Effects of experimental nitrogen fertilization on planktonic metabolism and CO.sub.2 flux in a hypereutrophic hardwater lake

• Published in: PloS one Vol. 12; no. 12; p. e0188652
• Main Authors: Bogard, Matthew J, Finlay, Kerri, Waiser, Marley J, Tumber, Vijay P, Donald, Derek B, Wiik, Emma, Simpson, Gavin L, del Giorgio, Paul A, Leavitt, Peter R
• Format: Journal Article
• Language: English
• Published: Public Library of Science 12-12-2017
• Subjects: Analysis; Environmental aspects; Eutrophication; Lakes; Nitrogen metabolism; Physiological aspects; Canada
• ISSN: 1932-6203; 1932-6203
• DOI: 10.1371/journal.pone.0188652

Hardwater lakes are common in human-dominated regions of the world and often experience pollution due to agricultural and urban effluent inputs of inorganic and organic nitrogen (N). Although these lakes are landscape hotspots for CO.sub.2 exchange and food web carbon (C) cycling, the effect of N enrichment on hardwater lake food web functioning and C cycling patterns remains unclear. Specifically, it is unknown if different eutrophication scenarios (e.g., modest non point vs. extreme point sources) yield consistent effects on auto- and heterotrophic C cycling, or how biotic responses interact with the inorganic C system to shape responses of air-water CO.sub.2 exchange. To address this uncertainty, we induced large metabolic gradients in the plankton community of a hypereutrophic hardwater Canadian prairie lake by adding N as urea (the most widely applied agricultural fertilizer) at loading rates of 0, 1, 3, 8 or 18 mg N L.sup.-1 week.sup.-1 to 3240-L, in-situ mesocosms. Over three separate 21-day experiments, all treatments of N dramatically increased phytoplankton biomass and gross primary production (GPP) two- to six-fold, but the effects of N on autotrophs plateaued at ~3 mg N L.sup.-1 . Conversely, heterotrophic metabolism increased linearly with N fertilization over the full treatment range. In nearly all cases, N enhanced net planktonic uptake of dissolved inorganic carbon (DIC), and increased the rate of CO.sub.2 influx, while planktonic heterotrophy and CO.sub.2 production only occurred in the highest N treatments late in each experiment, and even in these cases, enclosures continued to in-gas CO.sub.2 . Chemical effects on CO.sub.2 through calcite precipitation were also observed, but similarly did not change the direction of net CO.sub.2 flux. Taken together, these results demonstrate that atmospheric exchange of CO.sub.2 in eutrophic hardwater lakes remains sensitive to increasing N loading and eutrophication, and that even modest levels of N pollution are capable of enhancing autotrophy and CO.sub.2 in-gassing in P-rich lake ecosystems.