Long-term organic fertilization regulates the abundance of major nitrogen-cycling-related genes in aggregates from an acidic Ultisol

被引:18
|
作者
Lin, Yongxin [1 ,2 ]
Ye, Guiping [1 ,3 ]
Luo, Jiafa [4 ]
Di, Hong J. [5 ]
Lindsey, Stuart [4 ]
Fan, Jianbo [1 ]
Liu, Deyan [1 ]
Ding, Weixin [1 ]
机构
[1] Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China
[2] Fujian Normal Univ, Sch Geog Sci, Key Lab Humid Subtrop Eco Geog Proc, Minist Educ, Fuzhou 350007, Peoples R China
[3] Minjiang Univ, Inst Oceanog, Fuzhou 350108, Peoples R China
[4] AgResearch Ltd, Ruakura Res Ctr, Hamilton 3240, New Zealand
[5] Lincoln Univ, Fac Agr & Life Sci, Lincoln 7647, New Zealand
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Acidic soils; Aggregate size; Fungal denitrifying genes; Niche differentiation; N2O-reducing genes; SOIL BACTERIAL COMMUNITIES; MICROBIAL COMMUNITY; DENITRIFIER COMMUNITIES; FUNGAL DENITRIFICATION; AMMONIA OXIDIZERS; AGRICULTURAL SOILS; SIZE FRACTIONS; N2O EMISSION; RED SOIL; CARBON;
D O I
10.1016/j.apsoil.2021.104014
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The soil nitrogen (N) cycle is crucial to biogeochemical cycling, plant nutrient absorption, and greenhouse gas emissions and is primarily mediated by microorganisms. Although organic fertilization regulating aggregation has been well studied in various soils, how organic fertilization mediates microbial groups involved in soil N cycle in aggregates remained largely unclear. Therefore, the objective was to investigate the effect of 27 years of application of mineral and organic fertilizers (peanut straw, rice straw, radish, and pig manure) on the abundance of major microbial groups involved in the soil N cycle in four soil aggregate size classes. The results showed that organic fertilizers exerted significant impacts on the communities of microbes possessing N-cycling related genes, with pig manure having a more important effect than plant residues. However, aggregate size classes contributed more to the variation (20%) than organic fertilizers (12%). Organic fertilizer types did not impact the abundance of ammonia-oxidizing archaea (AOA) or ammonia-oxidizing bacteria (AOB). However, aggregate size strongly altered the abundance of AOA, but not AOB, with AOA being particularly abundant in <53 mu m aggregates. Organic fertilizers and aggregate size significantly influenced the abundance of the nirS gene rather than the nirK gene. There were greater amounts of nirS in the soils treated with rice straw and pig manure, primarily due to the higher soil organic matter content. As for fungal denitrification, there was a greater abundance of FnirK in microaggregates than in macroaggregates. Organic fertilizers and aggregate size significantly influenced the abundance of nosZ I and nosZ II genes, with aggregate size playing a more pronounced role. The abundance of nosZ I increased with increasing aggregate size while the abundance of nosZ II gene showed the opposite trends. This result revealed the clear niche differentiation of nosZ I and nosZ II genes in Ultisols, with nosZ I and nosZ II preferred to inhabit in macroaggregates and microaggregates, respectively. Overall, our results provide critical insights into the ecophysiology of major N-cycling-related genes in aggregates from an acidic Ultisol.
引用
收藏
页数:9
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