Early Miocene (Aquitanian-Burdigalian) Clypeaster and schizaster fauna (Echinoidea: Clypeasteroida, spatangoida) from firat formation, Diyarbakir, southeastern anatolia

dc.contributor.authorEkin, İhsan
dc.date.accessioned2021-12-29T05:54:16Z
dc.date.available2021-12-29T05:54:16Z
dc.date.issued2021en_US
dc.departmentFakülteler, Mühendislik Fakültesi, Enerji Sistemleri Mühendisliği Bölümüen_US
dc.description.abstractSpecies belonging to Clypeasteroida and Spatangoida orders are common and abundant in carbonate deposits of the Miocene sedimentary sequences of the Mediterranean region. The current paper deals with the notifying of the Clypeaster and Schizaster fauna (Echinoidea: Clypeasteroida, Spatangoida) from early Miocene (Aquitanian-Burdigalian) of the Firat Formation in Diyarbakir (Egil town), Southeastern Anatolia (Turkey), and their palaeoenvironmental conditions. Eleven specimens have been detected as follows: Clypeaster latirostris (Michelin, 1861) (specimen CLL-1, CLL-2), Clypeaster michelotti (Agassiz, 1840) (specimen CLM), Clypeaster altus (Klein, 1734) (specimen CLA) and Clypeaster intermedius (Des Moulins, 1837) (specimen CLI-1, CLI-2) from Clypeasteroida order, and Schizaster eurynotus (Sismonda, 1841) (specimen SCE-1, SCE-2), Schizaster parkinsoni (Defrance, 1827), (specimen SCP-1, SCP-2) and Schizaster lovisatoi (Cotteau, 1895) (specimen SCL) from Spatangoida order. Southeastern Anatolia consists of soil and rock units (approximately 120,000 km(2)) from the Cambrian to the Miocene. The Miocene sequences of Southeastern Anatolia extend to cermik, Ergani, Dicle, Egil and Hani districts (Diyarbakir) in the north, and Harran (Urfa) and the Syrian border in the south. The article creates an annotated species list with notes on specific aspects of palaeogeographic distribution of Echinoids (Clypeasteroida, Spatangoida) from the early Miocene of Firat Formation in Southeastern Anatolia. Furthermore, since the fossil species identified prefer neritic and sandy-clay habitats, they indicate the tropical climate of the region and become useful for paleoenvironmental reconstructions. Lastly, these data will contribute to providing data for new paleoenvironmental studies by palaeontologists and geologists, and be a pioneer for new fossil records and paleological studies.en_US
dc.identifier.citationEkin, İ. (2021). Early Miocene (Aquitanian–Burdigalian) Clypeaster and Schizaster fauna (Echinoidea: Clypeasteroida, Spatangoida) from Fırat Formation, Diyarbakır, Southeastern Anatolia. Arabian Journal of Geosciences, 14(23), 1-23.en_US
dc.identifier.doi10.1007/s12517-021-09035-6en_US
dc.identifier.issue23en_US
dc.identifier.orcid0000-0002-3682-9756en_US
dc.identifier.urihttps://dx.doi.org/10.1007/s12517-021-09035-6
dc.identifier.urihttps://hdl.handle.net/11503/1965
dc.identifier.volume14en_US
dc.institutionauthorEkin, İhsan
dc.language.isoen
dc.publisherSPRINGERen_US
dc.relation.ispartofARABIAN JOURNAL OF GEOSCIENCESen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectClypeasteren_US
dc.subjectSchizasteren_US
dc.subjectEarly Mioceneen_US
dc.subjectFırat Formationen_US
dc.subjectSoutheastern Anatoliaen_US
dc.titleEarly Miocene (Aquitanian-Burdigalian) Clypeaster and schizaster fauna (Echinoidea: Clypeasteroida, spatangoida) from firat formation, Diyarbakir, southeastern anatoliaen_US
dc.typeArticle

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