ОСОБЕННОСТИ РАЗВИТИЯ ЧЕРНОМОРСКОГО ПОБЕРЕЖЬЯ ТАМАНСКОГО ПОЛУОСТРОВА В ПОЗДНЕМ ГОЛОЦЕНЕ

Abstract

The paper deals with the results of paleogeographical study of marine and deltaic sediments of the Black Sea’s shoreline of Taman’ peninsular, aimed to reconstruction of the local variation of the sea level changes and coast development in the Late Holocene. On the basis of litho-facial, palaeontological, geochronological and submarine archaeological studies an estimation of local neotectonic impact on the sea level changes for the last 5.0 ka was obtained and the time frame of recent coastal feature’s generation was determined.