Department of Ecology and Environmental Science, Umeå University, Umeå, Sweden.
Ecology. 2017 Apr;98(4):982-994. doi: 10.1002/ecy.1758.
Global change has increased inorganic nitrogen (N) and dissolved organic carbon (DOC; i.e., "browning") inputs to northern hemisphere boreal lakes. However, we do not know how phytoplankton in nutrient poor lake ecosystems of different DOC concentration respond to increased N availability. Here, we monitored changes in phytoplankton production, biomass and community composition in response to whole lake inorganic N fertilization in six boreal unproductive Swedish lakes divided into three lake pairs (control, N enriched) at three DOC levels (low, medium, high), with one reference year (2011) and 2 impact yr (2012, 2013). We found that phytoplankton biomass and production decreased with DOC concentration before N fertilization. Further, phytoplankton community composition also differed with respect to DOC, with a dominance of non-flagellated autotrophs at low DOC towards an increasing dominance of flagellated autotrophs with increased lake DOC concentration. The N fertilization increased phytoplankton biomass and production in all lakes, but did not affect phytoplankton community composition. However, the net response in biomass and production to N fertilization declined with increasing DOC, implying that the lake DOC concentration is critical in order to infer phytoplankton responses to N fertilization, and that the system switches from being primarily nutrient limited to becoming increasingly light limited with increased DOC concentration. In conclusion, our results show that browning will reduce phytoplankton production and biomass and influence phytoplankton community composition, whereas increased inorganic N loadings from deposition, forestry or other land use will primarily enhance phytoplankton biomass and production. Together, any change in the landscape that enhances inorganic N availability will increase phytoplankton production and biomass, but the positive effects of N will be much weaker or even neutralized in browner lakes as caused by light limitation.
全球变化增加了北半球北方冷水湖泊的无机氮(N)和溶解有机碳(DOC;即“褐变”)的输入。然而,我们不知道在不同 DOC 浓度的贫营养湖泊生态系统中,浮游植物对增加的 N 供应有何反应。在这里,我们监测了在 6 个北方贫瘠的瑞典湖泊中,由于整个湖泊无机 N 施肥,浮游植物生产力、生物量和群落组成的变化,这些湖泊分为 3 对(对照、富 N),DOC 水平(低、中、高),有一个参考年(2011 年)和 2 个影响年(2012 年、2013 年)。我们发现,浮游植物生物量和生产力在 N 施肥前随 DOC 浓度的增加而减少。此外,浮游植物群落组成也因 DOC 而不同,低 DOC 时以非鞭毛自养生物为主,随着湖泊 DOC 浓度的增加,鞭毛自养生物的优势逐渐增加。N 施肥增加了所有湖泊的浮游植物生物量和生产力,但没有影响浮游植物群落组成。然而,N 施肥对生物量和生产力的净响应随 DOC 的增加而下降,这意味着湖泊 DOC 浓度是推断浮游植物对 N 施肥反应的关键,并且随着 DOC 浓度的增加,系统从主要受营养限制转变为越来越受光限制。总之,我们的结果表明,褐变将减少浮游植物的生产力和生物量,并影响浮游植物的群落组成,而沉积、林业或其他土地利用增加的无机 N 负荷将主要增强浮游植物的生物量和生产力。总的来说,任何增强无机 N 可用性的景观变化都会增加浮游植物的生产力和生物量,但在较深褐色的湖泊中,由于光限制,N 的积极影响将减弱甚至被中和。