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    Palaeozoic (Silurian–Devonian) cherts from the Balkan Terrane, western Bulgaria: geochemistry, biostratigraphy and depositional settings

    Palaeozoic (Silurian and Devonian) bedded cherts from the Balkan Terrane in western Bulgaria occur in three tectonic units: Svoge, Lyubash-Golo Bardo, and Morava. The Silurian and Devonian ages of the chert-be...

    Iliana Boncheva, Polina Andreeva in Palaeobiodiversity and Palaeoenvironments (2023)

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    Conodont stratigraphy and conodont biofacies of the shallow-water Kuh-e-Bande-Abdol-Hossein section (SE Anarak, Central Iran)

    The Middle to Upper Devonian Kuh-e-Bande-Abdol-Hossein section in eastern Central Iran is an overall shallow marine, nearshore to open marine facies setting that contains a highly variable conodont record gene...

    Ali Bahrami, Peter Königshof in Palaeobiodiversity and Palaeoenvironments (2019)

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    Conodont biostratigraphy of the Kesheh and Dizlu sections, and the age range of the Bahram Formation in central Iran

    Conodont fauna from the Kesheh and Dizlu sections in the North Isfahan province were investigated. Shallow-water and/or near-shore conodonts, mainly belonging to the icriodidpolygnathid biofacies, dominate the c...

    Ali Bahrami, Peter Königshof, Iliana Boncheva in Palaeobiodiversity and Palaeoenvironments (2018)

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    A Late Devonian (Frasnian) bryozoan fauna from central Iran

    A bryozoan fauna from the Late Devonian (Frasnian) of the Bahram Formation of the Zefreh section in central Iran contains four species: three trepostomes and one rhabdomesine cryptostome. Two species are new: ...

    Andrej Ernst, Peter Königshof, Ali Bahrami in Palaeobiodiversity and Palaeoenvironments (2017)

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    Palaeoenvironmental study of the Palaeotethys Ocean: the Givetian-Frasnian boundary of a shallow-marine environment using combined facies analysis and geochemistry (Zefreh Section/Central Iran)

    The Zefreh section in central Iran represents a carbonate ramp succession with a general shallow-marine palaeoenvironment. This section represents most of the Bahram Formation (Givetian to at least Middle falsiov...

    Peter Königshof, Sarah K. Carmichael in Palaeobiodiversity and Palaeoenvironments (2017)

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    Middle Devonian (Givetian) conodonts from the northern margin of Gondwana (Soh and Natanz regions, north-west Isfahan, Central Iran): biostratigraphy and palaeoenvironmental implications

    Four sections of mainly Middle Devonian (Givetian) shallow-marine rocks at the northern margin of Gondwana (Central Iran) were investigated with a special focus on the Bahram Formation, as the stratigraphic ra...

    Ali Bahrami, Peter Königshof, Iliana Boncheva in Palaeobiodiversity and Palaeoenvironments (2015)