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The Senonian Ophiolitic Mirlange of the Ankara Mirlange Supergroup includes numerous blocks of radiolarian cherts. These blocks contain various radiolarian assemblages from the Albian to the Turonian (Pseudodictyomitra pseudomacrocephala, Thanarla tieneta), the Lower Cretaceous (Thanarla conica, Alievium helenae, Pseudodictyomitra carpatica), the Kimmeridgian-Tithonian (Ristola altissima, Sethocapsa cetia, Podocapsa umphitreptera) and the lower Jurassic (Parahsuum simplum). Upper Norian radiolarians were obtained from two of these blocks. The assemblage is represented by Betraccium deweveri Pessagno and Blome, Ferresium t riquetrum Carter, Pylostephanidium ankaraense n. sp. (Genus Pylostephanidizinz was formerly unknown in the upper Triassic) and other taxa. Thus, upper Norian fauna of Turkey exhibits close similarity to the radiolarian assemblages of western North America, Eastern Russia, Japan and the Philippines. This provides further evidence for the correlation of Mediterranean and Pacific Triassic sequences. These data allow for the conclusion that the sedimentation of radiolarian cherts was common in this part of Tethys during the Late Triassic and the Jurassic.

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