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LATE DEVONIAN (FRASNIAN) CORALS FROM CENTRAL DOLPO, NEPAL

open access: yesRivista Italiana di Paleontologia e Stratigrafia, 1993
Rivista Italiana di Paleontologia e Stratigrafia (Research In Paleontology and Stratigraphy), V.
FLUEGEL, HELMUT, TINTORI, ANDREA
openaire   +3 more sources

Biochemostratigraphy of the Upper Frasnian in the Namur–Dinant Basin, Belgium: Implications for a global Frasnian–Famennian pre-event [PDF]

open access: yesPalaeogeography, Palaeoclimatology, Palaeoecology, 2012
The Upper Frasnian sequence of the Namur–Dinant Basin in southern Belgium consists of mixed siliclastic–carbonate succession of a ramp setting, where the sequence spans the rhenana–linguiformis conodont zones. Earlier studies investigated the chemostratigraphic variations during the Frasnian–Famennian event, but little has been yet known about the ...
Azmy, Karem   +2 more
openaire   +2 more sources

Iron microbial communities in Belgian Frasnians carbonate mounds

open access: yesFacies, 2001
The Belgian Frasnian carbonate mounds occur in three stratigraphic levels in an overall backstepping succession. Petit-Mont and Arche Members form the famous red and grey “marble” exploited for ornamental stone since Roman times. The evolution and distribution of the facies in the mounds is thought to be associated with ecologic evolution and relative ...
Boulvain, Frédéric   +4 more
openaire   +1 more source

Frasnian carbonate mounds from Belgium:sedimentology and palaeoceanography

open access: yesGeological Society, London, Special Publications, 2007
Abstract The facies architecture, sedimentary dynamics and palaeogeographic evolution were reconstructed for a number of middle-late Frasnian carbonate mounds from the south side of the Dinant Synclinorium (Belgium). Nine facies were recognized in the buildups, each characterized by a specific range of textures and assemblage of organisms ...
openaire   +2 more sources

Biostratigraphy and biogeography of Frasnian, Upper Devonian conodonts [PDF]

open access: yesThe Paleontological Society Special Publications, 1992
Analysis of Frasnian conodont sequences in the Montagne Noire, southern France, results in the recognition of a conventional zonation consisting of thirteen zones. Graphic correlation of eight Montagne Noire sections with a total of 11 sections in the Alberta Rockies, the Hay River-Trout River areas of the southern Northwest Territories, Canada, the ...
openaire   +1 more source

Frasnian

open access: yes, 2006
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 ...
Coen-Aubert, M., Boulvain, Frédéric
openaire   +1 more source

Late Frasnian Atrypida (Brachiopoda) from Poland and the Frasnian-Famennian biotic crisis

open access: yes, 1998
Late Frasnian Atrypida (Brachiopoda) from the Holy Cross Mountains, Poland, include 15 taxa and were widely distributed in foreslope habitats of the declining Dyminy Reef complex. The PaJmatolepis semichatovae transgression, followed by the transgressivehypoxic Lower Kellwasser (KW) Event during the Palmatolepis rhenana Zone did not have catastrophic ...
Racki, Grzegorz, Baliński, Andrzej
openaire   +2 more sources

Frasnian (Late Devonian) foraminiferal biostratigraphy from Taurides, southern Turkey

open access: yesStratigraphy, 2011
The stratigraphic sections Halevikdere, Kocadere and Eceli covering the Devonian succession in the Eastern and Central Taurides have been measured and studied for biostratigraphy, geochemistry, sedimentology and facies in the context of the project "Devonian Ecosystems andClimate of Turkey (DEVEC-TR)".
openaire   +2 more sources

Givetian/Frasnian (Middle/Upper Devonian) transition in the eastern Taurides, Turkey

open access: yesTURKISH JOURNAL OF EARTH SCIENCES, 2019
Devonian strata, including siliciclastic and carbonate rocks that were deposited in shallow marine to coastal environments, are widely distributed in the eastern Taurides of southern Turkey. To document the regional formation of the Givetian (Middle Devonian)/ Frasnian (Upper Devonian) boundary, a section in the eastern Taurides was studied in high ...
Recep ÖZKAN   +11 more
openaire   +4 more sources

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