The evolution of locally tectonic-controlled foraminifera paleobiofacies formed as a result of this transgression 7.5-3.5 thousand years before present in the triple junction between entrance of Bosphorus in Northern Marmara Shelf-Mouth of Golden Horn-Üsküdar indicates that Mediterranean-Black Sea connection in late Quaternary was accomplished over Bosphorus as a result of tectonic-transgression association.
📌 3 Key Takeaways
🎯
Objective & Hypothesis:Young sediments in the shelf areas in the sea of Marmara have some faunal signs of Mediterranean transgression, Flandrian, developed following the Vürm period.
📊
Key Findings & Data:Young sediments in the shelf areas in the sea of Marmara have some faunal signs of Mediterranean transgression, Flandrian, developed following the Vürm period.
💡
Conclusion & Impact:The evolution of locally tectonic-controlled foraminifera paleobiofacies formed as a result of this transgression 7.5-3.5 thousand years before present in the triple junction between entrance of Bosphorus in Northern Marmara Shelf-Mouth of Golden Horn-Üsküdar indicates that Mediterranean-Black Sea connection in late Quaternary was accomplished over Bosphorus as a result of tectonic-transgression association.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters
Abstract
Young sediments in the shelf areas in the sea of Marmara have some faunal signs of Mediterranean transgression, Flandrian, developed following the Vürm period. The evolution of locally tectonic-controlled foraminifera paleobiofacies formed as a result of this transgression 7.5-3.5 thousand years before present in the triple junction between entrance of Bosphorus in Northern Marmara Shelf-Mouth of Golden Horn-Üsküdar indicates that Mediterranean-Black Sea connection in late Quaternary was accomplished over Bosphorus as a result of tectonic-transgression association.
🔖
Cite This Article
SAKINÇ, M. (1998). BENTHIC FORAMINIFERA (HOLOCENE) PALEOBIOFACIES OF BOSPHORUS (GOLDEN HORN - SARAYBURNU - ÜSKÜDAR): A NEW APPROACH TO MEDITERRANEAN-BLACK SEA WATERWAY. Maden Tetkik ve Arama Dergisi, Cilt: 120 - Sayı: 120, 118–119. https://ajindex.com/articles/54239
Barka, A.A. ve Kadinsky-Cade., 1988, Strike-Slip fault geometry in Turkey and its influence on earthguake activity. Tectonics, 7(3), 663-684
Bukry, D., 1973,
Coccolith stratigraphy, Eastern Eguatorial Pasific Leg. 16, Deep Sea Drilling Proc. XVI, 653-711.
Gökaşan, E.; Demirbağ, E.; Oktay; F.Y.; Ecevitoğlu, B.; Şimşek, M. ve Yüce, H., 1997, On the Origin of the Bosphorus. Marine Geology 140,183-199.
Göksu, Y.H.; Özer, M.A. ve Çetin, O., 1990, Mollüsk kavkılarının ESR yöntemi ile tarihlendirilmesi, istanbul Boğazı Güneyi ve Halic'in Geç Kuvaterner (Holosen ) dip tortulları (Ed: E.Meriç), 95-97, iTÜ Vakfı, Görür.N.; Çağatay, N.; Sakınç, M.; Sümengen, M.; Şentürk, K.; Yaltırak, CT. ve Chapalyga, A., 1997, Origin of the Sea of Marmara as deduced from the Neogene to Ouaternary Paleogeographic evolution of its frame. International Geological Rev. 39, 342-352.
Gücüm, A.H., 1990, istanbul Boğazı (Tüp Tünel) ve Haliç (Metro) sondajları, istanbul Boğazı Güneyi ve Halic'in Geç Kuvaterner (Holosen) dip tortulları (Ed: Meriç). 1-3, iTÜ Vakfı. Meriç, E. ve Sakınç, M., 1990, Foraminifera, istanbul Boğazı Güneyi ve Halic'in Geç Kuvaterner (Holosen) dip tortulları (Ed:Meriç), 15-41, iTÜ Vakfı. Meriç, E.; Oktay, Y.F.; Sakınç, M.; Gülen, D.; Ediger, Ş.V.; Meriç, N. ve Özdoğan, M., 1991 a, Kuşdili (Kadıköy) Kuvaterneri'nin Sedimenter Jeolojisi ve Paleoekolojisi. Cumhuriyet Üniv. Mühendislik Fak. Dergisi, Seri - Yerbilimleri 8, 1, 83-92. -; Oktay, Y.F.; Sakınç, M.; Gülen, O. ve inal, A., 1991 b, Ayamama (Bakırköy-lstanbul) Kuvaterneri'nin Sedimenter Jeolojisi ve Paleoekolojisi. Cumhuriyet Üniv. Mühendislik Fak. Dergisi, Seri-YerbiIimleri8, 1.93-100. -; Avşar, N. ve Çetin, O., 1996, Kuşdili (Kadıköy-lstanbul) Kuvaterneri'nin Stratigrafisi hakkında yeni görüşler. Yerbilimleri (Geosound), 29, 151, 159. Ryan, B.; Pitman, III.C.; Dimitrov, P.; Shimkus, K.; Majör, C.; Görür, N.; Sakınç, M. ve Yüce, H., 1997, An abrubt drowning of the Black Sea shelf. Marine Geology 138, 119-126.
Ross, D.A. ve Degens, ET., 1974, The Black Sea Geology Chemitstry and Biology. Mem. 20, 183-199,
A.A.P.G., Tulsa, USA. Sakınç, M., 1997, Marmara Kuzeyi'nin Holosen Paleobiyolojisi ve Akdeniz-Karadeniz Geç Kuvaterner su geçişi üzerine yeni bir yaklaşım. TÜBiTAK, MTA ÜNiVERSiTE. Deniz Jeolojisi Ulusal Deniz Araştırmaları VVorkshop III. Ankara Üniv Fen Fak. 44-50. -ve Bargu, S., 1989, izmit Körfezi Güneyi'ndeki Geç Pleyistosen (Tireniyen) çökel depolarının stratigrafisi ve Bölgenin Neo-Tektonik özellikleri. TJK