In: Geologica Carpathica, vol. 63, no. 5
Atike Nazik - Senol Capkinoglu - Emine Seker
Details:
Year, pages: 2012, 355 - 363
Language: eng
Keywords:
Ostracods, conodonts, Famennian, Istanbul Zone, NW Turkey
Original source URL: http://www.geologicacarpathica.com/browse-journal/volumes/63-5/article-607/
About article:
Famennian (Late Devonian) ostracods of the Thuringian Mega-Assemblage were recovered for the first time from three incomplete sections of the Ayineburnu Member of the Büyükada Formation in the Denizliköy area (Gebze, NW Turkey), which were sampled for conodonts. Conodont faunas define an interval extending from the Upper rhomboidea? or Lower marginifera Zone into the Middle expansa Zone of the standard Upper Devonian conodont zonation. The ostracod faunas found here consist of species mainly with thin-walls, long spines and often smooth surfaces such as Rectonaria, Tricornina, Orthonaria, Triplacera, Beckerhealdia, Timorhealdia, Bohemina, Paraberounella and Acratia. These taxa indicate faunal relationship with Thuringia and the Rhenish Massif in Germany, the Cantabrian Mountains and Pyrenees in Spain, Holy Cross Mountains in Poland, North Africa and China.
How to cite:
ISO 690:
Nazik, A., Capkinoglu, S., Seker, E. 2012. Famennian ostracods from the Istanbul Zone (Gebze, Kocaeli, NW Turkey) and their paleogeographical relations. In Geologica Carpathica, vol. 63, no.5, pp. 355-363. 1335-0552. DOI: https://doi.org/10.2478/v10096-012-0028-0
APA:
Nazik, A., Capkinoglu, S., Seker, E. (2012). Famennian ostracods from the Istanbul Zone (Gebze, Kocaeli, NW Turkey) and their paleogeographical relations. Geologica Carpathica, 63(5), 355-363. 1335-0552. DOI: https://doi.org/10.2478/v10096-012-0028-0
About edition: