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Last-interglacial records from central Asia to the northern Black Sea shoreline: stratigraphy and correlation

Published online by Cambridge University Press:  01 April 2016

A.E. Dodonov ,
A.L. Tchepalyga ,
C.D. Mihailescu ,
L.P. Zhou ,
A.K. Markova ,
V.M. Trubikhin ,
A.N. Simakova  and
E.G. Konikov
A.E. Dodonov*
Affiliation:
Geological Institute, Russian Academy of Sciences, Pyzhevsky 7, MOSCOW 109017, Russia
A.L. Tchepalyga
Affiliation:
Institute of Geography, Russian Academy of Sciences, Staromonetnyi 29, MOSCOW 109017, Russia
C.D. Mihailescu
Affiliation:
Institute of Geography, Moldavian Academy of Sciences, Academia Street 3, KISHINEV 2028, Moldova
L.P. Zhou
Affiliation:
The Godwin Laboratory, Department of Earth Sciences, University of Cambridge, Pembroke Street, CAMBRIDGE CB2 3SA, United Kingdom
A.K. Markova
Affiliation:
Institute of Geography, Russian Academy of Sciences, Staromonetnyi 29, MOSCOW 109017, Russia
V.M. Trubikhin
Affiliation:
Geological Institute, Russian Academy of Sciences, Pyzhevsky 7, MOSCOW 109017, Russia
A.N. Simakova
Affiliation:
Geological Institute, Russian Academy of Sciences, Pyzhevsky 7, MOSCOW 109017, Russia
E.G. Konikov
Affiliation:
Geological Department, Odessa University, Shampanskiy 2, ODESSA, Ukraine
*
1Corresponding author
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Abstract

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The records of the last interglacial in several palaeogeographical zones and various sedimentary environments from Central Asia to the Black Sea shoreline are presented. The last interglacial is characterized in the study areas by a two- or three-unit stratigraphical complex with both terrestrial and marine formations. Finds of significant small mammalian remains, together with a characteristic mollusc fauna in the Karangatian marine sediments, provide key levels for biostratigraphical correlation between the marine and continental deposits. New U/Th dates allow the correlation of the Karangatian transgression with δ18O substage 5e.

Keywords

last interglacialloessmarine transgressionmollusc faunapalaeosolstratigraphy
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 79 , Issue 2-3 , August 2000 , pp. 303 - 311
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2000

