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Nitrogen deposition and warming - effects on phytoplankton nutrient limitation in subarctic lakes.

机译:氮沉积和变暖-对北极湖中浮游植物养分限制的影响。

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The aim of this study was to predict the combined effects of enhanced nitrogen (N) deposition and warming on phytoplankton development in high latitude and mountain lakes. Consequently, we assessed, in a series of enclosure experiments, how lake water nutrient stoichiometry and phytoplankton nutrient limitation varied over the growing season in 11 lakes situated along an altitudinal/climate gradient with low N-deposition (<1 kg N ha-1 yr-1) in northern subarctic Sweden. Short-term bioassay experiments with N- and P-additions revealed that phytoplankton in high-alpine lakes were more prone to P-limitation, and with decreasing altitude became increasingly N- and NP-colimited. Nutrient limitation was additionally most obvious in midsummer. There was also a strong positive correlation between phytoplankton growth and water temperature in the bioassays. Although excess nutrients were available in spring and autumn, on these occasions growth was likely constrained by low water temperatures. These results imply that enhanced N-deposition over the Swedish mountain areas will, with the exception of high-alpine lakes, enhance biomass and drive phytoplankton from N- to P-limitation. However, if not accompanied by warming, N-input from deposition will stimulate limited phytoplankton growth due to low water temperatures during large parts of the growing season. Direct effects of warming, allowing increased metabolic rates and an extension of the growing season, seem equally crucial to synergistically enhance phytoplankton development in these lakes.
机译:这项研究的目的是预测高纬度和高山湖泊中增加的氮(N)沉积和变暖对浮游植物发展的综合影响。因此,我们通过一系列围护实验评估了11个湖泊中沿垂直/气候梯度,低N沉积(<1 kg N ha <补充>)的11个湖泊在生长季节内湖水养分的化学计量和浮游植物养分限制如何变化。 -1(sup> yr -1 ))。短期添加N和P的生物测定实验表明,高高山湖泊中的浮游植物更容易受到P限制,并且随着海拔的降低,N和NP限制越来越多。营养限制在仲夏最为明显。在生物测定中,浮游植物的生长与水温之间也存在很强的正相关。尽管春季和秋季有过量的养分,但在这种情况下,生长温度很可能受到水温低的限制。这些结果表明,除高高山湖泊外,瑞典山区N沉积的增加将增加生物量,并使浮游植物从N限制向P限制。但是,如果不伴有变暖,由于在生长期的大部分时间内水温较低,沉积物中的氮输入将刺激有限的浮游植物生长。变暖的直接影响(允许增加的代谢率和延长生长期)对于协同增强这些湖泊中浮游植物的发育似乎同样至关重要。

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