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The Response of Foraminifera and Ostracods Assemblages to the Sediment Properties of Southern Caspian Sea Shorelines

The Response of Foraminifera and Ostracods Assemblages to the Sediment Properties of Southern Caspian Sea Shorelines

Masoomeh Sohrabi Mollayousefi1* and Babak Moghaddasi2

1Department of Geology, Islamshahr Branch, Islamic Azad University, Islamshahr, Iran
2Department of Agriculture and Natural Resources, Savadkooh Branch, Islamic Azad University, Savadkooh, Iran

*      Corresponding author: sohrabi705@gmail.com

Fig. 1.

The percent value of total organic materials weight in different stations. F, G, H, I are stand for Chaboksar, Rudsar, Kalachai, Zibakenar and Gisum respectively. Subdivisions stands for different depths of 5, 10, 15 and 20 m from sea level

Fig. 2.

Mean concentration of lead, cupper and cadmium along the Gilan costline. Subdivisions stands for different depths in each station (the acronyms are as in Fig. 1).

Pakistan Journal of Zoology

October

Vol. 53, Iss. 5, Pages 1603-2000

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