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Palaeogeography, Palaeoclimatology, Palaeoecology, 1983, Vol 43, Issue 0, p. 195-204
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Palaeogeographic environment during the desiccation of the Black Sea
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Kojumdgieva Emilia,
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Abstract:
During the latest Chersonian (about 10.3 m.y. ago) tectonic movements took place leading to an elevation of the Crimean-Caucasian chain and to an isolation of the Fore-Caucasian part of the Black Sea Basin. This part of the basin had been draining the rivers of the Russian Platform and after the isolation it became desalinized, while the main part of the Black Sea Basin was almost desiccated and evaporites, mainly dolomites, formed in it due to the predominant calcium---magnesium---carbonate composition of the Chersonian Sea waters. These dolomites are found in the drillings of DSDP Leg 42B and are confirmed geophysically.The tectonic movements during the latest Chersonian led to the formation of a series of grabens along which the Mediterranean Sea invaded the north Aegean area and a little later (during the Early Maeotian) the Black Sea
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Keywords: area, basin, black sea, desiccation, dolomite, dolomites, environment, evaporite, evaporites, graben, mediterranean, mediterranean sea, mediterranean-sea, movement, north, part, platform, river, rivers, sea, sea-water, series, water, waters,
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