geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3494Research ArticleСтатьиArticleИстория развития побережий Каспийского моря в плейстоценеHistory of Caspian Sea coasts development in PleistoceneСвиточА. А.SvitotchA. A.ЯнинаТ. А.YaninaT. A.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия199819122023031627Copyright © Свиточ А.А., Янина Т.А., 20232023Свиточ А.А., Янина Т.А.Svitotch A.A., Yanina T.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/3494

Oscillations of Caspian Sea level, neotectonic structure and climatic changes were the main factors of coasts' formation. Phased development took place in Pleistocene in accordance with major stages of transgressions and regressions: Prebakynian (Tyurkyanian), Bakinian, Urundgiksko-Singilian. Early-Khazarian, Chernoyarsko-Late-Khazarian, Atelian, Khvalynian, and Late-Khvalynian (New-Caspian). Most of the stages have complex structure: some minor transgressive maxima, which coincide with warm climatic epochs may be marked in every regressive stage.

Oscillations of Caspian Sea level, neotectonic structure and climatic changes were the main factors of coasts' formation. Phased development took place in Pleistocene in accordance with major stages of transgressions and regressions: Prebakynian (Tyurkyanian), Bakinian, Urundgiksko-Singilian. Early-Khazarian, Chernoyarsko-Late-Khazarian, Atelian, Khvalynian, and Late-Khvalynian (New-Caspian). Most of the stages have complex structure: some minor transgressive maxima, which coincide with warm climatic epochs may be marked in every regressive stage.

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The authors declare that there are no conflicts of interest present.