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植物对升高的二氧化碳的化学计量响应因氮和磷输入而异:来自全球尺度荟萃分析的证据。

Plant stoichiometric responses to elevated CO2 vary with nitrogen and phosphorus inputs: Evidence from a global-scale meta-analysis.

作者信息

Huang Wenjuan, Houlton Benjamin Z, Marklein Alison R, Liu Juxiu, Zhou Guoyi

机构信息

Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650 China.

Department of Land, Air, and Water Resources, University of California-Davis, One Shields Avenue, Davis, CA 95616 USA.

出版信息

Sci Rep. 2015 Dec 14;5:18225. doi: 10.1038/srep18225.

Abstract

Rising levels of atmospheric CO2 have been implicated in changes in the nitrogen (N) and phosphorus (P) content of terrestrial vegetation; however, questions remain over the role of C, N and P interactions in driving plant nutrient stoichiometry, particularly whether N and P additions alter vegetation responses to CO2 enrichment singly. Here we use meta-analysis of 46 published studies to investigate the response of plant N and P to elevated CO2 alone and in combination with nutrient (N and P) additions across temperate vs. tropical biomes. Elevated CO2 reduces plant N concentrations more than plant P concentrations in total biomass pools, resulting in a significant decline in vegetation N/P. However, elevated CO2 treatments in combination with N additions increase plant P concentrations, whereas P additions have no statistical effect on plant N concentrations under CO2 enrichment. These results point to compensatory but asymmetrical interactions between N, P and CO2; that changes in N rapidly alter the availability of P, but not the converse, in response to increased CO2. Our finding implies widespread N limitation with increasing atmospheric CO2 concentrations alone. We also suggest that increased anthropogenic N deposition inputs could enhance plant N and P in a progressively CO2-enriched biosphere.

摘要

大气中二氧化碳水平的上升与陆地植被氮(N)和磷(P)含量的变化有关;然而,碳、氮和磷相互作用在驱动植物养分化学计量方面的作用仍存在疑问,特别是氮和磷的添加是否单独改变植被对二氧化碳富集的响应。在这里,我们对46项已发表的研究进行荟萃分析,以研究植物氮和磷对单独升高的二氧化碳以及与温带和热带生物群落中养分(氮和磷)添加相结合的响应。在总生物量库中,升高的二氧化碳降低植物氮浓度的幅度大于降低植物磷浓度的幅度,导致植被氮/磷显著下降。然而,升高的二氧化碳处理与氮添加相结合会增加植物磷浓度,而在二氧化碳富集条件下,磷添加对植物氮浓度没有统计学影响。这些结果表明氮、磷和二氧化碳之间存在补偿性但不对称的相互作用;即氮的变化会迅速改变磷的有效性,但在二氧化碳增加的情况下,磷的变化不会改变氮的有效性。我们的发现意味着仅随着大气二氧化碳浓度的增加就普遍存在氮限制。我们还表明,人为氮沉降输入的增加可能会在日益二氧化碳富集的生物圈中提高植物的氮和磷含量。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/aad3/4677399/c59c4b244e89/srep18225-f1.jpg

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