Abstract
The Strait of İstanbul (SoI) (Bosphorus) is a narrow valley, which has evolved tectonically from a stream, and in which thick sediment deposits have accumulated in the course of its evolution. Detailed seismic and multi-beam bathymetric data have revealed that the upper parts of the deeper channel deposits consist of parallel strata, which have mostly been eroded subsequently to their deposition. The resulting erosion surface is represented by the present channel floor in the strait, the estimated volume of the eroded material being approximately 2×108 m3 . Erosion rate and seafloor morphology indicate that the flow direction was from the south to the north. This inner channel may have been formed by an abrupt flooding of the Black Sea by Mediterranean waters at the beginning of the latest connection between the Marmara and the Black seas. Subsequently, the Mediterranean bottom current of the modern two-way flow system, which was established at about 5–4 ka b.p., has given the latest shape to the strait floor.
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References
Aksu AE, Hiscott RN, Yaşar D (1999) Oscillating Quaternary water levels of the Marmara Sea and vigorous outflow into the Aegean Sea from the Marmara Sea-Black Sea drainage corridor. Mar Geol 153:275–302
Aksu AE, Hiscott RN, Yaşar D, Işler FI, Marsh S (2002) Seismic stratigraphy of Late Quaternary deposits from the southwestern Black Sea shelf: evidence for non-catastrophic variations in sea-level during the last 10,000 years. Mar Geol 190(1/2):61–94
Akten N (2004) Analysis of shipping casualties in the Bosphorus. J Navig 57:1–12
Alavi SN, Okyar M, Timur K (1989) Late Quaternary sedimentation in the Strait of Bosphorus: high resolution seismic profiling. Mar Geol 89:185–205
Algan O, Çağatay N, Tchepalyga A, Ongan D, Eastoe C, Gökaşan E (2001) Stratigraphy of the sediment infill in Bosphorus Strait: water exchange between the Black and Mediterranean Seas during the last glacial Holocene. Geo-Mar Lett 20(4):209–218
Algan O, Gökaşan E, Gazioğlu C, Yücel ZY, Alpar B, Güneysu C, Kırcı E, Demirel S, Sarı E, Ongan D (2002) A high-resolution seismic study in Sakarya Delta and submarine canyon, southern Black Sea shelf. Cont Shelf Res 22(10):1511–1527
Andrussow N (1900) Bosphorus und Dardanellen. Annu Gèol Minéral Russie 4:3–10
Çağatay MN, Görür N, Algan O, Eastoe C, Tchapalyga A, Ongan D, Kuhn T, Kuşçu İ (2000) Last glacial-Holocene paleoceanography of the Sea of Marmara: timing of the last connections with the Mediterranean and the Black Sea. Mar Geol 167:191–206
Cvijic J (1908) Grundlinien der Geographie und Geologie von Mazedonien und Altserbien. Gotha, Petermans Mitteil Erganzungsh I(162)
Darkot B (1938) Origin of the Turkish Straits (in Turkish). Geographical Research, Istanbul University, Lett Fak Geogr Inst Bull 4:1–14
Demirbağ E, Gökaşan E, Oktay FY, Şimşek M, Yüce H (1999) The last sea level changes in the Black Sea: evidence from the seismic data. Mar Geol 157:249–265
Di Iorio D, Yüce H (1999) Observations of Mediterranean flow into the Black Sea. J Geophys Res 104(C2):3091–3108
Ergin M, Bodur MN, Ediger V (1991) Distribution of surfical shelf sediiments in the northeastern and southwestern of the Sea of Marmara: strait and canyon regimes of the Dardanelles and Bosporus. Mar Geol 96:313–340
Erinç S (2000) In: Ertek A, Güneysu C (eds) Geomorphology I (in Turkish), 5th edn. Der Press, İstanbul
