Li Xin, Cui Yuanquan, Ma Dalong, Song Dandan, Liu Lin
College of Geographical Sciences Harbin Normal University Harbin China.
Personnel department Harbin Normal University Harbin China.
Ecol Evol. 2022 Jul 11;12(7):e9106. doi: 10.1002/ece3.9106. eCollection 2022 Jul.
Soil microorganisms are crucial contributors to the function of permafrost ecosystems, as well as the regulation of biogeochemical cycles. However, little is known about the distribution patterns and drivers of high-latitude permafrost microbial communities subject to climate change and human activities. In this study, the vertical distribution patterns of soil bacterial communities in the Greater Khingan Mountain permafrost region were systematically analyzed via Illumina Miseq high-throughput sequencing. Bacterial diversity in the active layer was significantly higher than in the permafrost layer. Principal coordinate analysis (PCoA) indicated that the bacterial community structure in the active layer and the permafrost layer was completely separated. Permutational multivariate analysis of variance (PERMANOVA) detected statistically significant differentiation across the different depths. The relative abundance of the dominant phyla Chloroflexi (17.92%-52.79%) and Actinobacteria (6.34%-34.52%) was significantly higher in the permafrost layer than in the active layer, whereas that of Acidobacteria (4.98%-38.82%) exhibited the opposite trend, and the abundance of Proteobacteria (2.49%-22.51%) generally decreased with depth. More importantly, the abundance of bacteria linked to human infectious diseases was significantly higher in the permafrost layer according to Tax4Fun prediction analysis. Redundancy analysis (RDA) showed that ammonium nitrogen (NH -N), total organic carbon (TOC), and total phosphorus (TP) were major factors affecting the bacterial community composition. Collectively, our findings provide insights into the soil bacterial vertical distribution patterns and major environmental drivers in high-latitude permafrost regions, which is key to grasping the response of cold region ecosystem processes to global climate changes.
土壤微生物是多年冻土生态系统功能以及生物地球化学循环调节的关键贡献者。然而,对于受气候变化和人类活动影响的高纬度多年冻土微生物群落的分布模式和驱动因素,我们知之甚少。在本研究中,通过Illumina Miseq高通量测序系统分析了大兴安岭多年冻土区土壤细菌群落的垂直分布模式。活动层中的细菌多样性显著高于多年冻土层。主坐标分析(PCoA)表明,活动层和多年冻土层中的细菌群落结构完全分离。置换多元方差分析(PERMANOVA)检测到不同深度之间存在统计学上的显著差异。优势菌门绿弯菌门(17.92%-52.79%)和放线菌门(6.34%-34.52%)在多年冻土层中的相对丰度显著高于活动层,而酸杆菌门(4.98%-38.82%)则呈现相反趋势,变形菌门(2.49%-22.51%)的丰度一般随深度降低。更重要的是,根据Tax4Fun预测分析,与人类传染病相关的细菌在多年冻土层中的丰度显著更高。冗余分析(RDA)表明,铵态氮(NH₄⁺-N)、总有机碳(TOC)和总磷(TP)是影响细菌群落组成的主要因素。总体而言,我们的研究结果为高纬度多年冻土区土壤细菌垂直分布模式和主要环境驱动因素提供了见解,这对于掌握寒冷地区生态系统过程对全球气候变化的响应至关重要。