Dominance of net autotrophy in arid landscape low relief polar lakes, Nunavut, Canada.

The Arctic is the fastest warming biome on the planet, and environmental changes are having striking effects on freshwater ecosystems that may impact the regional carbon cycle. The metabolic state of Arctic lakes is often considered net heterotrophic, due to an assumed supply of allochthonous organic matter that supports ecosystem respiration and carbon mineralization in excess of rates of primary production. However, lake metabolic patterns vary according to regional climatic characteristics, hydrological connectivity, organic matter sources and intrinsic lake properties, and the metabolism of most Arctic lakes is unknown. We sampled 35 waterbodies along a connectivity gradient from headwater to downstream lakes, on southern Victoria Island, Nunavut, in an area characterized by low precipitation, organic-poor soils, and high evaporation rates. We evaluated whether lakes were net autotrophic or heterotrophic during the open water period using an oxygen isotopic mass balance approach. Most of the waterbodies were autotrophic and sites of net organic matter production or close to metabolic equilibrium. Autotrophy was associated with higher benthic primary production, as compared to its pelagic counterpart, due to the high irradiance reaching the bottom and efficient internal carbon and nutrient cycling. Highly connected midstream and downstream lakes showed efficient organic matter cycling, as evidenced by the strong coupling between gross primary production (GPP) and ecosystem respiration, while decoupling was observed in some headwater lakes with significantly higher GPP. The shallow nature of lakes in the flat, arid region of southern Victoria Island supports net autotrophy in most lakes during the open water season. Ongoing climate changes that lengthen the ice-free irradiance period and increase rates of nutrient evapoconcentration may further promote net autotrophy, with uncertain long-term effects for lake functioning.

Biosensor for screening bacterial mercury methylation: example within the Desulfobulbaceae.

Mercury methylation and demethylation processes govern the fate of methylmercury in aquatic ecosystems. Under anoxic conditions, methylation activity is mainly of biological origin and is often the result of sulfate-reducing bacteria. In this study, the use of a luminescent biosensor for screening methylmercury production was validated by exposing the reporter strain to methylating or non-methylating Desulfovibrio strains. The sensitivity of the biosensor to methylmercury was shown to depend on sulfate-reducing bacterial growth conditions. Bioluminescence was measured using 1-10 mM of sulfides. As the sulfide level increased, luminescence decreased by 40-70%, respectively. Nevertheless, assuming an average of 5 mM of sulfide produced during sulfate-reducing growth, a mercury methylation potential of over 4% was detected when using 185 nM of inorganic mercury. Due to technical limitations, mercury speciation has, to date, only been investigated in a small number of bacterial strains, and no consistent phylogenetic distribution has been identified. Here, the biosensor was further used to assess the Hg methylation capacities of an additional 21 strains related to the Desulfobulbaceae. Seven of them were identified as methylmercury producers. Cultivation procedures combined with bacterial biosensors could provide innovative tools to identify new methylator clades amongst the prokaryotes.