Abstract

Harmful algal blooms (HABs) in arctic lakes are recent phenomena. In our study, we performed a long-term analysis (1990–2017) of the eutrophication of Lake Imandra, a large subarctic lake, and explored the biodiversity of bloom-forming microorganisms of a 2017 summer HAB. We performed a 16Sr rRNA metabarcoding study of microbial communities, analysed the associations between N, P, C, and chlorophyll concentrations in the lake water, and developed models for the prediction of HABs based on total P concentration. We have demonstrated that blooms in Lake Imandra occur outside of optimal Redfield ratios and have a nonlinear association with P concentrations. We found that recent summer HABs in a lake occur as simultaneous blooms of a diatom Aulacoseira sp. and cyanobacteria Dolichospermum sp. We have studied the temporal dynamics of microbial communities during the bloom and performed an analysis of the publicly available Dolichospermum genomes to outline potential genetic mechanisms beneath simultaneous blooming. We found genetic traits requisite for diatom-diazotroph associations, which may lay beneath the simultaneous blooming of Aulacoseira sp. and Dolichospermum sp. in Lake Imandra. Both groups of organisms have the ability to store nutrients and form a dormant stage. All of these factors will ensure the further development of the HABs in Lake Imandra and the dispersal of these bloom-forming species to neighboring lakes.

Highlights

  • Lake Imandra is the largest freshwater lake located in the southwestern part of the KolaPeninsula, Russia

  • We found that recent summer Harmful algal blooms (HABs) in a lake occur as simultaneous blooms of a diatom Aulacoseira sp. and cyanobacteria Dolichospermum sp

  • We found genetic traits requisite for diatom-diazotroph associations, which may lay beneath the simultaneous blooming of Aulacoseira sp. and Dolichospermum sp. in Lake Imandra

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Summary

Introduction

Lake Imandra is the largest freshwater lake located in the southwestern part of the KolaPeninsula, Russia. The lake has a surface area of 876 km , an average depth of 16 m, and a maximum depth of 67 m and is used for hydropower generation. The area is populated by approximately 80,000 people, and along with industrial effluents, the lake receives treated municipal wastewater from three settlements [1]. The apatite processing industry is a major source of phosphorous for Lake Imandra, while the mining industry (MI) and municipal wastewater (MWs) are sources of nitrogen. The load distribution is not equivalent among the major parts of the lake [2]. The most eutrophic part of the lake, Bolshaya Imandra (average mineralisation: 73.2 mg/L), receives 1233 tonnes of anthropogenic nitrogen (N) and 300 tonnes of phosphorous (P) annually. The two remaining parts of the lake, Jokostrovskaya Imandra (average mineralisation: 68.1 mg/L)

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