Late Albian ammonites from the Aitamir Formation (Koppeh Dagh,northeast Iran) |
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Institution: | 1. State Key Laboratory of Systematic and Evolutionary Botany, Institute of Botany, Chinese Academy of Sciences, Xiangshan, Beijing 100093, PR China;2. University of the Chinese Academy of Sciences, Beijing 100049, PR China;3. Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia;4. Centre for Past Climate Change, School of Archaeology, Geography and Environmental Sciences, University of Reading, Whiteknights, Reading, UK;5. Senckenberg Research Institute and Natural History Museum, Senckenberganlage 25, D-60325, Frankfurt/Main, Germany;6. Department of Palaeontology, University of Vienna, Althanstrasse 14, Vienna A-1090, Austria;7. Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu, Nepal;8. Birbal Sahni Institute of Palaeobotany, University Road, Lucknow 226007, India;1. Central Scientific Research Institute of Geology of Industrial Minerals, ul. Zimina 4, Kazan, 420097, Russia;2. Kazan (Volga region) Federal University, ul. Kremlyovskaya 18, Kazan, 420008, Russia |
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Abstract: | Late Albian ammonite faunas from the Aitamir Formation of the Koppeh Dagh Basin in northeast Iran are described and illustrated. These comprise 14 taxa, several of which are recorded from Iran for the first time, namely Anahoplites planus (formerly recorded from central Iran in open nomenclature only), Semenoviceras solidus, Epihoplites (Metaclavites) iphitus, Hysteroceras orbignyi and Pseudhelicoceras robertianum. New records of Placenticeras grossouvrei extend the stratigraphic range of this species downwards into the Late Albian; previously it was known from the Early and Middle Cenomanian only. The record of the rare E. (M.) iphitus fills a palaeobiogeographic gap between Crimea and Tajikistan, and the holotype of Spath is re-illustrated here. Additionally, Epihoplites trapezoidalis, from the Late Albian of Tajikistan, is relegated into the synonymy of Spath's species. A large number of taxa typical of the Late Albian (upper part of the Gault Clay Formation) of northwest Europe indicate close palaeobiogeographic affinities with the Koppeh Dagh Basin and faunal exchange across the Russian Platform and Transcaspia. The stratigraphic succession of the ammonite faunas is used for a biostratigraphic subdivision of the upper Aitamir Formation. |
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Keywords: | Early Cretaceous Systematic palaeontology Biostratigraphy Palaeobiogeography |
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