短期氮添加通过调节喀斯特森林磷循环微生物群落提高土壤磷有效性

IF 6.6 1区 农林科学 Q1 SOIL SCIENCE
Yuanshuang Yuan, Xianwang Du, Yicong Yin, Guowei Xia
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引用次数: 0

摘要

氮沉降与土壤磷消耗之间的不平衡日益加剧,加大了研究陆地生态系统磷循环过程的紧迫性。然而,在氮沉降增强的情况下,磷循环功能谱驱动土壤磷动员的机制仍有待研究。在喀斯特森林进行了为期3年的不同速率的施氮试验后,我们确定了参与调节根际和块状土壤中磷循环的土壤磷组分和相关细菌群落。结果表明,施氮增加了块状土壤(低氮+ 17%,高氮+ 22%)和根际土壤(+6%,+ 23%)的植物有效磷,同时降低了块状土壤(- 18%,- 24%)和根际土壤(- 8%,- 23%)的有机磷。此外,N处理显著改变了P循环细菌群落的组成,增加了群落的丰富度,表明N输入可能通过调节参与P循环的细菌群落来提高P的有效性。此外,我们发现负责磷转化的功能细菌基因在块状土壤和根际土壤之间存在差异。在块状土壤中,施氮显著增加了磷矿化基因和磷增溶基因。根际土壤中磷矿化和磷调控基因随施氮量的增加而增加。综上所述,施氮可通过调节磷循环功能菌群提高土壤磷有效性;然而,驱动磷动员的具体功能特征可能在散装土壤和根际土壤之间有所不同。这些发现从微生物基因的角度对全球变化(如氮沉降)下陆地生态系统土壤磷循环的调控过程提供了新的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Short-term nitrogen addition improves soil phosphorus availability by regulating phosphorus-cycling microbial communities in a karst forest
The widening imbalance between escalating nitrogen (N) deposition and depleting soil phosphorus (P) amplifies the urgency of investigating P cycling processes in terrestrial ecosystems. However, the mechanisms by which P-cycling functional profiles drive soil P mobilization under enhanced N deposition remain to be addressed. After a three-year N-addition experiment at varying rates in a karst forest, we determined the soil P fractions and associated bacterial communities involved in regulating P cycling in rhizosphere and bulk soils. Our results showed that N addition increased plant-available P in both bulk soil (+17 % under low N, +22 % under high N) and rhizosphere soil (+6%, +23 %), while concurrently reducing organic P in bulk soil (−18 %, −24 %) and rhizosphere soil (−8%, –23 %) under corresponding N rates. In addition, N treatment substantially shifted the composition of the P-cycling bacterial community and increased the richness of the community, indicating that N input enhances P availability, potentially through the regulation of the bacterial communities involved in P cycling. Moreover, we found that the functional bacterial genes responsible for P transformation differed between the bulk and rhizosphere soils. Specifically, in the bulk soil, P mineralization genes and P solubilization genes were significantly increased by N treatment. In contrast, in the rhizosphere soil, P mineralization and P regulation genes increased in response to N addition. Together, these results suggest that N addition improves soil P availability by regulating P-cycling functional bacterial communities; however, the specific functional profiles driving P mobilization may differ between bulk and rhizosphere soils. These findings provide novel insight into the regulatory processes of soil P cycling in terrestrial ecosystems under global changes (e.g., N deposition) from a microbial gene perspective.
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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