Lower Devonian ostracods from the Istanbul area, Western Pontides (NW Turkey): Gondwanan and peri-Gondwanan affinities

Olempska, Ewa; NAZİK, ATİKE; ÇAPKINOĞLU, ŞENOL; SAYDAM-DEMIRAY, Dilek

doi:10.1017/s0016756814000296

Lower Devonian ostracods from the Istanbul area, Western Pontides (NW Turkey): Gondwanan and peri-Gondwanan affinities

Atıf İçin Kopyala

Olempska E., NAZİK A., ÇAPKINOĞLU Ş., SAYDAM-DEMIRAY D. G.

GEOLOGICAL MAGAZINE, cilt.152, sa.2, ss.298-315, 2015 (SCI-Expanded)

Yayın Türü: Makale / Tam Makale
Cilt numarası: 152 Sayı: 2
Basım Tarihi: 2015
Doi Numarası: 10.1017/s0016756814000296
Dergi Adı: GEOLOGICAL MAGAZINE
Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
Sayfa Sayıları: ss.298-315
Anahtar Kelimeler: Early Devonian, Ostracoda, Istanbul Terrane, Turkey, palaeogeography, palaeoecology, PALEOZOIC EVOLUTION, TERRANES, VARISCAN, STRATIGRAPHY, PALEOGEOGRAPHY, MOUNTAINS, GEOGRAPHY, SUTURES, HISTORY, KOCAELI
Çukurova Üniversitesi Adresli: Evet

A Lower Devonian silicified ostracod fauna has been recovered from limestone interbeds in the Buyukdere section of the Kozyatagi Member of the Pendik Formation. Forty-one species belonging to 33 genera have been recognized. Twenty-three are already known, and 15 are described in open nomenclature. One genus and three species (Omerliella rectangulata gen. et sp. nov., Microcheilinella istanbulensis sp. nov. and Roundyella goekchenae sp. nov.) are described. Silicified larval stages of trilobites, agglutinated foraminifers and conodonts co-occur with the ostracods. The ostracod assemblages are `mixed faunas', between the epineritic Eifelian Mega-Assemblage, representative of high-energy environments, and the basinal Thuringian Mega-Assemblage, representative of lowenergy environments. The conodont faunas of the Pendik Formation represent the serotinus, patulus and partitus biozones of the late Emsian -earliest Eifelian. The Emsian ostracods of NW Turkey show numerous species-level links between the Western Pontides (Istanbul Terrane) and assemblages of contemporaneous faunas of the Cantabrian Mountains (Spain), Morocco and Thuringia (Germany), and of similar biofacies. This supports the notion that the Istanbul Terrane, Armorican terrane-collage and northern margins of Gondwana were in geographical proximity in late Early Devonian time.

Lower Devonian ostracods from the Istanbul area, Western Pontides (NW Turkey): Gondwanan and peri-Gondwanan affinities

By:Olempska, E (Olempska, Ewa)^{[ 1 ]}; Nazik, A (Nazik, Atike)^{[ 2 ]}; Capkinoglu, S (Capkinoglu, Senol)^{[ 3 ]}; Saydam-Demiray, DG (Saydam-Demiray, Dilek Gulnur)^{[ 4 ]}