首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Nonlinear responses to nitrogen and strong interactions with nitrogenand phosphorus additions drastically alter the structure and functionof a high arctic ecosystem
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Nonlinear responses to nitrogen and strong interactions with nitrogenand phosphorus additions drastically alter the structure and functionof a high arctic ecosystem

机译:对氮的非线性响应以及与氮和磷的强相互作用强烈地改变了北极高生态系统的结构和功能

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Significant changes in ecosystem CO2 exchange and vegetation characteristics wereobserved following multiple additions of nitrogen (N) and factorial additions of Nand phosphorus (P) to prostrate dwarf-shrub, herb tundra in Northwest Greenland.Ecosystem CO2 exchange and vegetation cover and composition were very sensitive tolow rates of N inputs (0.5 g M-2 y-'), indicating that even low rates of atmosphericN deposition may alter high arctic ecosystem structure and function. Increasing Naddition from 1 to 5 g N M-2 y-1 did not alter CO2 exchange or vegetation characteristics,suggesting the ecosystem had become N saturated. Factorial additions of both N andP released the ecosystem from N saturation and dramatically increased grossecosystem photosynthesis (+500%) and ecosystem respiration (+250%), such that theecosystem switched from a small source of CO2 to a small sink for CO2 at middayduring the 2005 growing season. Changes in the component fluxes of CO2 exchangewere largely explained by a doubling of the normalized difference vegetation index, a100% increase in vascular plant cover and dramatic increases in the abundance of severalpreviously rare grass species. Our results clearly demonstrate that high arctic prostratedwarf-shrub, herb tundra is highly sensitive to low levels of N addition and that futureincreases in N deposition or N mineralization will likely lead to change in carboncycling and vegetation characteristics, but the magnitude of the response will beconstrained by P availability.
机译:在西北格陵兰西南部矮化灌丛,草本冻原中多次添加氮(N)和因子磷(N)后,观察到生态系统CO2交换和植被特征发生了显着变化。生态系统CO2交换,植被覆盖和组成非常敏感降低了氮的输入速率(0.5 g M-2 y-'),表明即使较低的大气氮沉积速率也可能会改变北极的高生态系统结构和功能。将N的添加量从1 g N M-2 y-1增加到5 g不会改变CO2交换或植被特征,暗示生态系统已变为N饱和。 N和P的因子添加使生态系统从N饱和状态释放出来,并显着增加了生态系统的光合作用(+ 500%)和生态系统呼吸作用(+ 250%),从而使生态系统在中午期间从少量的CO2变为较小的CO2汇。 2005年生长季节。归一化差异植被指数加倍,维管植物覆盖率增加100%以及几种先前稀有草种的丰度显着增加,很大程度上解释了CO2交换通量的变化。我们的结果清楚地表明,高寒带刺的灌木丛,草本苔原对低水平的氮添加高度敏感,未来氮沉降或氮矿化的增加可能会导致碳循环和植被特征的变化,但是响应的幅度将受到限制。由P可用性。

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