuses on the early and middle Frasnian stratigraphic interval from the Ardennes area in...
Ostracods from the Sourd d'Ave section have been collected in the Moulin Boreux and Fort Hulobiet Me...
Trilobites are recorded from Frasnian strata in Belgium on the basis of old museum collections and c...
This paper provides a synthetic sedimentological overview of themiddle Frasnian carbonate platform o...
The Devonian Coumiac carbonate series is well known since it is the point reference in time for the ...
About 2,450 carapaces, valves and fragments of ostracods have been extracted from 94 samples collect...
The Givetian Stage in the Givet area is represented by the main part of the Hanonet Fm, the Trois-Fo...
Eighty-nine samples have been collected for ostracods, from the stratotypes for the upper part of th...
Frechastraea coeni n. sp. is widely distributed at the base of the Late Frasnian from the Philippevi...
Frechastraea pentagona (Goldfuss, 1826), type species of Frechastraea Scrutton, 1968, F. minima (Roz...
The name of the Famennian stage originated in the 19th century from the Famenne region in southern B...
Samples from the Upper Frasnian (Devonian) of Lompret Quarry and Nismes railway section in Dinant Sy...
Abstract: Recent opening of the La Thure quarry in Western Belgium allowed the collection of new dat...
Above Givetian and Frasnian continental deposits, the Upper Frasnian transgression starts in the Boo...
A high-resolution correlation of 10 Frasnian sections in the Belgian Ardennes is made using the grap...
This paper focuses on the early and middle Frasnian stratigraphic interval from the Ardennes area in...
Ostracods from the Sourd d'Ave section have been collected in the Moulin Boreux and Fort Hulobiet Me...
Trilobites are recorded from Frasnian strata in Belgium on the basis of old museum collections and c...
This paper provides a synthetic sedimentological overview of themiddle Frasnian carbonate platform o...
The Devonian Coumiac carbonate series is well known since it is the point reference in time for the ...
About 2,450 carapaces, valves and fragments of ostracods have been extracted from 94 samples collect...
The Givetian Stage in the Givet area is represented by the main part of the Hanonet Fm, the Trois-Fo...