School of Space and Environment, Beihang University, Beijing, 100191, China.
School of Space and Environment, Beihang University, Beijing, 100191, China; Advanced Innovation Center for Big Data-Based Precision Medicine, Beihang University, Beijing, 100191, China.
Environ Res. 2022 Nov;214(Pt 4):114109. doi: 10.1016/j.envres.2022.114109. Epub 2022 Aug 15.
The migration of organic matter in salinized lakes was critical in maintaining ecological balance and material circulation process of inland shallow lakes. To clarify the ecological and microbial mechanism of material transport and transformation, the microbial community structure and the characteristics of dissolved organic matter (DOM) in the sediment of Daihai Lake, a typical saline lake at the Yellow River Basin, were explored with three-dimensional excitation and emission matrix fluorescence (3DEEM), parallel factor analysis (PARAFAC) and 16 S rRNA techniques. The correlation between environmental factors, DOM composition and the bacterial community structure were also studied for identifying the key factors of community formation. DOM in the lake demonstrated both terrigenous and endogenous characteristics. Protein-like materials accounted for 74% of the total fluorescence intensity in the sediment, where 1127 species, 671 genera, 468 families, 157 classes, 317 orders, 59 phyla of microorganisms were detected. Among the top 10 abundant taxa of each level, Firmicutes, Actinobacterota, Acidimicrobiia and Alphaproteobacteria had the greatest influence on the composition and structure of DOM (|R| > 0.7, p < 0.01). Microbial metabolism was a key process of transforming sediment organic matter from terrestrial humic-like to protein-like matter, accounting for 81% of total fluorescence signal in saline lake samples, while salinity, temperature, dissolved oxygen and electrical conductivity also had significant impacts during the process (|R|>0.7, p < 0.05). The research provides fundamental data and enlightenment for the improvement of the saline inland lake environment.
盐湖中有机质的迁移对于维持生态平衡和内陆浅水湖泊物质循环过程至关重要。为了阐明物质输运和转化的生态和微生物机制,本研究采用三维激发发射矩阵荧光(3DEEM)、平行因子分析(PARAFAC)和 16S rRNA 技术,探讨了黄河流域典型盐湖岱海沉积物中微生物群落结构和溶解有机质(DOM)特征。还研究了环境因子、DOM 组成与细菌群落结构之间的相关性,以确定群落形成的关键因素。该湖的 DOM 具有生源和内源特征。沉积物中总荧光强度的 74%由类蛋白物质组成,共检测到 1127 种、671 属、468 科、157 纲、317 目、59 门微生物。在每个水平的前 10 个丰度类群中,厚壁菌门、放线菌门、酸杆菌门和α变形菌门对 DOM 的组成和结构影响最大(|R|>0.7,p<0.01)。微生物代谢是将沉积物有机质从陆生腐殖质样转化为类蛋白样物质的关键过程,占咸水湖样品总荧光信号的 81%,而盐度、温度、溶解氧和电导率在该过程中也有显著影响(|R|>0.7,p<0.05)。本研究为改善内陆咸水湖泊环境提供了基础数据和启示。