Abstract

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 CO2 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 CO2 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-1 week-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-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 CO2 influx, while planktonic heterotrophy and CO2 production only occurred in the highest N treatments late in each experiment, and even in these cases, enclosures continued to in-gas CO2. Chemical effects on CO2 through calcite precipitation were also observed, but similarly did not change the direction of net CO2 flux. Taken together, these results demonstrate that atmospheric exchange of CO2 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 CO2 in-gassing in P-rich lake ecosystems.

Highlights

  • Hardwater lakes and reservoirs exhibit some of the most extreme rates of atmospheric CO2 exchange of any ecosystem [1], yet the magnitude and direction of gas flux can vary dramatically in space and time [1,2,3], suggesting multiple regulatory mechanisms [4,5]

  • Hardwater lakes are alkaline, rich in dissolved inorganic carbon (DIC) and nutrients, and highly productive [6,7], factors which favour rates of CO2 exchange (>200 mmol m-2 d-1) that greatly exceed those of other aquatic ecosystems [1,8,9]

  • The carbon (C) content of hardwater lakes is regulated by terrestrial subsidies of inorganic C rather than dissolved organic C (DOC) [10,11,12], with most dissolved C existing as bicarbonate (HCO3-) and carbonate (CO32-) rather than free CO2, when pH values exceed 8.5 [1,2]

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Summary

Introduction

Hardwater lakes and reservoirs exhibit some of the most extreme rates of atmospheric CO2 exchange of any ecosystem [1], yet the magnitude and direction of gas flux can vary dramatically in space and time [1,2,3], suggesting multiple regulatory mechanisms [4,5]. The carbon (C) content of hardwater lakes is regulated by terrestrial subsidies of inorganic C rather than dissolved organic C (DOC) [10,11,12], with most dissolved C existing as bicarbonate (HCO3-) and carbonate (CO32-) rather than free CO2, when pH values exceed 8.5 [1,2] They exhibit intense heterotrophic metabolism [5,13] and temperature-dependent precipitation of CaCO3 [14,15] that can lead to supersaturation of CO2 even at elevated pH [1,11]. Little is known of how autotrophic responses balance with responses from the heterotrophic community to control net biotic CO2 fluxes

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