Conservation of the Biological Diversity as a Prerequisite by G. Agladze, L. Eliava, A. Komakhize, N. Mazmanidi, G.

By G. Agladze, L. Eliava, A. Komakhize, N. Mazmanidi, G. Nakhutsrishvili, P. Naskidashvili (auth.), V. Kotlyakov, M. Uppenbrink, V. Metreveli (eds.)

This quantity is a suite of news offered on the overseas NATO complicated learn Workshop Conservation of the organic variety as a Prerequisite for Sustainaible improvement of the Black Sea area. The seminar was once held at Batumi - Kobuleti, Georgia, at the Black Sea in the course of October five -12, 1996 with individuals from the nations of the Black Sea quarter -Georgia, Russia, the Ukraine, Turkey, Bulgaria, Romania, in addition to Germany, Italy and the U.S. of the United States. The Black Sea area is an important and specific a part of southern Europe due to its geographical, cultural and old positive aspects. it's the cradle of eu civilisation, including Greece and Rome. for hundreds of years it neighboured onto and interacted with the cultures of the northern and southern Mediterranean, the Christian and Moslim worlds, and was once the path of conquerors and migrations of entire countries. listed here are heavily interwoven the cultures and customs of countries, fiscal and exchange family members, the heritage of wars and civilised family of neighbouring countries.

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Simpheropol, Tavria, 192 pp. 10. Rukovodiashie Princhipi Issledovani po Stranam v Oblasti Biologicheckogo Raznoobrasia. Programa Organizachii Obiedinenich Naciih po Okrushaichei Srede (1994). Nairobi, 152 pp. 11. Phisicheskaia Geographia Stavropolskogo Kraia (1995). (Eds. V. V. Savelieva, V. A. Salnev). Stavropol: SKIPRO, 220 pp. 12. Beroutchachvili, N. Radvanye, J. (1996). Atlas Geopolitique Informatique du Caucase. Paris, Publication Langues'O, 78 pp. 13. Human Development Report. Armenia (1995).

4 -irretnevable consumpll on and loss. 5 -maximal and minimal estimations (afier data of Koronkevich 1982) 39 By Shiklomanov [22], the above mentioned forecasts of the anthropogenic changes of the river runoff should be considered approximate. It is a result of uncertain growth of water consumption, as well as necessary measures to mitigate unfavourable changes of the water resources, which rate is still unknown. However, these prerequisites for forecasting inflow of river water to the Black Sea are the only possible.

During that period the World Ocean level exceeded twice the present one. Thousands years BP 12 11 10 9 8 7 6 5 4 o 2 3 4 Contemporary sea level 1--------~--~------------------~L-~r+---~~------~~~--7 3 4 6 M 4 12 20 28 36 Figure 2. Black Sea level change during the Post-glacial time: 1 - New Euxin transgression; 2 - stages of the Post-glacial transgression: 2 - Old Black sea's stage, 3 - New Black sea's stage, 4 - Fanagorian stage, 5Nymphaean stage, 6 - Korsun stage (after [91, simplified). C. The Black Sea level variations of the Holocene described by Fedorov and Shherbakov, as well as other authors [11, 12] are slightly different by the occurence of the level change phases that can be described by difficulties of interpretation of Holocene deposits dating.

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