The stratigraphical position and the fossil content of several Triassic carbonate beds in the Betic Cordilleras are described. Three different conodont faunas have been found: one with Pseudofurnishius murcianus as the dominant species, a second in which Pseudofurnishius murcianus occurs together with Tardogondolella mungoensis mungoensis and a third in which Pseudofurnishius huddlei sp. nov. is the characteristic species
Conodonts are important index fossils for supra‐regional correlation especially in the Triassic. How...
The high intraspecific variability of conodont platform elements in the upper Carnian\u2013lower Nor...
More than one thousand and five hundreds specimens belonging to the squat coniform conodont Genus Ps...
Pseudofurnishius is a late Anisian (Pelsonian)–early Carnian (Cordevolian) conodont genus of gondole...
Pseudofurnishius is a late Anisian (Pelsonian)–early Carnian (Cordevolian) conodont genus of gondole...
Theree differents lithology can be differenciated basically in t he Triassic of the central sector o...
Conodonts are biostratigraphically very important microfossils in the Upper Triassic, occurring in d...
The base of the Norian Stage (Carnian/Norian boundary, Upper Triassic) is still awaiting a formal de...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) p...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) c...
By means of a field work, carried out in the Eastern Spain Triassic outcrops, (mainly Muschelkalk an...
The conodont fauna of the Rotelliforme, Meeki, Occidentalis and lower Subasperum zones of Nevada (Hu...
Slovenian Basin was formed during the Ladinian following disintegration of the Slovenian Carbonate P...
The high intraspecific variability of conodont platform elements in the upper Carnian–lower Norian i...
A small conodont fauna from limestone layers overlying the main limestone lens of the Triassic seque...
Conodonts are important index fossils for supra‐regional correlation especially in the Triassic. How...
The high intraspecific variability of conodont platform elements in the upper Carnian\u2013lower Nor...
More than one thousand and five hundreds specimens belonging to the squat coniform conodont Genus Ps...
Pseudofurnishius is a late Anisian (Pelsonian)–early Carnian (Cordevolian) conodont genus of gondole...
Pseudofurnishius is a late Anisian (Pelsonian)–early Carnian (Cordevolian) conodont genus of gondole...
Theree differents lithology can be differenciated basically in t he Triassic of the central sector o...
Conodonts are biostratigraphically very important microfossils in the Upper Triassic, occurring in d...
The base of the Norian Stage (Carnian/Norian boundary, Upper Triassic) is still awaiting a formal de...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) p...
New taxonomic and biostratigraphic investigations on the late Carnian to Rhaetian (Upper Triassic) c...
By means of a field work, carried out in the Eastern Spain Triassic outcrops, (mainly Muschelkalk an...
The conodont fauna of the Rotelliforme, Meeki, Occidentalis and lower Subasperum zones of Nevada (Hu...
Slovenian Basin was formed during the Ladinian following disintegration of the Slovenian Carbonate P...
The high intraspecific variability of conodont platform elements in the upper Carnian–lower Norian i...
A small conodont fauna from limestone layers overlying the main limestone lens of the Triassic seque...
Conodonts are important index fossils for supra‐regional correlation especially in the Triassic. How...
The high intraspecific variability of conodont platform elements in the upper Carnian\u2013lower Nor...
More than one thousand and five hundreds specimens belonging to the squat coniform conodont Genus Ps...