Sedimentary and environmental characteristics of the Gilan-Mazenderan plain, northern Iran: influence of long- and short-term Caspian water level fluctuations on geomorphology

Creative Commons License

Kazanci N., Gulbabazadeh T., Leroy S., Ileri O.

JOURNAL OF MARINE SYSTEMS, cilt.46, sa.1-4, ss.145-168, 2004 (SCI-Expanded, Scopus)

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 46 Sayı: 1-4
  • Basım Tarihi: 2004
  • Doi Numarası: 10.1016/j.jmarsys.2003.12.002
  • Dergi Adı: JOURNAL OF MARINE SYSTEMS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.145-168
  • Anahtar Kelimeler: Holocene, late Pleistocene, sea level fluctuation, coastal lowland, Lake Anzali, Talesh Mountains, northern Iran, Caspian Sea, SEA-LEVEL, SUBSIDENCE, TECTONICS, EVOLUTION, LOESS
  • Açık Arşiv Koleksiyonu: AVESİS Açık Erişim Koleksiyonu
  • Ankara Üniversitesi Adresli: Hayır

Özet

The south-southwestern Caspian coastal lowland in Iran, or the Gilan-Mazenderan plain, is a relatively narrow but long, composite depositional area of late Quaternary age. The Sefid Rud delta, the Anzali Lake (connected to the Caspian Sea by a meandering outlet 3.5 km long) and storm-dominated beaches are its prominent sedimentary features. They are controlled by the present water level of the Caspian Sea at -26.36 m in 2000. The late Pleistocene-Holocene deposits of the lowland, which are covered commonly by a modern loess-origin soil, mainly consist of alternations of marine and non-marine sediments. The marine units form coastal terraces at 19-20 m (I), 2-0 m (II) and -6- -8 m (III) corresponding to the Late Khvalinian and Neocaspian transgressions. The deposits of the youngest terrace (terrace III) that represents a prograding beach-ridge complex are a consequence of several medium-term, cyclic water level oscillations in late Holocene. Just after the initiation of the beach-ridge complex, Lake Anzali that formed by damming of rivers and then by progradation of the complex in time forced to form the outlet of the lake. The nearest medium-term cycle lasted c. 65 years between 1930 and 1995, and the records showed that it included a lot of short-term (c. 4-5 years) and very short-term (week to months) water level oscillations. During the last erratic rise of sea level (1977-1996), the area of Lake Anzali doubled; the delta and the coastal sands including modern beaches were eroded on a width of around 30-100 m. Overall, a steplike morphology, through the repetition of marine and non-marine facies and also water level records of the last 75 years, indicate that the ancient and recent deposition on the coastal lowland has been controlled by long-, medium- and short-term fluctuations of the Caspian Sea level. (C) 2004 Elsevier B.V. All rights reserved.