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Като се сдобиеш с долуспоменатите статии, виж в библиографиите им има още статии, които ще те заинтересуват. Приложил съм и цитат от статия, в която и г-н Раян е съавтор, тъй като има "известна" промяна във възгледите му през годините
А за колко се пълят през отвореният Босфор около 100-120-130 метра всеки с известни познания може да провери и сам. Имаш ширина на Босфора действай- смятай и ще провериш- 300 до 400 дни.
Аз пръв те попитах ... става въпрос са доста кубически метри ...
AKSU A. E., P. J. MUDIE, A. ROCHON, M. A. KAMINSKI, T. ABRAJANO, D. YASAR 2002. Persistent Holocene Outflow from the black Sea to the Eastern Mediterranean contradicts Noah’s Flood Hypothesis.Continents, 12(5): 4-10.
HISCOTT, R. N., A.E. AKSU. 2002. Late Quaternary history of the Marmara Sea and Black Sea from high resolution seismic and gravity core studies. - Marine Geology, 190(1/2): 261-282.
MAJOR C., W. RYAN, G. LERICOLAIS, I. HAJDAS. 2002. Constraints on Black Sea outflow to the Sea of Marmara during the last glacial–interglacial transition. - Marine Geology, 190(1/2): 19-34.
MAJOR C., S. GOLDSTEIN, W. RYAN, G. LERICOLAIS, A. PIOTROWSKI, I. HAJDAS. 2006. The co-evolution of Black Sea level and composition through the last deglaciation and its paleoclimatic significance. - Quaternary Science Reviews, 25(17/18): 2031-2047
“A final shift to marine values in Sr and oxygen isotope ratios at 9.4 ka BP cal corresponds to connection with the global ocean, and marks the onset of sedimentation on the Black Sea continental shelf. This date for the marine incursion is earlier than previously suggested based on the appearance of euryhaline fauna and the onset of sapropel formation in the deep basin.”
“Geochemical data show that the marine influence on Black Sea water chemistry began ~9,400 y BP cal and triggered changes in mollusk assemblages and the first faunal colonization atop a shelf-wide unconformity. The concurrence of the abrupt increases in 87Sr/86Sr and 18O to marine compositions in mollusks sampled from a thin shell gravel horizon atop the unconformity suggests that the incursion of Mediterranean water may have been the causative agent for the drowning of the lake margin. The date of 7.5 ka BP cal reported by Ryan et al. (1997) is not the incursion itself, but time when salinity rose to a sufficient threshold for a introduction of euryhaline taxa following the first brackish species.”
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Re: Черноморският регион 6500-5500г пр.Хр. [re: т-pekc]
