Small Boreal Lake Ecosystem Evolution under the Influence of Natural and Anthropogenic Factors: Results of Multidisciplinary Long-Term Study

• Published in: Water
• Main Authors: Liudmila Shirokova, Taissia Vorobieva, Svetlana Zabelina, Sergey Klimov, Olga Moreva, Artem Chupakov, Natalia Makhnovich, Vladimir Gogolitsyn, Elena Sobko, Natalia Shorina, Natalia Kokryatskaya, Anna Ershova, Oleg Pokrovsky
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2016
• Subjects: boreal; multidisciplinary long-term study; small lake; Hydraulic engineering; TC1-978; Water supply for domestic and industrial purposes; TD201-500; Canada; Boreal Lake; Humic Lake; Northwest Russia
• Online Access: https://doi.org/10.3390/w8080316; https://doaj.org/article/3c37c521c14a4381ac4f67d417bb521b

Small aquatic ecosystems of the boreal zone are known to be most sensitive indicators of on-going environmental change as well as local anthropogenic pressure, while being highly vulnerable to external impacts. Compared to rather detailed knowledge of the evolution of large and small lakes in Scandinavia and Canada, and large lakes in Eurasia, highly abundant small boreal lakes of northwest Russia have received very little attention, although they may become important centers of attraction of growing rural population in the near future. Here we present the results of a multidisciplinary, multi-annual study of a small boreal humic lake of NW Russia. A shallow (3 m) and a deep (16 m) site of this lake were regularly sampled for a range of chemical and biological parameters. Average multi-daily, summer-time values of the epilimnion (upper oxygenated) layer of the lake provided indications of possible trends in temperature, nutrients, and bacterio-plankton concentration that revealed the local pollution impact in the shallow zone and overall environmental trend in the deep sampling point of the lake. Organic phosphorus, nitrate, and lead were found to be most efficient tracers of local anthropogenic pollution, especially visible in the surface layer of the shallow site of the lake. Cycling of trace elements between the epilimnion and hypolimnion is tightly linked to dissolved organic matter speciation and size fractionation due to the dominance of organic and organo-ferric colloids. The capacity of lake self-purification depends on the ratio of primary productivity to mineralization of organic matter. This ratio remained >1 both during winter and summer periods, which suggests a high potential of lake recovery from the input of allochthonous dissolved organic matter and local anthropogenic pollution.