Regressive periods of the Great Caspian
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  • 作者:A. A. Svitoch
  • 关键词:the Great Caspian ; level variations ; regression ; pliopleistocene ; paleogeography
  • 刊名:Water Resources
  • 出版年:2016
  • 出版时间:March 2016
  • 年:2016
  • 卷:43
  • 期:2
  • 页码:270-282
  • 全文大小:711 KB
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    37.Shnitnikov, A.A., Zakonomernosti kolebaniya urovnya Kaspiiskogo morya v svyazi s izmenchivost’yu uvlazhneniya materikov Severnogo polushariya (Regularities in Caspian Level Variations in the Context of Moistening of Continents of the Northern Hemisphere), Moscow: Izd. AN SSSR, 1957.
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  • 作者单位:A. A. Svitoch (1)

    1. Moscow State University, Moscow, 119991, Russia
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Hydrogeology
    Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
    Russian Library of Science
  • 出版者:MAIK Nauka/Interperiodica distributed exclusively by Springer Science+Business Media LLC.
  • ISSN:1608-344X
文摘
The Late Pliocene–Quaternary Great Caspian, in addition to the positive transgressive rhythmics shows regressions of different scales: balakhanskaya, domashkinskaya, tyurkyanskaya, venedskaya, chelekenskaya, chernoyarskaya, atel’skaya, enotaevskaya, mangyshlakskaya, and izerbashzkaya. In these periods, large-scale natural phenomena took place on the Caspian shelf, coasts, and adjacent inundated territories, including sea level drop, drying of a part of seabed, and change of landscapes and the sedimentation character. The neaped water area showed changes in water salt composition and temperature regime, along with a change in faunistic complexes. Different hierarchic state of sea level and different correlation with climate events on the surrounding territories was shown to take place during the regression with predominance of warm (interglacial) periods among them.

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