Nitrogen Fixation in Arctic Coastal Waters (Qeqertarsuaq, West Greenland): Influence of Glacial Melt on Diazotrophs, Nutrient Availability, and Seasonal Blooms
Abstract. The Arctic Ocean is undergoing rapid transformation due to climate change, with decreasing sea ice contributing to a predicted increase in primary productivity. A critical factor determining future productivity in this region is the availability of nitrogen, a key nutrient that often limits biological growth in Arctic waters. The fixation of dinitrogen (N2) gas, a biological process mediated by diazotrophs, not only supplies new nitrogen to the ecosystem but also plays a central role in shaping the biological productivity of the Arctic. Historically it was believed to be limited to oligotrophic tropical and subtropical oceans, Arctic N2 fixation has only garnered significant attention over the past decade, leaving a gap in our understanding of its magnitude, the diazotrophic community, and potential environmental drivers. In this study, we investigated N2 fixation rates and the diazotrophic community in Arctic coastal waters, using a combination of isotope labeling, genetic analyses and biogeochemical profiling, in order to explore its response to glacial meltwater, nutrient availability and its impact on primary productivity. Here we show, N2 fixation rates, ranging from 0.16 to 2.71 nmol N L-1 d-1, to be notably higher than those observed in many other oceanic regions, suggesting a previously unrecognized significance of N2 fixation in these high-latitude waters. The diazotrophic community is predominantly composed of UCYN-A. We found highest N2 fixation rates co-occurring with maximum chlorophyll a concentrations and primary production rates at a station in the Vaigat Strait close impacted by glacier meltwater inflow, possibly providing otherwise limiting nutrients. Our findings illustrate the importance of N2 fixation in an environment previously not considered important for this process and provide insights into its response to the projected melting of the polar ice cover.