Zhang Ni, Chen Kelong, Chen Ji, Ji Wei, Yang Ziwei, Chen Zhirong
Qinghai Province Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining 810008, China.
Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), Qinghai Normal University, Xining 810008, China.
Biology (Basel). 2024 Aug 7;13(8):596. doi: 10.3390/biology13080596.
The nitrogen cycling process in alpine wetlands is profoundly affected by precipitation changes, yet the dynamic response mechanism of denitrifiers to long-term precipitation shifts in the alpine wetland of the Qinghai-Tibet Plateau remains enigmatic. Utilizing high-throughput sequencing analysis of nirS-type functional genes, this study delved into the dynamic response mechanism of nirS-type denitrifiers to precipitation changes in the alpine wetland of Qinghai Lake. The findings revealed that nirS-type denitrifiers in the alpine wetland of Qinghai Lake were primarily Proteobacteria, and Alpha diversity exhibited a negative correlation with the precipitation gradient, with deterministic processes predominating in the community assembly of denitrifying microbes. A 50% increase in rainfall shifted the community assembly process of denitrifiers from deterministic to stochastic. Dominant microflora at the genus level responded significantly to precipitation changes, with aerobic bacteria comprising the majority of differentially abundant taxa (55.56%). As precipitation increased, the complexity of the microbial interaction network decreased, and a 25% reduction in precipitation notably elevated the relative abundance of three key functional groups: chemoheterotrophic, aerobic chemoheterotrophic, and nitrogen fixation. Precipitation notably emerged as the primary regulator of nirS-type denitrifiers in the alpine wetland of Qinghai Lake, accounting for 51% of the variation in community composition. In summary, this study offers a fresh perspective for investigating the ecological processes of nitrogen cycling in alpine ecosystems by examining the diversity and community composition of nirS-type denitrifiers in response to precipitation changes.
高山湿地的氮循环过程深受降水变化的影响,然而青藏高原高山湿地中反硝化细菌对长期降水变化的动态响应机制仍不明确。本研究利用nirS型功能基因的高通量测序分析,深入探究了青海湖高山湿地中nirS型反硝化细菌对降水变化的动态响应机制。研究结果表明,青海湖高山湿地中的nirS型反硝化细菌主要为变形菌门,α多样性与降水梯度呈负相关,反硝化微生物群落组装过程中确定性过程占主导地位。降雨量增加50%使反硝化细菌的群落组装过程从确定性转变为随机性。属水平上的优势微生物群落对降水变化有显著响应,需氧细菌占差异丰富类群的大部分(55.56%)。随着降水量增加,微生物相互作用网络的复杂性降低,降水量减少25%显著提高了三个关键功能组的相对丰度:化学异养菌、需氧化学异养菌和固氮菌。降水量显著成为青海湖高山湿地nirS型反硝化细菌的主要调节因子,解释了群落组成变异的51%。总之,本研究通过研究nirS型反硝化细菌的多样性和群落组成对降水变化的响应,为调查高山生态系统中氮循环的生态过程提供了新的视角。