Eroskay O, Kale S (1986) Geotechnical results along the submarine passing line of the Strait of İstanbul (in Turkish). Eng Geol Bull 8:2–7
Gökaşan E (1998) The investinigation of the Quaternary evolution of the Bosporus by the seismic stratigraphic interpretation (in Turkish). PhD Thesis, Institute of Marine Science and Management, Istanbul University
Gökaşan E, Demirbağ E, Oktay FY, Ecevitoğlu B, Doğan E, Fettahoğlu MK, Şimşek M (1995) Discussion on the formation of the Strait of İstanbul using shallow seismic data (in Turkish). Geophysics 9(1/2):280–284
Gökaşan E, Demirbağ E, Oktay FY, Ecevitoğlu B, Şimşek M, Yüce H (1997) On the origin of the Bosphorous. Mar Geol 140:183–197
Gökaşan E, Gazioğlu C, Alpar B, Yüce ZY, Ersoy Ş, Gündoğdu O, Yaltırak C, Tok B (2002) Evidence of NW extension of the North Anatolian Fault Zone in the Marmara Sea; a new interpretation of the Marmara Sea (İzmit) earthquake on 17 August 1999. Geo-Mar Lett 21:183–199
Gökaşan E, Ustaömer T, Gazioğlu C, Yücel ZY, Öztürk K, Tur H, Ecevitoğlu B, Tok B (2003) Morpho-tectonic evolution of the Marmara Sea inferred from multi-beam bathymetric and seismic data. Geo-Mar Lett 23(1):19–33
Gunnerson CG, Özturgut E (1974) The Bosporus. In: Degens ET, Ross DA (eds) The Black Sea—geology, chemistry and biology. AAPG Bull 20:99–114
Hiscott RN, Aksu AE, Yaşar D, Kaminski MA, Mudie PJ, Kostylev VE, MacDonald JC, Işler FI, Lord AR (2002) Deltas south of the Bosphorus Strait record persistent Black Sea outflow to the Marmara Sea since 10 ka. Mar Geol 190(1/2):95–118
Hochstätter F (1870) Die Geologischen Verhältnisse des Östlichen Teils der Europäischen Türkei. Jahrb Kk Geol Reichsanstalt 20(1):365–461
von Hoff KEA (1822) Geschichte der durch Überlieferung nachgewiesenen natürlichen Veränderungen der Erdoberfläche,vol 8. Perthes, Gotha, pp 105–144
Kerey E, Meriç E, Tunoğlu C, Kelling G, Brenner RL, Doğan AU (2004) Black Sea-Marmara Sea Quaternary connections: new data from the Bosphorus, İstanbul, Turkey. Paleo 204:277–295
Meriç E, Oktay FY, Sakınç M, Gülen D, İnal A (1991a) Sedimentary geology and palaeoecology of the Quaternary sequences of Ayamama (Bakırköy-İstanbul) (in Turkish). Çukurova Univ Eng Fac Earthsci Bull 8(1):93–100
Meriç E, Oktay FY, Sakınç M, Gülen D, Ediger VS, Meriç N, Özdoğan M (1991b) Sedimentary geology and palaeoecology of the Quaternary sequences of Kuşdili (Kadıköy-İstanbul) (in Turkish). Çukurova Univ Eng Fac Earthsci Bull 8(1):3–91
Meriç E, Kerey İE, Avşar N, Tunoğlu C, Taner G, Kapan-Yeşilyurt S, Ünsal İ, Rosso A (2000) New results about the Mediterranean-Black Sea connection during the Late Quaternary (Holocene) (in Turkish). Turk Geol Bull 43(1):73–118
Oktay FY, Sakınç M (1991) The Late Quaternary tectonics of the Istanbul graben and the origin of the Bosphorus. EUG 6 Strasb Terra Abstr 3(1):351
Oktay FY, Gökaşan E, Sakınç M, Yaltırak C, İmren C, Demirbağ E (2002) The effect of North Anatolian Fault Zone to the latest connection between Black Sea and Sea of Marmara. Mar Geol 190(1/2):367–382
Oğuz T, Özsoy E, Latif MA, Sur Hİ, Ünlüata Ü (1990) Modelling of hydraulically controlled exchange flow in the Bosphorus Strait. J Phys Oceanogr 20(7):945–965
Özsoy E, Latif MA, Sur Hİ, Goryachkin Y (1996) A review of the exchange flow regimes and mixing in the Bosphorus Straits. In: Briand F (ed) Dynamics of the Mediterranean Straits, spec, vol 17. Bulletin de l’Institut Océanographique, Monaco, CIESM Science Séries No. 1, pp187–204
