College of Life Sciences, University of Chinese Academy of Sciences, Beijing 100049, China; Environmental Futures Research Institute, School of Environment and Science, Griffith University, Brisbane 4111, Australia.
Nanjing Normal University, Nanjing 210097, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China.
Sci Total Environ. 2018 Oct 15;639:997-1006. doi: 10.1016/j.scitotenv.2018.05.238. Epub 2018 May 26.
Biological nitrogen fixation, conducted by soil diazotrophs, is the primary nitrogen source for natural grasslands. However, the diazotrophs in grassland soils are still far from fully investigated. Particularly, their regional-scale distribution patterns have never been systematically examined. Here, soils (0-5 cm) were sampled from 54 grasslands on the Tibetan Plateau to examine the diazotroph abundance, diversity, and community composition, as well as their distribution patterns and driving factors. The diazotroph abundance was expressed as nifH gene copies, measured using real-time PCR. The diversity and community composition of diazotrophs were analyzed through MiSeq sequencing of nifH genes. The results showed that Cyanobacteria (47.94%) and Proteobacteria (45.20%) dominated the soil diazotroph communities. Most Cyanobacteria were classified as Nostocales which are main components of biological crusts. Rhizobiales, most of which were identified as potential symbiotic diazotrophs, were also abundant in approximately half of the soil samples. The soil diazotroph abundance, diversity, and community composition followed the distribution patterns in line with mean annual precipitation. Moreover, they also showed significant correlations with prokaryotic abundance, plant biomass, vegetation cover, soil pH values, and soil nutrient contents. Among these environmental factors, the soil moisture, organic carbon, available phosphorus, and inorganic nitrogen contents could be the main drivers of diazotroph distribution due to their strong correlations with diazotroph indices. These findings suggest that autotrophic and symbiotic diazotrophs are the predominant nitrogen fixers in Tibetan grassland soils, and highlight the key roles of water and nutrient availability in determining the soil diazotroph distribution on the Tibetan Plateau.
生物固氮作用由土壤固氮菌进行,是天然草原的主要氮源。然而,草原土壤中的固氮菌仍远未被充分研究。特别是,它们的区域尺度分布模式从未被系统地研究过。在这里,从青藏高原的 54 个草原采集了土壤(0-5cm),以研究固氮菌的丰度、多样性和群落组成,以及它们的分布模式和驱动因素。固氮菌的丰度用实时 PCR 测量的 nifH 基因拷贝数来表示。通过 nifH 基因的 MiSeq 测序分析了固氮菌的多样性和群落组成。结果表明,蓝细菌(47.94%)和变形菌(45.20%)是土壤固氮菌群落的主要组成部分。大多数蓝细菌被归类为生物结皮的主要组成部分 Nostocales。根瘤菌目,其中大部分被鉴定为潜在的共生固氮菌,也在大约一半的土壤样本中丰富。土壤固氮菌的丰度、多样性和群落组成与年平均降水量的分布模式一致。此外,它们还与原核生物丰度、植物生物量、植被覆盖、土壤 pH 值和土壤养分含量呈显著相关。在这些环境因素中,由于与固氮菌指数密切相关,土壤水分、有机碳、有效磷和无机氮含量可能是固氮菌分布的主要驱动因素。这些发现表明,自养和共生固氮菌是青藏高原草原土壤中主要的固氮生物,并强调了水和养分供应在决定青藏高原土壤固氮菌分布方面的关键作用。