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首页> 外文期刊>Global change biology >Nitrogen concentration and delta super(15)N signature of ombrotrophicSphagnum mosses at different N deposition levels in Europe
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Nitrogen concentration and delta super(15)N signature of ombrotrophicSphagnum mosses at different N deposition levels in Europe

机译:欧洲不同氮沉降水平下滋养的水生苔藓的氮浓度和δsuper(15)N特征

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摘要

Alteration of the global nitrogen (N) cycle because of human-enhanced N fixation is a major concern particularly for those ecosystems that are nutrient poor by nature. Because Sphagnum-dominated mires are exclusively fed by wet and dry atmospheric deposition, they are assumed to be very sensitive to increased atmospheric N input. We assessed the consequences of increased atmospheric N deposition on total N concentration, N retention ability, and delta super(15)N isotopic signature of Sphagnum plants collected in 16 ombrotrophic mires across 11 European countries. The mires spanned a gradient of atmospheric N deposition from about 0.1 up to about 2 g m super(-2) yr super(-1). Mean N concentration in Sphagnum capitula was about 6 mg g super(-1) in less polluted mires and about 13 mg g super(-1) in highly N-polluted mires. The relative difference in N concentration between capitulum and stem decreased with increasing atmospheric N deposition, suggesting a possible metabolic mechanism that reduces excessive N accumulation in the capitulum. Sphagnum plants showed lower rates of N absorption under increasing atmospheric N deposition, indicating N saturation in Sphagnum tissues. The latter probably is related to a shift from N-limited conditions to limitation by other nutrients. The capacity of the Sphagnum layer to filter atmospheric N deposition decreased exponentially along the depositional gradient resulting in enrichment of the mire pore water with inorganic N forms (i.e., NO sub(3) super(-)+NH sub(4) super(+)). Sphagnum plants had delta super(15)N signatures ranging from about -8ppt to about -3ppt. The isotopic signatures were rather related to the ratio of reduced to oxidized N forms in atmospheric deposition than to total amount of atmospheric N deposition, indicating that delta super(15)N signature of Sphagnum plants can be used as an integrated measure of delta super(15)N signature of atmospheric precipitation. Indeed, mires located in areas characterized by greater emissions of NH sub(3) (i.e., mainly affected by agricultural activities) had Sphagnum plants with a lower delta super(15)N signature compared with mires located in areas dominated by NO sub(x) emissions (i.e., mainly affected by industrial activities).
机译:由于人为固氮作用的增强,全球氮循环的变化是一个主要问题,特别是对于那些自然营养贫乏的生态系统而言。由于以泥炭藓为主的泥潭仅由湿法和干法大气沉积物喂养,因此假定它们对增加的大气氮输入非常敏感。我们评估了增加的大气氮沉积量对欧洲11个国家的16个营养养分泥ro中所收集的泥炭藓植物总N浓度,N保留能力和δSuper(15)N同位素特征的影响。泥沼跨越了从约0.1到约2 g m super(-2)yr super(-1)的大气N沉积梯度。在污染较轻的泥潭中,泥炭藓中的平均N浓度约为6 mg g super(-1),而在高度N污染的泥沼中约为13 mg g super(-1)。随着大气中氮沉降量的增加,花冠和茎之间的氮浓度相对差异减小,表明可能的代谢机制减少了花冠中过多的氮积累。泥炭藓植物在增加的大气N沉积下显示出较低的N吸收速率,表明泥炭藓组织中的N饱和。后者可能与氮限制条件向其他营养素限制条件的转变有关。泥炭藓层过滤大气中N沉积的能力沿沉积梯度呈指数下降,导致泥孔水富含无机N形式(即NO sub(3)super(-)+ NH sub(4)super(+ ))。泥炭藓植物的δsuper(15)N特征值范围约为-8ppt至-3ppt。同位素特征与大气沉积物中还原态N的比值而非大气中氮沉积总量的比值有关,这表明水生植物的delta super(15)N特征值可以作为delta super( 15)N代表大气降水。确实,与以NO sub(x)为主的泥沼相比,位于以NH sub(3)的较大排放为特征(即主要受农业活动影响)的泥潭中,具有超低(15)N签名的泥炭藓植物具有较低的delta(15)N签名。 )排放(即主要受工业活动影响)。

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