Pamir HN (1938) On the problem about the formation of the Strait of İstanbul (in Turkish). MTA Bull 3/4:61–69
Penck W (1919) Grundzüge der geologie des bosporus. Veröffentl Inst Meereskund Berl NF Reihe A 4:72
Perinçek D (1991) Possible strand of the North Anatolian Fault Zone in the Thrace Basin, Turkey—an interpretation. AAPG Bull 75:241–257
Phillipson A (1898) Bosporus und Hellespont. Geogr Zeitschr 4:16–26
Ross DA, Uchupi E, Prada KE, McIlvaine JC (1974) Bathymetry and microtopography of Black Sea. In: Degens ET, Ross DA (eds) The Black Sea—geology, chemistry and biology. AAPG Bull 20:99–114
Ryan BFW, Pitman WC III, Major CO, Shimkus K, Moskalenko V, Jones GA, Dimitrov P, Görür N, Sakınç M, Yüce H (1997) An abrupt drowning of the Black Sea shelf. Mar Geol 138:119–126
Sholten R (1974) Role of the Bosporus in Black Sea chemistry and sedimentation. In: Degens ET, Ross DA (eds) The Black Sea—geology, chemistry and biology. AAPG Bull 20:115–127
Smith AD, Taymaz T, Oktay Y, Yüce H, Alpar B, Başaran H, Jackson JA, Kara S, Şimşek M (1995) High-resolution seismic profilling in the Sea of Marmara (northwest Turkey): Late Quaternary sedimentation and sea level changes. Geol Soc Am Bull 107:923–936
Sur Hİ, Doğan E, Güven KC, Sarıkaya HZ, Okuş E, Öztürk İ, Eroğlu V (2000) Monitoring of the marine outfall system of the City of İstanbul. In: Avanzini C (ed) Proceedings of the conference on marine waste water discharge 2000. University of Genova, Italy, pp 295–305
Uluğ A, Özel E, Çiftçi G (1987) Seismic studies in the Strait of İstanbul (in Turkish). Geophysics 1(2):130–144
Yalçınlar İ (1947) About valleys around the Strait of İstanbul (in Turkish). Istanbul University Press, Fac Lett Hist Geogr Bull VI(1):69–72
Yıldırım M, Özaydın K, Erguvanlı A (1992) Geological structures and geotechnical features of the southern part of the Strait of İstanbul and Golden Horn (in Turkish). Geol Eng 40:5–14
Yılmaz Y (2005) Morphotectonic evolution of the southern Black Sea region and the Bosphorus channel. In: Yanko-Hombach V (ed) The Black Sea flood question: changes in the coastline, climate, and human settlement. NATO Science Series IV, Earth and Environmental Sciences (in press)
Yılmaz Y, Sakınç M (1990) Approach about the geological evolution of the Strait of İstanbul (in Turkish). In: Meriç E (ed) Late Quaternary (Holocene) deposits of the southern part of the Strait of İstanbul and Golden Horn. ITü Foundation Publications, Istanbul, pp 99–105
Acknowledgements
This study was supported by the Research Foundation of Istanbul University (grants 1766/21122001). We thank the TN-DNHO, and the crew of the R/V T.C.G. Çubuklu for their enthusiasm and help during seismic and bathymetric data collection. We are also grateful to T. Ustaömer, F.Y. Oktay, O. Algan, and H.İ. Sur for their valuable contributions. Constructive comments by W.B. Ryan, G. Kelling and the editor of the journal B.W. Flemming were very helpful for the improvement of the paper.
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Gökaşan, E., Tur, H., Ecevitoğlu, B. et al. Evidence and implications of massive erosion along the Strait of İstanbul (Bosphorus). Geo-Mar Lett 25, 324–342 (2005). https://doi.org/10.1007/s00367-005-0216-3
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DOI: https://doi.org/10.1007/s00367-005-0216-3