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Belowground competition and the response of developing forest communities to atmospheric CO2 and O-3

机译:地下竞争和发展中的森林群落对大气CO2和O-3的响应

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As human activity continues to increase CO2 and O-3, broad expanses of north temperate forests will be simultaneously exposed to elevated concentrations of these trace gases. Although both CO2 and O-3 are potent modifiers of plant growth, we do not understand the extent to which they alter competition for limiting soil nutrients, like nitrogen (N). We quantified the acquisition of soil N in two 8-year-old communities composed of trembling aspen genotypes (n = 5) and trembling aspen-paper birch which were exposed to factorial combinations of CO2 (ambient and 560 mu L L-1) and O-3 (ambient = 30-40 vs. 50-60 nL L-1). Tracer amount of (NH4+)-N-15 were applied to soil to determine how these trace gases altered the competitive ability of genotypes and species to acquire soil N. One year after isotope addition, we assessed N acquisition by measuring the amount of N-15 tracer contained in the plant canopy (i.e. recent N acquisition), as well as the total amount of canopy N (i.e. cumulative N acquisition). Exposure to elevated CO2 differentially altered recent and cumulative N acquisition among aspen genotypes, changing the rank order in which they obtained soil N. Elevated O-3 also altered the rank order in which aspen genotypes obtained soil N by eliciting increases, decreases and no response among genotypes. If aspen genotypes respond similarly under field conditions, then rising concentrations of CO2 and O-3 could alter the structure of aspen populations. In the aspen-birch community, elevated CO2 increased recent N (i.e. N-15) acquisition in birch (68%) to a greater extent than aspen (19%), suggesting that, over the course of this experiment, birch had gained a competitive advantage over aspen. The response of genotypes and species to rising CO2 and O-3 concentrations, and how these responses are modified by competitive interactions, has the potential to change the future composition and productivity of northern temperate forests.
机译:随着人类活动继续增加CO2和O-3的排放,广阔的北方温带森林将同时暴露于高浓度的这些痕量气体中。尽管CO2和O-3都是植物生长的有效调节剂,但我们不了解它们在多大程度上改变了对限制土壤养分(如氮)的竞争。我们量化了两个8岁的社区的土壤氮素的获取,这些社区由颤抖的白杨基因型(n = 5)和颤抖的白杨纸桦木组成,暴露于CO2的分解组合(环境和560μL L-1)和O-3(环境= 30-40对50-60 nL L-1)。将示踪量的(NH4 +)-N-15应用于土壤,以确定这些微量气体如何改变基因型和物种获取土壤N的竞争能力。添加同位素一年后,我们通过测量N-的量来评估氮的获取植物冠层(即最近的N采集)中包含的15种示踪剂,以及冠层N的总量(即累积的N采集)。暴露于升高的CO2会不同地改变白杨基因型之间最近和累积的N吸收,从而改变他们获得土壤N的等级顺序。升高的O-3也会改变白杨基因型通过引起增加,降低和无反应而获得土壤N的等级顺序。在基因型之间。如果白杨基因型在田间条件下也有类似反应,那么升高的CO2和O-3浓度可能会改变白杨种群的结构。在白桦树群落中,升高的二氧化碳增加了桦树中新近获得的N(即N-15)(68%),其增幅大于白杨树(19%),这表明在该实验过程中,桦树获得了与白杨的竞争优势。基因型和物种对CO2和O-3浓度升高的反应,以及如何通过竞争相互作用改变这些反应,有可能改变北部温带森林的未来组成和生产力。

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