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On the age of the Mangyshlakian deposits of the northern Caspian Sea

Published online by Cambridge University Press:  20 January 2017

Yuri P. Bezrodnykh
Affiliation:
Moringeologia Company, Riga, Latvia
Valentin M. Sorokin*
Affiliation:
Lomonosov Moscow State University, Moscow, Russia
*
Corresponding author. Fax: +495 9395000. E-mail address:sorokin@geol.msu.ru (V.M. Sorokin).

Abstract

The distribution, sedimentology, and age of early Holocene Mangyshlakian deposits beneath the northern Caspian Sea are studied. Analyses and interpretations derive from high-resolution sub-bottom profiling, lithological analysis of core sections and boreholes, biostratigraphic analysis of mollusc shells, and radiocarbon dating. We show that the Mangyshlakian deposits overlie Upper Pleistocene Khvalynian deposits, filling valleys and depressions that formed during lower water levels, similar to present lacustrine water bodies (ilmeni) of the Volga Delta. Transgressive marine Holocene Neo-Caspian sediments that are filling facies overlie the Mangyshlakian deposits. The deposits are composed of both organogenous and terrigenous materials. The flora and fauna in the sediment indicate deposition into freshwater, differing from marine biota in the underlying and overlying sediments. Eighteen radiocarbon ages indicate that the Mangyshlakian deposits accumulated between 9 and 12 ka.

