International audienceFour informal Lochkovian-Pragian conodont faunal intervals, FI 1 to FI 4 have been recognized in Lower Devonian sections yielding in the westernmost part of the Massif Armoricain. The conodont assemblages are in general not abundant, poorly diversified, and largely dominated by icriodids. The structural constraints induced poor preservation and fragmentation of conodont elements. Most conodont taxa are endemic and show close affinities with those of the Lower Devonian of Spain, mainly Celtiberia and the Guadarrama. One of the rare, widespread conodont species, is Masaraella pandora. A new morphotype, angustoides angustoides beta, is described. The vertical range of conodont taxa and the biostratigraphic interpretation ...
The conodont fauna from the Devonian–Carboniferous Shahmirzad section, located in the Central Alborz...
The Devonian/Carboniferous boundary definition is under revision because of problems recognized in t...
Abstract: The Late Devonian Gmßali formation of the eastern Taurides is a terrigenous-carbonate rock...
International audienceFour informal Lochkovian-Pragian conodont faunal intervals, FI 1 to FI 4 have ...
In the Podolian Dniester Basin (southwestern Ukraine) the Lower Devonian marine deposits are represe...
In the Podolian Dniester Basin (southwestern Ukraine) the Lower Devonian marine deposits are represe...
The problems around the Pragian/Emsian (P/E) boundary have been widely discussed by several authors,...
Conodont data from the Rio Malinfier section, located in the Cason di Lanza area (Carnic Alps, Italy...
The presented work consists of three separate papers that have been published in peer- reviewed jour...
A comprehensive conodont study of five sections of Emsian age, carried out in the Spanish Central Py...
2noThe ontogeny of the Lochkovian conodont species Ancyrodelloides carlsi (Boersma) is demonstrated ...
4siThe conodont stratigraphy of the lower Lochkovian part of the famous Cellon section is presented....
The problems around the Pragian/Emsian (P/E) boundary have been widely discussed by several authors,...
Conodont faunas were collected from the Devonian and Lower Carboniferous in an area ranging from the...
This work is focused on conodont biostratigraphy of the Silurian/Devonian boundary interval in the P...
The conodont fauna from the Devonian–Carboniferous Shahmirzad section, located in the Central Alborz...
The Devonian/Carboniferous boundary definition is under revision because of problems recognized in t...
Abstract: The Late Devonian Gmßali formation of the eastern Taurides is a terrigenous-carbonate rock...
International audienceFour informal Lochkovian-Pragian conodont faunal intervals, FI 1 to FI 4 have ...
In the Podolian Dniester Basin (southwestern Ukraine) the Lower Devonian marine deposits are represe...
In the Podolian Dniester Basin (southwestern Ukraine) the Lower Devonian marine deposits are represe...
The problems around the Pragian/Emsian (P/E) boundary have been widely discussed by several authors,...
Conodont data from the Rio Malinfier section, located in the Cason di Lanza area (Carnic Alps, Italy...
The presented work consists of three separate papers that have been published in peer- reviewed jour...
A comprehensive conodont study of five sections of Emsian age, carried out in the Spanish Central Py...
2noThe ontogeny of the Lochkovian conodont species Ancyrodelloides carlsi (Boersma) is demonstrated ...
4siThe conodont stratigraphy of the lower Lochkovian part of the famous Cellon section is presented....
The problems around the Pragian/Emsian (P/E) boundary have been widely discussed by several authors,...
Conodont faunas were collected from the Devonian and Lower Carboniferous in an area ranging from the...
This work is focused on conodont biostratigraphy of the Silurian/Devonian boundary interval in the P...
The conodont fauna from the Devonian–Carboniferous Shahmirzad section, located in the Central Alborz...
The Devonian/Carboniferous boundary definition is under revision because of problems recognized in t...
Abstract: The Late Devonian Gmßali formation of the eastern Taurides is a terrigenous-carbonate rock...