International audienceThe Givetian to Famennian (Middle-Upper Devonian) Bahram Formation deposits (Bondar and Shahzadeh Mohammad sections) in the Kerman region, Central Iran were sampled for conodonts. The conodonts were described, their distribution investigated, and the studied sections were correlated. In the previous conodont-based papers, the age of the Bahram Formation in the Kerman region was from the upper Givetian hermanni Zone to the middle Famennian Uppermost marginifera Zone (Middle to Late Devonian). However, the new results of this study show that the Bondar section spans from the middle Givetian ansatus Zone to the upper Famennian (middle part of the Middle expansa Zone=Bispathodus aculeatus aculeatus Zone) and the Shahzadeh ...
The Givetian and Frasnian conodont suc cession investigated in the Compte section (Spanish Pyrenees)...
Abstract Chelcheli section (397m thick) about 70 km northwest of Shahroud on the Shahroud-Gorgan roa...
5We present detailed biostratigraphy based on conodonts and palaeoenvironmental trends deduced from ...
International audienceThe Givetian to Famennian (Middle-Upper Devonian) Bahram Formation deposits (B...
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...
Abstract Devonian deposits of the Bahram Formation with a thickness of 300 m were studied based on c...
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 ...
A relatively complete conodont record from Famennian to the Mississippian/Pennsylvanian boundary was...
The study of the conodont fauna from the Bahram Formation in the Sar-e-Ashk section provides new dat...
Conodont data from acid-leaching 110 samples from two Late Devonian-Carboniferous areas in the Shoto...
The Frasnian-Famennian (F-F) boundary in Central Iran has been investigated on the basis of conodont...
4A rich and diverse conodont fauna from upper Frasnian and lower-middle Famennian strata in three se...
Sixty-three conodont species and subspecies from the Kal-e-Sardar section indicate that the strata s...
The Givetian and Frasnian conodont suc cession investigated in the Compte section (Spanish Pyrenees)...
Abstract Chelcheli section (397m thick) about 70 km northwest of Shahroud on the Shahroud-Gorgan roa...
5We present detailed biostratigraphy based on conodonts and palaeoenvironmental trends deduced from ...
International audienceThe Givetian to Famennian (Middle-Upper Devonian) Bahram Formation deposits (B...
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...
Abstract Devonian deposits of the Bahram Formation with a thickness of 300 m were studied based on c...
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 ...
A relatively complete conodont record from Famennian to the Mississippian/Pennsylvanian boundary was...
The study of the conodont fauna from the Bahram Formation in the Sar-e-Ashk section provides new dat...
Conodont data from acid-leaching 110 samples from two Late Devonian-Carboniferous areas in the Shoto...
The Frasnian-Famennian (F-F) boundary in Central Iran has been investigated on the basis of conodont...
4A rich and diverse conodont fauna from upper Frasnian and lower-middle Famennian strata in three se...
Sixty-three conodont species and subspecies from the Kal-e-Sardar section indicate that the strata s...
The Givetian and Frasnian conodont suc cession investigated in the Compte section (Spanish Pyrenees)...
Abstract Chelcheli section (397m thick) about 70 km northwest of Shahroud on the Shahroud-Gorgan roa...
5We present detailed biostratigraphy based on conodonts and palaeoenvironmental trends deduced from ...