Abstract

Shark teeth discovered in the late Paleocene-early Eocene Chehel-Kaman Formation in NE Iran bring new data on the fossil fish record from this country. Two genera from the location are described and figured. The present record is one of the very few reports of fossil shark teeth from the Cenozoic of Iran and the first one from this formation and region. The marine vertebrates known from this region of the Tethys Sea are very scarce.

Highlights

  • The Cenozoic fossil sharks are poorly known in Iran. only a few other records from this country are known, but their exact origin is in general vague and none of them originate in the Kopet-dagh basin

  • The rest of fossil Chondrichthyes reported from Iran belong exclusively to the Paleozoic, forming a rather diverse fauna

  • The study area is located in the North-Khorasan province, northeast Iran (Fig. 1). during the last decades a lot of geological investigations have been led in this region, especially in the fields of litho- and biostratigraphy, this tectono-sedimentary zone requires additional further studies in other different fields of research as well

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Summary

Introduction

The Cenozoic fossil sharks are poorly known in Iran. only a few other records from this country are known (adNET et al, 2009; owFI et al, 2016), but their exact origin is in general vague and none of them originate in the Kopet-dagh basin. The Cenozoic fossil sharks are poorly known in Iran. Only a few other records from this country are known (adNET et al, 2009; owFI et al, 2016), but their exact origin is in general vague and none of them originate in the Kopet-dagh basin. The rest of fossil Chondrichthyes reported from Iran belong exclusively to the Paleozoic, forming a rather diverse fauna (hamPE, 2000; loNG & haIraPETIaN, 2000; YazdI & TurNEr, 2000; haIraPETIaN et al, 2008; haIraPETIaN & GINTEr, 2010; habIbI & GINTEr, 2011).

Geological Setting
Materials and methods
Systematic paleontology
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