Conodonts (34 species and subspecies) from the Hojedk section north of Kerman span the late Givetian to early Famennian. The new data suggest that Devonian biostromes in central and eastern Iran were deposited on differing levels, and that the currently accepted ranges of Icriodus excavatus, Polygnathus subincompletus and P. mosquensis are late Givetian - late Frasnian, early to late Frasnian, and middle to late Frasnian. Polygnathus ashourii n. sp. is proposed.
The conodont fauna from the Devonian–Carboniferous Shahmirzad section, located in the Central Alborz...
The Givetian and Frasnian conodont suc cession investigated in the Compte section (Spanish Pyrenees)...
A rich and diverse conodont fauna represented by fifty-six taxa belonging to fifteen genera is descr...
Conodonts (34 species and subspecies) from the Hojedk section north of Kerman span the late Givetian...
The study of the conodont fauna from the Upper Devonian Shams Abad section provides new data on the ...
International audienceDevonian deposits of the Bahram Formation with a thickness of 300 m were studi...
The Middle - Late Devonian boundary is investigated based on twenty-two conodont species and subspec...
The study of the conodont fauna from the Bahram Formation in the Sar-e-Ashk section provides new dat...
International audienceThe Givetian to Famennian (Middle-Upper Devonian) Bahram Formation deposits (B...
Conodont data from acid-leaching 110 samples from two Late Devonian-Carboniferous areas in the Shoto...
Sixty-three conodont species and subspecies from the Kal-e-Sardar section indicate that the strata s...
Abstract Devonian deposits of the Bahram Formation with a thickness of 300 m were studied based on c...
4A rich and diverse conodont fauna from upper Frasnian and lower-middle Famennian strata in three se...
The Frasnian-Famennian (F-F) boundary in Central Iran has been investigated on the basis of conodont...
A relatively complete conodont record from Famennian to the Mississippian/Pennsylvanian boundary was...
The conodont fauna from the Devonian–Carboniferous Shahmirzad section, located in the Central Alborz...
The Givetian and Frasnian conodont suc cession investigated in the Compte section (Spanish Pyrenees)...
A rich and diverse conodont fauna represented by fifty-six taxa belonging to fifteen genera is descr...
Conodonts (34 species and subspecies) from the Hojedk section north of Kerman span the late Givetian...
The study of the conodont fauna from the Upper Devonian Shams Abad section provides new data on the ...
International audienceDevonian deposits of the Bahram Formation with a thickness of 300 m were studi...
The Middle - Late Devonian boundary is investigated based on twenty-two conodont species and subspec...
The study of the conodont fauna from the Bahram Formation in the Sar-e-Ashk section provides new dat...
International audienceThe Givetian to Famennian (Middle-Upper Devonian) Bahram Formation deposits (B...
Conodont data from acid-leaching 110 samples from two Late Devonian-Carboniferous areas in the Shoto...
Sixty-three conodont species and subspecies from the Kal-e-Sardar section indicate that the strata s...
Abstract Devonian deposits of the Bahram Formation with a thickness of 300 m were studied based on c...
4A rich and diverse conodont fauna from upper Frasnian and lower-middle Famennian strata in three se...
The Frasnian-Famennian (F-F) boundary in Central Iran has been investigated on the basis of conodont...
A relatively complete conodont record from Famennian to the Mississippian/Pennsylvanian boundary was...
The conodont fauna from the Devonian–Carboniferous Shahmirzad section, located in the Central Alborz...
The Givetian and Frasnian conodont suc cession investigated in the Compte section (Spanish Pyrenees)...
A rich and diverse conodont fauna represented by fifty-six taxa belonging to fifteen genera is descr...