Physical Oceanography

, Volume 6, Issue 4, pp 273–281 | Cite as

Some peculiarities of the Black Sea palaeohydrology in various geological periods

  • V. N. Eremeev
  • S. G. Bogullavsky
  • V. A. Zhorov
Experimental and field research

Abstract

Deep drilling data, palaeobiological indicators, evidence on the sea-level, and mathematical modelling have been used to reconstruct the Black Sea palaeohydrological regime during the Karangat transgression, the new Euxinic regression, and Holocene. The mechanism responsible for salting of the sea and the accompanying processes during the inter-glacial period are studied.

Keywords

Climate Change Mathematical Modelling Drilling Holocene Environmental Physic 

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  1. 1.
    Klige, R.K. Ocean level variations in the earth's history. In:Fluctuations of the Level of Seas and Oceans over 15 000 Years. Moscow: Nauka (1982), pp. 11–12.Google Scholar
  2. 2.
    Neprochnov, Yu.P. (Ed.).Geological History of the Black Sea from Deep-Water Drilling Data. Moscow: Nauka (1980).Google Scholar
  3. 3.
    Neprochnov, Yu.P. R/VGlomar Challenger in the Black Sea.Zemlya Vselennaya (1976), No. 2, 87–90.Google Scholar
  4. 4.
    Serebryanny, L.R. Radiocarbon clock measures the pulse of the glaciation period.Zemlya Vselennaya (1976), No. 2, 45–51.Google Scholar
  5. 5.
    Arkhangelsky, A.D. and Strakhov, N.M.Geological Structure and Evolution of the Black Sea. Moscow: Acad. Sci. USSR (1938).Google Scholar
  6. 6.
    Ostrovsky, A.B. Palaeogeographic criteria for the latest changes in the palaeohydrological regime of enclosed seas. InFluctuations of the Level of Seas and Oceans over 15 000 Years. Moscow: Nauka (1982), pp. 102–112.Google Scholar
  7. 7.
    Örsoy, E., Latif, M.A., Tugrul, S. and Ünlüata, U. Water and nutrient fluxes through the Bosphorus, Mediterranean, and Black Sea. In:Problems of the Black Sea. Sevastopol: MHI (1992), pp. 54–67.Google Scholar
  8. 8.
    Shishkina, O.V. On the possible use of data on chlorine distribution in silt waters for palaeohydrochemical reconstructions.Okeanologia (1974)15, 1053–1058.Google Scholar
  9. 9.
    Emel'yanov, E.M. On the application of the stagnation degree of hydrogen sulphide contamination coefficient for palaeogeographic reconstractions.Okeanologia (1978)18, 508–511.Google Scholar
  10. 10.
    Shishkina, O.V.Geochemistry of Marine and Oceanic Silt Waters. Moscow: Nauka (1972).Google Scholar
  11. 11.
    Shcherbakov, F.A. Reflection of sea-level variations in the sections of late quaternary marine sediments. In:Fluctuations of the Level of Seas and Oceans over 15 000 Years. Moscow: Nauka (1982), pp. 112–120.Google Scholar
  12. 12.
    Fyodorov, P.V. Post-glacial transgression of the Black Sea and the problem of ocean level variation over the last 15 000 years. In:Fluctuations of the Level of Seas and Oceans over 15 000 Years. Moscow: Nauka (1982), pp. 151–156.Google Scholar
  13. 13.
    Boguslvsky, S.G. and Kotovshchikov, B.B. Formation of the contemporary salinity field in the Black Sea.Okeanologia (1984),14, 110–116.Google Scholar

Copyright information

© VSP 1995

Authors and Affiliations

  • V. N. Eremeev
  • S. G. Bogullavsky
  • V. A. Zhorov

There are no affiliations available

Personalised recommendations