Middle-Late Devonian Conodont Fauna of Bahram Formation in the East of Chatroud, Kerman

رخساره‌های رسوبی

Article 3, Volume 14, Issue 1 - Serial Number 26, September 2021

Document Type: Original Article

DOI: 10.22067/sed.facies.2021.47081

Authors

Zamani Fatane¹; Mehdi Yazdi^{* 2}; Ali Bahrami³; Hamed Ameri⁴

¹Ph.D. student in Stratigraphy & Paleontology, Department of Geology, Faculty of Sciences, University of Isfahan, Isfahan, Iran

²Professor, Department of Geology, Faculty of Sciences, University of Isfahan, Isfahan, Iran

³Associate Professor, Department of Geology, Faculty of Sciences, University of Isfahan, Isfahan, Iran

⁴Assistant Professor, Department of Ecology, Institute of Science and High Technology and Environmental Science, Graduate University of Advanced Technology, Kerman, Iran

Abstract

Devonian deposits of the Bahram Formation with a thickness of 458 m in the Bondar section 8 km east of Chatroud city in the structural zone of Central Iran were studied based on conodont fauna. According to 44 species and subspecies have been identified and based on their stratigraphic development, ten conodont biozones can be distinguished, which indicate the middle Givetian to upper Famennian age. The middle Givetian ansatus Zone and also the late Famennian Bispathodus aculeatus aculeatus Zone determine the oldest and newest reported age and determine the widest sequence of Bahram Formation in Kerman region. The first occurrence of Ancyrodella rotundiloba pristina marks the Givetian/Frasnian boundary in Sample B11.

Keywords

Devonian; conodont; Givetian; Famennian; Bahram Formation; Kerman

References