Д.П. Димитров. ПАЛЕОГЕОГРАФИЧЕСКИЕ РЕКОНСТРУКЦИИ И УСЛОВИЯ ФОРМИРОВАНИЯ НЕТРАДИЦИОННЫХ РЕСУРСОВ ЧЕРНОГО МОРЯ

Д.П. Димитров 
Институт океанологии, Болгарская академия наук, Варна, Болгария
ПАЛЕОГЕОГРАФИЧЕСКИЕ РЕКОНСТРУКЦИИ И УСЛОВИЯ ФОРМИРОВАНИЯ НЕТРАДИЦИОННЫХ РЕСУРСОВ ЧЕРНОГО МОРЯ 
Современные Средиземное, Черное и Каспийское моря неоднократно подвергались геокатастрофическим событиям, вызванным резкими изменениями климата или глобальными геологическими процессами. Ярким примером этого служит мессинский кризис в Средиземном море на границе миоцен — плиоцен (5,7—5,2 млн лет тому назад), когда сформировалась эвапоритово-сероносная формация. В это же время формируется Азово-Черноморская железорудная провинция и балханская свита Каспийского моря, с которой связаны крупные месторождения нефти и газа. Черноморский кризис около 8—9 тыс. лет тому назад связан с геокатастрофическим событием в результате таяния ледников вюрмского оледенения: воды Средиземного моря соленостью 38 ‰ хлынули в Черноморский пресноводный бассейн, что привело к формированию гигантских скоплений органо-минеральных осадков (сапропелей). 
Ключевые слова: ранний плейстоцен, нижний, средний, верхний плейстоцен, голоцен, мессиний, занклий, галесий, биостратиграфия. 
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