Type
Original Articles
Copyright
University of Washington

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References

Aksu, A.E., Hiscott, R.N., Kaminski, M.A., Mudia, P.J., Gillespie, H., Adrajano, T., and Yaṣar, D. (2002). Last glacial–Holocene paleoceanography of the Black Sea and Marmara Sea: stable isotopic, foraminiferal and coccolith evidence. Marine Geology 190, 1-2 119149.Google Scholar
Arkhangelsky, A.D., and Strakhov, N.M. (1938). Geological structure and history of development of the Black Sea. Nauka Press, Moscow.(in Russian)Google Scholar
Arslanov, Kh.A. (1993). Late Pleistocene Geochronology of European Russia. Radiocarbon 35, 421427.Google Scholar
Arslanov, Kh.A., Lokshin, N.V., and Mamedov, A.V. (1988). On the age of Khazarian, Khvalynian, and New Caspian deposits of the Caspian Sea. Bulletin of the Quaternary Commission 57, 4558.(in Russian)Google Scholar
Badyukova, E.N. (2007). Age of Khvalynian Transgressions in the Caspian Sea Region. Oceanology 47, 400405.Google Scholar
Bahr, A., Lami, F., Arz, H., Kuhlmann, H., and Wefer, G. (2005). Late Glacial to Holocene climate and sedimentation history in the NW Black Sea. Marine Geology 214, 309322.Google Scholar
Balabanov, I.P. (2009). Paleogeographical background to formation of modern natural conditions of the Caucasus littoral Holocene terraces and their long-term development forecast. Dalnauka Press, Moscow-Vladivostok.(in Russian)Google Scholar
Bezrodnykh, Yu.P., Romanyuk, B.F., Deliya, S.V., Magomedov, R.D., Sorokin, V.M., Parunin, O.B., and Babak, E.V. (2004). Biostratigraphy and structure of the Upper Quaternary deposits and some paleogeographic features of the north Caspian region.Stratigraphy. Geological Correlation 12, Pleiades Publishing, Ltd, 102120.Google Scholar
Bolikhovskaya, N.S. (2011). Features of environmental and climatic changes in the Northern Caspian sea region and Caspian Sea level fluctuations controlled by climate during the Holocene.Proceeding of the VII All-Russian Quaternary Conference. The Quaternary in all of its variety. Basic issues, results, and major trends of further research. Apatity. Saint-Peterburg. V.1.7477.(in Russian)Google Scholar
Chepalyga, A.L. (2007). The Late Glacial great flood in the Ponto-Caspian basin.Yanro-Hombach, V., Gilbert, A.S., Panin, N., Dolukhanov, P.M. The Black sea flood Question: Changes in Coastline, Climate, and Human Settlement Springer, 119148.Google Scholar
Chernyshova, M.B., and Sorokin, V.M. (1984). Comparison of palynological characteristics of Late Quaternary sediments from the Mediterranean and Black Seas, IzvestiyaVysshihUchebnih. Zavedeniy. Geologiyai Razvedka 2, 118120.(in Russian)Google Scholar
Fedorov, P.V. (1978). Pleistocene of the Ponto Caspian. Nauka Press, Moscow.(in Russian)Google Scholar
Fedorov, P.V. (1995). Modern geology of the Caspian Sea. Herald of the Academy of Sciences. 65, 7 622625.(in Russian)Google Scholar
Khain, V.E. (1958). On the problem of the tectonics of Caspian depression and structural bounds between Caucasus and Trans Caspian region. Oil and Gas Geology 9, 1118.(in Russian)Google Scholar
Komarov, A.V., Bozhilova, E.D., Filipova, M.V., and Udintseva, O.G. (1978). Palynological spectra and their stratigraphic interpretation.Geology and Hydrology of the Western Black Sea. Sofia: Bulgar. Acad. Sci. 8591.(in Russian)Google Scholar
Kuprin, P.N., Sorokin, V.M., Babak, E.V., and Chernyshova, M.B. (1984). Correlation of Quaternary sections in the western part of the Black Sea.The Study of the Geological History and Recent Sedimentation in the Black and Baltic Seas. Kiev, Naukova dumka.116122.(in Russian)Google Scholar
Kuzmin, Y.V., Nevesskaya, L.A., Krivonogov, S.K., and Burr, G.S. (2007). Apparent 14C ages of the ‘pre-bomb’ shells and correction values (R, ΔR) for Caspian and Aral seas (Central Asia). Nuclear Instruments and Methods in Physics Research B 259, 463466.Google Scholar
Kvasov, D.D. (1975). Late Quaternary history of large lakes and inland seas of Eastern Europe. Nauka Press, Leningrad.(in Russian)Google Scholar
Lebedev, L.I., Bordovskiy, O.K., and Maev, E.G. (1973). Sediments of the Caspian Sea. Science Press, Moscow.(in Russian)Google Scholar
Leonov, Yu.G., Lavrushin, Yu.A., Antipov, M.N., Spiridonova, E.A., Kuzmin, Ya.V., Jail, E., Burr, S., Jelinovsky, A., and Shali, F. (2002). New data on the age transgressive phase Early Khvalynskaya transgression of the Caspian Sea. DokladyAkademii Nauk 386, 229233.(in Russian)Google Scholar
Leontyev, O.K. (1961). The ancient shorelines of Quaternary transgressions of the Caspian Sea.Trudy InstitutaGeografii. Akademii. Nauk SSSR.8, 4564.(in Russian)Google Scholar
