Key Laboratory for Green Chemical Process of Ministry of Education, School of Environmental Ecology and Biological Engineering, Wuhan Institute of Technology, Wuhan, People's Republic of China.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciencesgrid.162107.3, Wuhan, People's Republic of China.
mSystems. 2022 Aug 30;7(4):e0033522. doi: 10.1128/msystems.00335-22. Epub 2022 Jul 12.
The compositional and physiological responses of autotrophic microbiotas to salinity in lakes remain unclear. In this study, the community composition and carbon fixation pathways of autotrophic microorganisms in lacustrine sediments with a salinity gradient (82.6 g/L to 0.54 g/L) were investigated by using metagenomic analysis. A total of 117 metagenome-assembled genomes (MAGs) with carbon fixation potentially belonging to 20 phyla were obtained. The abundance of these potential autotrophs increased significantly with decreasing salinity, and the variation of sediment autotrophic microbial communities was mainly affected by salinity, pH, and total organic carbon. Notably, along the decreasing salinity gradient, the dominant lineage shifted from to . Meanwhile, the dominant carbon fixation pathway shifted from the Wood-Lungdahl pathway to the less-energy-efficient Calvin-Benson-Bassham cycle, with glycolysis shifting from the Embden-Meyerhof-Parnas pathway to the less-exergonic Entner-Doudoroff pathway. These results suggest that the physiological efficiency of autotrophic microorganisms decreased when the environmental salinity became lower. Metabolic inference of these MAGs revealed that carbon fixation may be coupled to the oxidation of reduced sulfur compounds and ferrous iron, dissimilatory nitrate reduction at low salinity, and dissimilatory sulfate reduction in hypersaline sediments. These results extend our understanding of metabolic versatility and niche diversity of autotrophic microorganisms in saline environments and shed light on the response of autotrophic microbiomes to salinity. These findings are of great significance for understanding the impact of desalination caused by climate warming on the carbon cycle of saline lake ecosystems. The Qinghai-Tibetan lakes are experiencing water increase and salinity decrease due to climate warming. However, little is known about how the salinity decrease will affect the composition of autotrophic microbial populations and their carbon fixation pathways. In this study, we used genome-resolved metagenomics to interpret the dynamic changes in the autotrophic microbial community and metabolic pathways along a salinity gradient. The results showed that desalination drove the shift of the dominant microbial lineage from to , enriched autotrophs with lower physiological efficiency pathways, and enhanced coupling between the carbon cycle and other element cycles. These results can predict the future response of microbial communities to lake desalination and improve our understanding of the effect of climate warming on the carbon cycle in saline aquatic ecosystems.
湖泊中自养微生物群落的组成和生理响应仍不清楚。本研究通过宏基因组分析,研究了盐度梯度(82.6 g/L 至 0.54 g/L)下湖泊沉积物中自养微生物群落的组成和碳固定途径。共获得了 117 个具有潜在碳固定功能的宏基因组组装基因组(MAG),这些 MAG 可能属于 20 个门。这些潜在自养生物的丰度随着盐度的降低而显著增加,沉积物自养微生物群落的变化主要受盐度、pH 值和总有机碳的影响。值得注意的是,随着盐度梯度的降低,优势谱系从 转变为 。同时,主导的碳固定途径从 Wood-Lungdahl 途径转变为能量效率较低的 Calvin-Benson-Bassham 循环,糖酵解从 Embden-Meyerhof-Parnas 途径转变为能量更低的 Entner-Doudoroff 途径。这些结果表明,当环境盐度变低时,自养微生物的生理效率降低。对这些 MAG 的代谢推断表明,碳固定可能与还原态硫化合物和亚铁的氧化、低盐下的硝酸盐异化还原以及过盐沉积物中的硫酸盐异化还原相耦合。这些结果扩展了我们对盐环境中自养微生物代谢多功能性和生态位多样性的理解,并揭示了自养微生物组对盐度的响应。这些发现对于理解气候变暖引起的海水淡化对盐湖生态系统碳循环的影响具有重要意义。青藏高原湖泊由于气候变暖而出现水位上升和盐度下降的情况。然而,对于盐度下降将如何影响自养微生物种群的组成及其碳固定途径,人们知之甚少。在这项研究中,我们使用基于基因组的宏基因组学来解释沿盐度梯度自养微生物群落和代谢途径的动态变化。结果表明,淡化作用促使优势微生物谱系从 转变为 ,富集了生理效率较低的自养生物,并增强了碳循环与其他元素循环之间的耦合。这些结果可以预测未来微生物群落对湖泊淡化的反应,提高我们对气候变暖对盐水水生生态系统碳循环影响的理解。