Scientific Quarterly Journal of Geosciences

Scientific Quarterly Journal of Geosciences

Revision in stratigraphic position of the Cephalopod Bed and the boundary between Devonian and Carboniferous and to introducing 5 Conodont zones in Hoze-Dorah (East Iran)

Document Type : Original Research Paper

Author
Ferdowsi University, Mashhad, Iran
Abstract
Conodonts of Cephalopod Bed of Shishtu Formation in its reference section in Howz-e-Dorah, south of Shotori Range, has been studied. The Cephalopod Bed, mainly consists of red oolittic limestone and shale which has a rich macrofossil fauna of cephalopoda, brachiopoda, corals and also a good fauna of conodonts.
Conodont study reveals an age of Late Frasnian to Late Famennian for the Cephalopod Bed. A condont zone in the Late Frasnian (gigas) and conodont zones in Famennian (Palmatolepis triangularis, rhomboidea and expansus) also have been introduced.
The previous studies indicated Devonian -Carboniferous boundary in a succession of 82 meters thick, which is overlain the Cephalopod Bed (Stocklin et al. 1965 and Stepanov, 1971). In this study the succession which contains Devonian- Carboniferous boundary reduced to 10 meters.
In Carboniferous conodont fauna the conodont zone of anchoralis- latus has been introduced.
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Volume 7, 25-26
Autumn & Winter 1998, vol. 7, No. 25-26
Winter 1998
Pages 10-17