College of Resources and Environmental Sciences, National Academy of Agriculture Green Development, Key Laboratory of Plant-Soil Interactions, Ministry of Education, China Agricultural University, Beijing 100193, China.
College of Resources and Environmental Sciences, National Academy of Agriculture Green Development, Key Laboratory of Plant-Soil Interactions, Ministry of Education, China Agricultural University, Beijing 100193, China.
Sci Total Environ. 2021 Sep 1;785:147329. doi: 10.1016/j.scitotenv.2021.147329. Epub 2021 Apr 24.
The soil microbiome, existing as interconnected communities closely associated with soil aggregates, is the key driver in nutrient cycling. However, the underlying genomic information encoding the machinery of the soil microbiome involved in nutrient cycling at the soil aggregate scale is barely known. Here comparative metagenomics and genome binning were applied to investigate microbial functional profiles at the soil aggregate scale under different organic material amendments in a long-term field experiment. Soil samples were sieved into large macroaggregates (>2 mm), macroaggregates (0.25-2 mm) and microaggregates (<0.25 mm). Microbial taxonomic and functional alpha diversity were significantly correlated to soil NO and SOC. The highest abundance of nasB, nirK, and amoA genes, which are responsible for denitrification and ammonia oxidizers driving nitrification, was observed in microaggregates. Both manure and peat treatments significantly decreased the abundance of napA and nrfA that encode enzymes involved in dissimilatory nitrate reduction to ammonium (DNRA). As a biomarker for soil inorganic P solubilization, the relative abundance of gcd was significantly increased in macroaggregates and large macroaggregates. Three nearly complete genomes of Nitrososphaeraceae (AOA) and seven bacterial genomes were shown to harbor a series of genes involved in nitrification and P solubilization, respectively. Our study provides comprehensive insights into the microbial genetic potential for DNRA and P-solubilizing activity across different soil aggregate fractions and fertilization regimes.
土壤微生物组与土壤团聚体密切相关,作为相互关联的群落存在,是养分循环的关键驱动因素。然而,在土壤团聚体尺度上参与养分循环的土壤微生物组的潜在基因组信息编码机制还知之甚少。在这里,比较宏基因组学和基因组分类被应用于在长期田间试验中研究不同有机物质添加下土壤团聚体尺度上的微生物功能谱。将土壤样品筛分到大的团聚体(>2 毫米)、大团聚体(0.25-2 毫米)和微团聚体(<0.25 毫米)中。微生物分类和功能α多样性与土壤 NO 和 SOC 显著相关。负责反硝化和氨氧化驱动硝化作用的 nasB、nirK 和 amoA 基因的丰度最高,存在于微团聚体中。粪肥和泥炭处理均显著降低了 napA 和 nrfA 的丰度,这两个基因编码参与异化硝酸盐还原为铵(DNRA)的酶。作为土壤无机 P 溶解的生物标志物,gcd 的相对丰度在大团聚体和大团聚体中显著增加。三个几乎完整的硝化螺旋菌科(AOA)和七个细菌基因组显示出一系列参与硝化和 P 溶解的基因。我们的研究提供了全面的见解,了解了不同土壤团聚体分馏和施肥制度下 DNRA 和 P 溶解活性的微生物遗传潜力。