The most commonly used Lower and Middle Devonian conodont zonations that some times have been presented as standard zonations are evaluated. The author questions whether the Frasnian standard conodont zonation based on a phylogenetic succession of species belonging to the pelagicgenera Mesotaxis, Palmatolepis and Siphonodella can be used for world wide correlation. He fa vours the idea of an in ter national cono dont ref er ence scale based on a syn the sis of well established and documented conodont successions (with figured specimens of first and last occurrences of index-species) from key areas representing a variety of facies. Graphic correlation is likely to be the most objective and precise method to provide such a synthesis represent...
International audienceStudying the palaeobiology of extinct organisms relies on assessing the releva...
The Devonian record presents an opportunity to test and validate an existing marine bioregionalizati...
2Previous conodont studies on the Devonian/Carboniferous (D/C) boundary revealed that the current de...
The revision of the Famennian part of the “Late Devonian Standard Conodont Zonation” is based on the...
The revision of the Famennian part of the âLate Devonian Standard Conodont Zonationâ is based on the...
The proposed revision of the Famennian part of the Late Devonian Standard Conodont Zonation of Zieg...
The Devonian/Carboniferous boundary definition is under revision because of problems recognized in t...
The presented work consists of three separate papers that have been published in peer- reviewed jour...
Working on biostratigraphy of the late Silurian and of the early Devonian by means of conodont succe...
The Devonian–Carboniferous Boundary (DCB) was defined in the section La Serre trench E’ (Montagne No...
This paper is a contribution to the redefinition of the base of Carboniferous system. At present the...
Most of the Frasnian regional stages of the Ukhta region, South Timan, Russia, are composed of basin...
International audienceFour informal Lochkovian-Pragian conodont faunal intervals, FI 1 to FI 4 have ...
International audienceStudying the palaeobiology of extinct organisms relies on assessing the releva...
The Devonian record presents an opportunity to test and validate an existing marine bioregionalizati...
2Previous conodont studies on the Devonian/Carboniferous (D/C) boundary revealed that the current de...
The revision of the Famennian part of the “Late Devonian Standard Conodont Zonation” is based on the...
The revision of the Famennian part of the âLate Devonian Standard Conodont Zonationâ is based on the...
The proposed revision of the Famennian part of the Late Devonian Standard Conodont Zonation of Zieg...
The Devonian/Carboniferous boundary definition is under revision because of problems recognized in t...
The presented work consists of three separate papers that have been published in peer- reviewed jour...
Working on biostratigraphy of the late Silurian and of the early Devonian by means of conodont succe...
The Devonian–Carboniferous Boundary (DCB) was defined in the section La Serre trench E’ (Montagne No...
This paper is a contribution to the redefinition of the base of Carboniferous system. At present the...
Most of the Frasnian regional stages of the Ukhta region, South Timan, Russia, are composed of basin...
International audienceFour informal Lochkovian-Pragian conodont faunal intervals, FI 1 to FI 4 have ...
International audienceStudying the palaeobiology of extinct organisms relies on assessing the releva...
The Devonian record presents an opportunity to test and validate an existing marine bioregionalizati...
2Previous conodont studies on the Devonian/Carboniferous (D/C) boundary revealed that the current de...