Xu Qian, Du Zhiheng, Wang Lei, Xue Kai, Wei Zhiqiang, Zhang Gaosen, Liu Keshao, Lin Jiahui, Lin Penglin, Chen Tuo, Xiao Cunde
State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Microorganisms. 2022 Aug 10;10(8):1620. doi: 10.3390/microorganisms10081620.
One of the most significant environmental changes across the Tibetan Plateau (TP) is the rapid lake expansion. The expansion of thermokarst lakes affects the global biogeochemical cycles and local climate regulation by rising levels, expanding area, and increasing water volumes. Meanwhile, microbial activity contributes greatly to the biogeochemical cycle of carbon in the thermokarst lakes, including organic matter decomposition, soil formation, and mineralization. However, the impact of lake expansion on distribution patterns of microbial communities and methane cycling, especially those of water and sediment under ice, remain unknown. This hinders our ability to assess the true impact of lake expansion on ecosystem services and our ability to accurately investigate greenhouse gas emissions and consumption in thermokarst lakes. Here, we explored the patterns of microorganisms and methane cycling by investigating sediment and water samples at an oriented direction of expansion occurred from four points under ice of a mature-developed thermokarst lake on TP. In addition, the methane concentration of each water layer was examined. Microbial diversity and network complexity were different in our shallow points (MS, SH) and deep points (CE, SH). There are differences of microbial community composition among four points, resulting in the decreased relative abundances of dominant phyla, such as Firmicutes in sediment, Proteobacteria in water, Thermoplasmatota in sediment and water, and increased relative abundance of Actinobacteriota with MS and SH points. Microbial community composition involved in methane cycling also shifted, such as increases in USCγ, and , with higher relative abundance consistent with low dissolved methane concentration in MS and SH points. There was a strong correlation between changes in microbiota characteristics and changes in water and sediment environmental factors. Together, these results show that lake expansion has an important impact on microbial diversity and methane cycling.
青藏高原(TP)最显著的环境变化之一是湖泊迅速扩张。热喀斯特湖的扩张通过水位上升、面积扩大和水量增加影响全球生物地球化学循环和局部气候调节。与此同时,微生物活动对热喀斯特湖碳的生物地球化学循环有很大贡献,包括有机物分解、土壤形成和矿化。然而,湖泊扩张对微生物群落分布模式和甲烷循环的影响,尤其是冰下水体和沉积物中的影响,仍然未知。这阻碍了我们评估湖泊扩张对生态系统服务的真正影响,以及准确调查热喀斯特湖温室气体排放和消耗的能力。在这里,我们通过调查TP上一个成熟发育的热喀斯特湖冰下四个点在扩张方向上的沉积物和水样,探索了微生物和甲烷循环的模式。此外,还检测了每个水层的甲烷浓度。我们的浅点(MS,SH)和深点(CE,SH)的微生物多样性和网络复杂性不同。四个点的微生物群落组成存在差异,导致优势菌门的相对丰度降低,如沉积物中的厚壁菌门、水体中的变形菌门、沉积物和水体中的热原体门,以及MS和SH点放线菌门的相对丰度增加。参与甲烷循环的微生物群落组成也发生了变化,如USCγ等的增加,且相对丰度较高,这与MS和SH点较低的溶解甲烷浓度一致。微生物群特征变化与水和沉积物环境因素变化之间存在很强的相关性。总之,这些结果表明湖泊扩张对微生物多样性和甲烷循环有重要影响。