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首页> 外文期刊>Global change biology >Atmospheric CO2 and O3 alter competition for soil nitrogen in developing forests.
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Atmospheric CO2 and O3 alter competition for soil nitrogen in developing forests.

机译:大气中CO 2 和O 3 的变化改变了发展中森林对土壤氮的竞争。

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摘要

Plant growth responses to rising atmospheric CO2 and O3 vary among genotypes and between species, which could plausibly influence the strength of competitive interactions for soil N. Ascribable to the size-symmetric nature of belowground competition, we reasoned that differential growth responses to CO2 and O3 should shift as juvenile individuals mature, thereby altering competitive hierarchies and forest composition. In a 12-year-long forest FACE experiment, we used tracer 15N and whole-plant N content to assess belowground competitive interactions among five Populus tremuloides genotypes, between a single P. tremuloides genotype and Betula papryrifera, as well as between the same single P. tremuloides genotype and Acer saccharum. Under elevated CO2, the amount of soil N and 15N obtained by the P. tremuloides genotype common to each community was contingent on the nature of belowground competition. When this genotype competed with its congeners, it obtained equivalent amounts of soil N and tracer 15N under ambient and elevated CO2; however, its acquisition of soil N under elevated CO2 increased by a significant margin when grown in competition with B. papyrifera (+30%) and A. saccharum (+60%). In contrast, elevated O3 had no effect on soil N and 15N acquisition by the P. tremuloides genotype common in each community, regardless of competitive interactions. Under elevated CO2, the rank order of N acquisition among P. tremuloides genotypes shifted over time, indicating that growth responses to CO2 change during ontogeny; this was not the case under elevated O3. In the aspen-birch community, the competitive advantage elevated CO2 initially conveyed on birch diminished over time, whereas maple was a poor competitor for soil N in all regards. The extent to which elevated CO2 and O3 will shape the genetic structure and composition of future forests is, in part, contingent on the time-dependent effects of belowground competition on plant growth response.
机译:植物对大气CO 2 和O 3 上升的生长响应在基因型之间和物种之间变化,这可能似乎影响了土壤氮素竞争性相互作用的强度。我们认为地下竞争具有对称性,因此随着少年个体的成熟,对CO 2 和O 3 的不同生长响应应该发生变化,从而改变了竞争等级和森林组成。在一项为期12年的森林FACE实验中,我们使用示踪剂 15 N和全株N含量评估了单个基因之间的五种杨木基因型之间的地下竞争相互作用。 P tremuloides 基因型和 Betula papryrifera 以及同一单个 P之间。 tremuloides 基因型和蔗糖。在CO 2 升高的情况下, P获得的土壤氮和 15 N量。每个群落共有的tremuloides 基因型取决于地下竞争的性质。当该基因型与其同族竞争时,在环境和升高的CO 2 下获得了等量的土壤氮和示踪物 15 N;然而,与 B竞争生长时,在CO 2 升高的条件下,其对土壤氮的吸收显着增加。纸莎草(+ 30%)和 A。糖(+ 60%)。相反,升高的O 3 对 P采集的土壤氮和 15 N无效。不论竞争性相互作用如何,在每个社区中常见的tremuloides 基因型。在CO 2 升高的情况下, P中氮素获取的排名顺序。 tremuloides 基因型随时间变化,表明在个体发育过程中对CO 2 的生长响应发生了变化。在O 3 升高的情况下不是这种情况。在白桦树群落中,最初通过桦树传递的CO 2 的竞争优势随着时间的推移而降低,而枫树在所有方面都不是土壤氮的竞争者。升高的CO 2 和O 3 对未来森林的遗传结构和组成的影响程度部分取决于地下竞争对森林的时间依赖性。植物生长反应。

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