Yang Chao, Sun Juan
Grassland Agri-Husbandry Research Center, College of Grassland Science, Qingdao Agricultural University, Qingdao, China.
Front Microbiol. 2020 Dec 23;11:594284. doi: 10.3389/fmicb.2020.594284. eCollection 2020.
High soil salinity is the main factor that limits soil microbial activity in the Yellow River Delta (YRD); however, its effects on fungal community and ecological function are unknown. Here, we comparatively investigated the diversity and structures of soil fungal communities targeting the internally transcribed fungal spacer gene using Illumina MiSeq sequencing methods under a salt gradient with five levels, namely, Low: low-salinity soil, Medium: medium-salinity soil, High: high-salinity soil, Extreme: extreme-salinity soil, and a non-salted site as the control (Non-saline). The results show that bulk density (BD) values significantly increased ( < 0.05), while significantly lower values of soil total carbon (TC), total nitrogen (TN), and fungal Shannon and Chao indexes were observed as the salinization gradient increased ( < 0.05). The relatively high levels of the families and distinguished two of the clusters, indicating two enterotypes of low (Non-saline and Low) and high (Medium, High, and Extreme) salinity soils, respectively. The family was most abundant in the networks, and the positive correlations were more pronounced than negative correlations; however, was the family most negatively correlated with others based on the network analysis. At the ecological function level, plant saprotrophs and litter saprotroph were significantly less abundant in extremely saline soil than non-saline soil. The change in soil properties (TC, TN, and BD) caused by soil salinization [salt and electrical conductivity (EC)] regulated the diversity of soil fungal communities, and ecological function, as indicated by Pearson correlation analyses. We suggest further investigation into the ecological functions of soil microorganisms in the extremely saline-alkaline soils of the YRD.
高土壤盐分是限制黄河三角洲土壤微生物活性的主要因素;然而,其对真菌群落和生态功能的影响尚不清楚。在此,我们采用Illumina MiSeq测序方法,以内部转录间隔区基因作为目标,在五个盐分梯度水平下(即低:低盐度土壤、中:中盐度土壤、高:高盐度土壤、极端:极端盐度土壤,以及一个非盐渍位点作为对照(非盐渍)),比较研究了土壤真菌群落的多样性和结构。结果表明,随着盐渍化梯度增加,土壤容重(BD)值显著升高(P<0.05),而土壤总碳(TC)、总氮(TN)以及真菌香农指数和Chao指数显著降低(P<0.05)。相对较高丰度的[某两个科名未给出]科区分出了两个聚类,分别表明低盐度(非盐渍和低)和高盐度(中、高和极端)土壤的两种肠型。[某科名未给出]科在网络中最为丰富,正相关比负相关更显著;然而,根据网络分析,[某科名未给出]科与其他科的负相关性最强。在生态功能水平上,极端盐渍土壤中植物腐生菌和凋落物腐生菌的丰度显著低于非盐渍土壤。Pearson相关性分析表明,土壤盐渍化[盐分和电导率(EC)]引起的土壤性质(TC、TN和BD)变化调节了土壤真菌群落的多样性和生态功能。我们建议进一步研究黄河三角洲极端盐碱土壤中土壤微生物的生态功能。