2014
DOI: 10.1134/s1995082914030109
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Zooplankton of lakes of the Uldza and Kerulen river valleys of northeastern Mongolia

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Cited by 13 publications
(8 citation statements)
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“…The water temperature varied from 19.5 to 35.2 °C. In terms of water mineralization, the studied lakes may be divided into three groups: oligohaline lakes having water mineralization of 0.7–4.2 g l −1 , mesohaline lakes with water mineralization of 5.0–16.2 g l −1 , and polyhaline lakes with mineralization over 20 g l −1 (Itigilova et al, 2014). The dominant cation was sodium, hydrocarbonate was the dominant anion, chloride was the sub-dominant anion with increasing mineralization (Sklyarov et al, 2011) (Table 1).…”
Section: Methodsmentioning
confidence: 99%
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“…The water temperature varied from 19.5 to 35.2 °C. In terms of water mineralization, the studied lakes may be divided into three groups: oligohaline lakes having water mineralization of 0.7–4.2 g l −1 , mesohaline lakes with water mineralization of 5.0–16.2 g l −1 , and polyhaline lakes with mineralization over 20 g l −1 (Itigilova et al, 2014). The dominant cation was sodium, hydrocarbonate was the dominant anion, chloride was the sub-dominant anion with increasing mineralization (Sklyarov et al, 2011) (Table 1).…”
Section: Methodsmentioning
confidence: 99%
“…The values of pH ranged from 9.2 to 9.3. The water transparency varied from 0.5 m to 4.5 m (Itigilova et al, 2014).…”
Section: Methodsmentioning
confidence: 99%
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“…The ecosystem of Lake Zun-Torey follows the trend common for salt lakes, where lower water levels lead to a higher salinity and pH and, hence, to poorer species diversity (Gorlacheva et al, 2014;Itigilova et al, 2014). As the chemical properties of the water change, the total numbers and biomass of aquatic organisms may either increase (Echaniz, Vignatti, 2011;Vignatti et al, 2017) or decrease (Balushkina et al, 2009;Litvinenko et al, 2013).…”
Section: Discussionmentioning
confidence: 99%