Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Institute of Soil and Water Resources and Environmental Science, Zhejiang University, Hangzhou, China.
Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, USA.
Glob Chang Biol. 2018 Aug;24(8):3452-3461. doi: 10.1111/gcb.14163. Epub 2018 Apr 25.
Long-term elevated nitrogen (N) input from anthropogenic sources may cause soil acidification and decrease crop yield, yet the response of the belowground microbial community to long-term N input alone or in combination with phosphorus (P) and potassium (K) is poorly understood. We explored the effect of long-term N and NPK fertilization on soil bacterial diversity and community composition using meta-analysis of a global dataset. Nitrogen fertilization decreased soil pH, and increased soil organic carbon (C) and available N contents. Bacterial taxonomic diversity was decreased by N fertilization alone, but was increased by NPK fertilization. The effect of N fertilization on bacterial diversity varied with soil texture and water management, but was independent of crop type or N application rate. Changes in bacterial diversity were positively related to both soil pH and organic C content under N fertilization alone, but only to soil organic C under NPK fertilization. Microbial biomass C decreased with decreasing bacterial diversity under long-term N fertilization. Nitrogen fertilization increased the relative abundance of Proteobacteria and Actinobacteria, but reduced the abundance of Acidobacteria, consistent with the general life history strategy theory for bacteria. The positive correlation between N application rate and the relative abundance of Actinobacteria indicates that increased N availability favored the growth of Actinobacteria. This first global analysis of long-term N and NPK fertilization that differentially affects bacterial diversity and community composition provides a reference for nutrient management strategies for maintaining belowground microbial diversity in agro-ecosystems worldwide.
长期以来,人为来源的氮(N)输入可能导致土壤酸化并降低作物产量,但人们对地下微生物群落对长期 N 输入(单独或与磷(P)和钾(K)结合)的反应知之甚少。我们通过对全球数据集的元分析,探讨了长期 N 和 NPK 施肥对土壤细菌多样性和群落组成的影响。N 施肥降低了土壤 pH 值,并增加了土壤有机碳(C)和有效 N 含量。单独 N 施肥降低了细菌分类多样性,但 NPK 施肥增加了细菌多样性。N 施肥对细菌多样性的影响因土壤质地和水分管理而有所不同,但与作物类型或 N 施用量无关。在单独 N 施肥下,细菌多样性的变化与土壤 pH 值和有机 C 含量呈正相关,但在 NPK 施肥下仅与土壤有机 C 呈正相关。长期 N 施肥下,微生物生物量 C 随细菌多样性的降低而降低。N 施肥增加了变形菌门和放线菌门的相对丰度,但降低了酸杆菌门的丰度,这与细菌的一般生活史策略理论一致。N 施用量与放线菌门相对丰度之间的正相关表明,增加的 N 有效性有利于放线菌的生长。这是首次对长期 N 和 NPK 施肥对细菌多样性和群落组成产生差异影响的全球分析,为全球农业生态系统中维持地下微生物多样性的养分管理策略提供了参考。