References

Andrusov, N.I., 1904-1905. On the age of the marine post-tertiary terraces of the Kerch peninsula. Annual Issue [Ezhegodnik] on Geology and Mineralogy of Russia 7(6): 158–172.Google Scholar
Arkhangel’sky, A.D. & Strakhov, N.M., 1938. Geological structure and history of development of the Black Sea. The Academy of Sciences of the USSR Press (Moscow-Leningrad): 226 pp.Google Scholar
Arslanov, H.A., Gey, N.A., Izmailov, Ya.A., Lokshin, N.V. Gerasimova, S.A. & Tertychnyi, N.I., 1983. Age and climatic conditions of the late Pleistocene marine terrace formations on a coastline of the Kerch strait [in Russian]. Vestnik of Leningrad University, series of Geology and Geography 12: 69–79.Google Scholar
Arslanov, H.A., Lokshin, N.V., Mamedov, A.V., Aleskerov, B.D., Gerasimov, S.A., Tertychnyi, N.I., Tertychnaya, T.V. & Chernov, S.B., 1988. On the age of the Khazarian, Khvalynian and New Caspian deposits in the Caspian Sea [in Russian]. Bulletin of the Commission on the Quaternary Research 57: 28–38.Google Scholar
Bosch, J.H.A., Cleveringa, P. & Meijer, T., 2000. The Eemian stage in the Netherlands: history character and new research. In: Van Kolfschoten, Th. & Gibbard, P.L. (eds.):The Eemian - local sequences, global perspectives. Geologie en Mijnbouw / Netherlands Journal of Geosciences 79: 135–145 (this issue).Google Scholar
Cleveringa, P., Meijer, T., Van Leeuwen, R.J.W., De Wolf, F., Pouwer, R. Lissenberg, T. & Burger, A.W., 2000. The Eemian type locality at Amersfoort in the central Netherlands: redeployment of old and new data. In: Van Kolfschoten, Th. & Gibbard, P.L. (eds.): The Eemian - local sequences, global perspectives. Geologie en Mijnbouw / Netherlands Journal of Geosciences 79: 197–216 (this issue).Google Scholar
Dodonov, A.E., 1991. Loess of central Asia. Geojournal 24: 185–194.Google Scholar
Dodonov, A.E. & Baiguzina, L.L., 1995. Loess stratigraphy of central Asia: palaeoclimate and palaeoenvironmental aspects. Quaternary Science Reviews 14: 707–720.Google Scholar
Fedorov, P.V., 1978. The Ponto-Caspian Pleistocene [in Russian]. Transactions of the Geological Institute of the Academy of Sciences of the USSR: 166 pp.Google Scholar
Fedorov, P.V., 1988. The problem of changes of the Black Sea level during the Pleistocene [in Russian]. Bulletin of the Moscow Society of Nature Researchers (MOIP), Geology 63: 55–61.Google Scholar
Forster, T. & Heller, F., 1994. Loess deposits from the Tajik depression (Central-Asia) - magnetic properties and paleoclimate. Earth and Planetary Science Letters 128: 501–512.Google Scholar
Frechen, M. & Dodonov, A.E., 1998. Loess chronology of the middle and upper Pleistocene in Tadjikistan. Geologische Rundschau 87: 2–20.Google Scholar
Huang, J., 1984. Changes of sea-level since the late Pleistocene in China. In: The evolution of the East Asian environment 1: Geology and palaeogeography. University of Hong Kong: 309–319.Google Scholar
Kemp, R.A., Derbyshire, E., Xingmin, M., Fahu, C. & Baotian, P., 1995. Pedosedimentary reconstruction of a thick loess-palaeosol sequence near Lanhzou in North-Central China. Quaternary Research 43: 30–45.Google Scholar
Kukla, G., McManus, J.F., Rousseau, D.-D. & Chuine, I., 1997. How long and how stable was the last interglacial? Quaternary Science Reviews 16: 605–612.Google Scholar
Li, P.Y. & Zhou, L.P., 1993. Occurrence and palaeoenvironmental implications of the Late Pleistocene loess along the Eastern coasts of the Bohai Sea, China. In: Pye, K. (ed): The dynamics and environmental context of aeolian sedimentary systems. Geological Society Special Publication 42: 293–309.Google Scholar
Markova, A.K. & Mihailescu, C.D., 1990. The new locality of therio- and mollusc fauna in Mikulino deposits of Lower Danube [in Russian]. Bulletin of the Commission on the Quaternary Research 59: 94–101.Google Scholar
Mihailescu, C.D. & Markova, A.K., 1992. Palaeogeographical stages of Anthropogene fauna of the Southern Moldova [in Russian]. Shtiintsa Press (Kishinev) 310 pp.Google Scholar
Nevesskaya, L.A., 1965. Late Quaternary bevale molluscs of the Black Sea, their sistematics and ecology [in Russian]. Transactions of the Palaeontological Institute of the Academy of Sciences of the USSR 105: 391 pp.Google Scholar
Ostrovsky, A.B., Izmailov, Ya. A., Scheglov, A.P., Aslanov, A.H., Tertychnyi, N.I., Gey, N.A., Piotrowskaya, T.Yu., Muratov, V.M., Schelinskii, V.E., Balabanov, I.P. & Skiba, S.I., 1977. New stratigraphical and geochronological data on the Pleistocene marine terraces in the Black Sea shore of the Caucasus and Kerch-Taman region [in Russian]. In: Kaplin, P.A. & Scherbakov, F.A. (eds.): Pleistocene palaeogeography and sediments of southern seas in USSR. Nauka Press (Moscow): 61–68.Google Scholar
Popov, G.I., 1983. Pleistocene of the Black Sea - Caspian Sea straits (Stratigraphy, correlation, fauna, geological history) [in Russian]. Nauka Press (Moscow): 216 pp.Google Scholar
Scherbakov, F.A., Kuprin, P.N. & Morgunov, Yu.G., 1979. Late Quaternary stage of the Black Sea development [in Russian]. Bulletin of the Commission on the Quaternary Research 49: 3–16.Google Scholar
Shackleton, N.J., An, Z., Dodonov, A.E., Gavin, J., Kukla, G.J., Ranov, V.A. & Zhou, L.P., 1955. Accumulation rate of loess in Tadjikistan and China: relationship with global ice volume cycles. Quaternary Proceedings 4: 1–6.Google Scholar
Sotnikova, M.V., Dodonov, A.E. & Pen’kov, A.V., 1997. Upper Cenozoic bio-magnetic stratigraphy of central Asian mammalian localities. Palaeogeography Palaeoclimatology Palaeoecology 133: 243–258.Google Scholar
Tchepalyga, A.L., 1997. Detailed event stratigraphy of Black Sea Pleistocene [in Russian]. In: Alekseev, M.N. & Khoreva, I.M. (eds.): Quaternary geology and palaeogeography of Russia. GEOS Press (Moscow): 196–201.Google Scholar
Veklich, M.F., 1982. Palaeostages and stratotypes of Upper Cenozoic soil formations [in Russian]. Naukova dumka (Kiev): 205 pp.Google Scholar
Velichko, A.A. (ed.), 1993. Evolution of landscapes and climates of the Northern Eurasia. Late Pleistocene-Holocene; elements of prognosis. 1: Regional palaeogeography [in Russian]. Nauka (Moscow): 102 pp.Google Scholar
Velichko, A.A., Markova, A.K., Morozova, T.D., Nechaev, V.P., Svetlitskaya, T.V., Tsatskin, A.I. & Chichagov, O.A., 1992. Geochronology of loess-palaeosol formation in South-West Russian plain on new data [in Russian]. In: Geochronology of the Quaternary. Nauka (Moscow): 28–33.Google Scholar
Xiao, J., Porter, S.C, An, Z., Kumai, H. SiYoshikawa, S., 1995. Grain size of quartz as an indicator of winter monsoon strength on the Loess Plateau of Central China during the last 130,000 yr. Quaternary Research 43: 22–29.Google Scholar
Zagwijn, W.H., 1983. Sea-level changes in The Netherlands during the Eemian. Geologie en Mijnbouw 62: 437–450.Google Scholar
Zagwijn, W.H., 1989. Vegetation and climate during warmer intervals in the late Pleistocene ofWestern and Central Europe. Quaternary International 3/4: 57–67.Google Scholar
Zhou, L.P., Dodonov, A.E. & Shackleton, N.J., 1995.Thermoluminescence dating of the Orkutsay loess section in Tashkent Region, Uzbekistan, central Asia. Quaternary Science Reviews 14: 721–730.Google Scholar
Zhou, L.P., Oldfield, F., Winde, A.G., Robinson, S.G. & Wang, J.T., 1990. Partly pedogenic origin of magnetic variations in Chinese loess. Nature 346: 737–739.Google Scholar