Romanenko V I, Peres Eĭris M, Kudriavtsev V M, Avrora Pubienes M
Mikrobiologiia. 1976 May-Jun;45:539-46.
The lake was studied in April and July of 1973. Gleothece prevailed in mixolimnion and green sulphur bacterium Pelodyction phaeum in the layer of pink water down to 10 m. The production of photosynthetic suphlur bacteria comprises 3% of the production of algae. Sulphate reduction takes place mainly in water beyond the layer of sulphur bacteria. The content of hydrogen sulphide in monimolimnion is 104 mg/litre. Bacteria utilize, at the account of photosynthesis, 40% of produced hydrogen sulphide. Three maxima in the bacterial content in water have been registered: (a) at a depth of 7 m; (b) in the layer of pink water, at a depth of 10 m; (c) at the bottom. Total mineralization and electroconductance of water at the bottom are higher by a factor of 6 than those at the surface. Destruction of organic substance is higher than its production a little.
1973年4月和7月对该湖泊进行了研究。在混合湖上层，格氏藻占优势，而在深度达10米的粉色水层中，绿色硫细菌暗褐泥生绿菌占优势。光合硫细菌的产量占藻类产量的3%。硫酸盐还原主要发生在硫细菌层以外的水中。静水层中硫化氢含量为104毫克/升。细菌通过光合作用利用了所产生硫化氢的40%。已记录到水中细菌含量的三个最大值：(a) 在7米深处；(b) 在粉色水层，10米深处；(c) 在底部。底部水的总矿化度和电导率比表层高6倍。有机物的分解略高于其产生量。
