RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 18, ES6003, doi:10.2205/2018ES000639, 2018


Figure 1. Research area, hydrophysical and hydrochemical characteristics of the Caspian Sea: a) – map-scheme of the research area and the location of the sampling Station 3916; b) – CTD-profiles of distribution of temperature ($T$), salinity ($S$), conventional density ($\delta_t$), and oxygen (O$_2$) in the water column of Station 3916 [Ivanov et al., 2013]; c) – evolution of the level of the Caspian Sea in the 20th century in relation to the level of the World Ocean [Lebedev, 2005].


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Citation: Kozina N., L. Reykhard, O. Dara, V. Gordeev (2018), Framboidal pyrite formation in the bottom sediments of the South Caspian Basin under conditions of hydrogen sulfide contamination, Russ. J. Earth Sci., 18, ES6003, doi:10.2205/2018ES000639.


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