Leroy, S.A.G., Tudryn, A., Chalié, F., López-Merino, L., and Gasse, F. (2013). From the Allerød to the mid-Holocene: palynological evidence from the south basin of the Caspian Sea. Quaternary Science Reviews 78, 7797.Google Scholar
Maev, E.G. (2006). Extreme regression of the Caspian Sea during early Holocene.Proceedings of the international science conference. Extreme and hydrogeological events in Aral-Caspian seas, Moscow.6266.(in Russian)Google Scholar
Maev, E.G. (2009). Phases of mangishlak regression in the Caspian Sea. VestnikMoskovskogouniversiteta. Seria Geografia 1, 1520.(in Russian)Google Scholar
Major, C., Ryan, W., Lericolais, G., and Hajdas, I. (2002). Constraints on Black Sea outflow to the Sea of Marmara during the last glacial interglacial transition. Marine Geology 190, 1934.Google Scholar
Major, C.O., Goldstein, S.L., Ryan, W.B.F., Lericolais, G., Piotrovski, A.M., and Haidas, I. (2006). The co-evolution of Black Sea level and composition through the last deglaciation and its paleoclimatic significance. Quaternary Science Reviews 25, 20312047.Google Scholar
Popov, G.I. (1983). Pleistocene of the Black Sea–Caspian Seaways. Nauka Press, Moscow.(in Russian)Google Scholar
Ross, D.A., and Degens, E.T. (1974). Recent Sediments of Black Sea.Ross, D.A., Degens, E.T. The Black Sea, Geology, Chemistry and Biology. Tulsa, Oklahoma Am. Assoc. Petrol. Geol Google Scholar
Ross, D.A., Neprochnov, Y.P., Hsű, K.J., Stoffers, P., Supko, P., Trimonis, E.S., Percival, S.F., Erickson, A.J., Degens, E.T., Hunt, J.M. Initial Report of the Deep Sea Drilling Project 42, pt. 2. U.S. Government Printing Office, Washington.Google Scholar
Ryan, W.B.F., Pitman, W.C. III, Major, C.O., Shimkus, K., Moskalenko, V., Jones, G.A., Dimitrov, P., Görür, N., Sakinç, M., and Yüce, H. (1997). An abrupt drowning of the Black Sea shelf. Marine Geology 138, 119126.Google Scholar
Ryan, W.B.F., Panin, N., and Dolukhanov, P.M. (2007). Status of the Black sea flood hypothesis.Yanro-Hombach, V., Gilbert, A.S. The Black sea flood Question: Changes in Coastline, Climate, and Human Settlement Springer, 6388.Google Scholar
Rychagov, G.I. (1997). Pleistocene History of the Caspian Sea. Moscow State University Press, Moscow.(in Russian)Google Scholar
Schrøder, N., Højlund Pedersen, L., and Juel Bitsch, R. (2004). 10,000 Years of climate change and human impact on the environment in the area surrounding Lejre. The Journal of Transdisciplinary Environmental Studies 3, 1 127.Google Scholar
Shimkus, K.M., Emel’yanov, E.S., and Trimonis, E.M. (1975). Black Sea bottom sediments and features of the Late Quaternary History.The Earth’s Crust and Evolution of the Black Sea Depression. Nauka Press, Moscow.138161.(in Russian)Google Scholar
Sorokin, V.M., and Chernyshova, M.B. (1983). Late Quaternary climatic fluctuations by data of sediment studies in the Caspian Sea. IzvestiyaVysshihUchebnih. Zavedeniy. Geologiyai Razvedka 6, 2429.(in Russian)Google Scholar
Sorokin, V.M., and Kuprin, P.N. (2007). On the character of Black Sea level rise during the Holocene.Moscow University Geology Bulletin.62, © Allerton Press, Inc., 334341.Google Scholar
Sorokin, V.M., Kuprin, P.N., and Chernyshova, M.B. (1983). Late Quaternary comparative paleogeography of the Black and Caspian Seas.Paleogeography of the Caspian and Aral Seas in the Cenozoic. MoskovskiGosudarstvenniy Universitet, Moscow.4252.(in Russian)Google Scholar
Sorokin, V.M., Sokolov, V.N., and Shlykov, V.G. (1987). Genetic types of carbonates from the Late Quaternary sediments of the Black sea. Litologiya I poleznie iskopaemie 1, 2430.(in Russian)Google Scholar
Stuiver, M., Reimer, P.J., and Reimer, R. (2014). Calib radiocarbon calibration.html. www.calib.qub.ac.uk/calib/(Execute version 7.0)Google Scholar
Svitoch, A.A., and Yanina, T.A. (1997). Quaternary sediments of the Caspian Sea coasts. RASHN Press, Moscow.(in Russian)Google Scholar
Svitoch, A.A., Selivanov, A.O., and Yanina, T.A. (1998). Pleistocene paleogeographic events in the Ponto-Caspian and Mediterranean regions. MoskovskiyGosudarstvenniy Universitet, Moscow.(in Russian)Google Scholar
Varushchenko, S.I., Varushchenko, A.I., and Klige, R.K. (1987). The change of the regime of the Caspian Sea and closed water basins during Paleotimem, Moscow. Nauka Press, Moscow.(in Russian)Google Scholar
Vronskii, V.A. (2006). Ecological and geographical problems of the Caspian Sea. GeografiyaiPrirodnie Resursi 1, 3135.Google Scholar
Yanina, T.A. (2012). Correlation of the Late Pleistocene paleogeographical events of the Caspian Sea and Russian Plain. Quaternary International 271, 120129.Google Scholar
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