Denitrification and hydrologic transient storage in a glacial meltwater stream, McMurdo Dry Valleys, Antarctica

• Published in: Limnology and Oceanography
• Main Authors: Gooseff, Michael N., McKnight, Diane M., Runkel, Robert L., Duff, John H.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2004
• Subjects: McMurdo Dry Valleys; Antarc*; Antarctica
• Online Access: http://dx.doi.org/10.4319/lo.2004.49.5.1884; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2004.49.5.1884; https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2004.49.5.1884

In extreme environments, retention of nutrients within stream ecosystems contributes to the persistence of aquatic biota and continuity of ecosystem function. In the McMurdo Dry Valleys, Antarctica, many glacial meltwater streams flow for only 5–12 weeks a year and yet support extensive benthic microbial communities. We investigated NO 3 − uptake and denitrification in Green Creek by analyzing small‐scale microbial mat dynamics in mesocosms and reach‐scale nutrient cycling in two whole‐stream NO 3 − enrichment experiments. Nitrate uptake results indicated that microbial mats were nitrogen (N)‐limited, with NO 3 − uptake rates as high as 16 nmol N cm −2 h −1 . Denitrification potentials associated with microbial mats were also as high as 16 nmol N cm −2 h −1 . During two whole‐stream NO 3 − −enrichment experiments, a simultaneous pulse of NO 2 − was observed in the stream water. The one‐dimensional solute transport model with inflow and storage was modified to simulate two storage zones: one to account for short time scale hydrologic exchange of stream water into and out of the benthic microbial mat, the other to account for longer time scale hydrologic exchange with the hyporheic zone. Simulations indicate that injected NO 3 − was removed both in the microbial mat and in the hyporheic zone and that as much as 20% of the NO 3 − that entered the microbial mat and hyporheic zone was transformed to NO 2 − by dissimilatory reduction. Because of the rapid hydrologic exchange in microbial mats, it is likely that denitrification is limited either by biotic assimilation, reductase limitation, or transport limitation (reduced NO 2 − is transported away from reducing microbes).