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氮沉降、植物碳分配和土壤微生物:由于富营养化而改变的相互作用。

Nitrogen deposition, plant carbon allocation, and soil microbes: changing interactions due to enrichment.

机构信息

Department of Environmental Science, Policy & Management, University of California, Berkeley, Berkeley, California 94720, USA.

出版信息

Am J Bot. 2013 Jul;100(7):1458-70. doi: 10.3732/ajb.1200513. Epub 2013 Jun 26.

Abstract

PREMISE OF THE STUDY

Nitrogen (N) inputs to the terrestrial environment have doubled worldwide during the past century. N negatively impacts plant diversity, but it is unknown why some species are more susceptible than others. While it is often assumed that competition drives species decline, N enrichment also strongly affects soil microbial communities. Can these changes affect plant-microbe interactions in ways that differentially influence success of plant species? Furthermore, can altered plant-microbe interactions lead to carbon (C) limitation in plants?

METHODS

We focused on a species that increases (Deschampsia cespitosa) and one that decreases (Geum rossii) in abundance in N-fertilized plots in alpine tundra. We measured soil microbes using phospholipid fatty acids, and C limitation and transfer using a (13)C tracer experiment, C:N ratios, nonstructural carbohydrates, and leaf preformation.

KEY RESULTS

While N profoundly influenced microbial communities, this change occurred similarly in association with both plant species. N addition did not alter total C allocation to microbes in either species, but it changed patterns of microbial C acquisition more in Geum, specifically in gram-negative bacteria. Geum showed evidence of C limitation: it allocated less C to storage organs, had lower C:N and carbohydrate stores, and fewer preformed leaves in N plots.

CONCLUSIONS

Carbon limitation may explain why some species decline with N enrichment, and the decline may be due to physiological responses of plants to N rather than to altered plant-microbe interactions. Global change will alter many processes important in structuring plant communities; noncompetitive mechanisms of species decline may be more widespread than previously thought.

摘要

研究前提

在过去的一个世纪中,全球范围内向陆地环境输入的氮(N)增加了一倍。N 对植物多样性有负面影响,但尚不清楚为什么有些物种比其他物种更容易受到影响。虽然人们通常认为竞争导致物种减少,但 N 富集也强烈影响土壤微生物群落。这些变化是否会以不同的方式影响植物-微生物相互作用,从而影响植物物种的成功?此外,改变的植物-微生物相互作用是否会导致植物的碳(C)限制?

方法

我们专注于一种在高山冻原中 N 施肥样地中丰度增加(Deschampsia cespitosa)和减少(Geum rossii)的物种。我们使用磷脂脂肪酸来测量土壤微生物,并用 13C 示踪实验、C:N 比、非结构性碳水化合物和叶片预成型来测量 C 限制和转移。

主要结果

虽然 N 深刻地影响了微生物群落,但这种变化在与两种植物物种相关联时发生的方式相似。N 添加并没有改变两种植物物种中总 C 向微生物的分配,但它改变了 Geum 中微生物 C 获得的模式,特别是在革兰氏阴性细菌中。Geum 表现出 C 限制的迹象:它向储存器官分配的 C 较少,C:N 和碳水化合物储存较低,N 样地中预先形成的叶片较少。

结论

碳限制可能解释了为什么一些物种随着 N 富集而减少,而这种减少可能是由于植物对 N 的生理反应,而不是由于改变的植物-微生物相互作用。全球变化将改变许多对植物群落结构重要的过程;物种减少的非竞争机制可能比以前想象的更为普遍。

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