The National Key Laboratory of Water Disaster Prevention, Hohai University, Nanjing, 210024, China.
College of Hydrology and Water Resources, Hohai University, Nanjing, 210024, China.
Microbiome. 2023 Aug 26;11(1):191. doi: 10.1186/s40168-023-01612-z.
Freshwater sediment microbes are crucial decomposers that play a key role in regulating biogeochemical cycles and greenhouse gas emissions. They often exhibit a highly ordered structure along depth profiles. This stratification not only reflects redox effects but also provides valuable insights into historical transitions, as sediments serve as important archives for tracing environmental history. The Anthropocene, a candidate geological epoch, has recently garnered significant attention. However, the human impact on sediment zonation under the cover of natural redox niches remains poorly understood. Dam construction stands as one of the most far-reaching anthropogenic modifications of aquatic ecosystems. Here we attempted to identify the ecological imprint of damming on freshwater sediment microbiome.
We conducted a year-round survey on the sediment profiles of Lake Chaohu, a large shallow lake in China. Through depth-discrete shotgun metagenomics, metataxonomics, and geophysiochemical analyses, we unveiled a unique prokaryotic hierarchy shaped by the interplay of redox regime and historical damming (labeled by the Cs peak in AD 1963). Dam-induced initial differentiation was further amplified by nitrogen and methane metabolism, forming an abrupt transition governing nitrate-methane metabolic interaction and gaseous methane sequestration depth. Using a random forest algorithm, we identified damming-sensitive taxa that possess distinctive metabolic strategies, including energy-saving mechanisms, unique motility behavior, and deep-environment preferences. Moreover, null model analysis showed that damming altered microbial community assembly, from a selection-oriented deterministic process above to a more stochastic, dispersal-limited one below. Temporal investigation unveiled the rapid transition zone as an ecotone, characterized by high species richness, low community stability, and emergent stochasticity. Path analysis revealed the observed emergent stochasticity primarily came from the high metabolic flexibility, which potentially contributed to both ecological and statistical neutralities.
We delineate a picture in which dam-induced modifications in nutrient availability and sedimentation rates impact microbial metabolic activities and generate great changes in the community structure, assembly, and stability of the freshwater sediment microbiome. These findings reflect profound ecological and biogeochemical ramifications of human-Earth system interactions and help re-examine the mainstream views on the formation of sediment microbial stratification. Video Abstract.
淡水沉积物微生物是至关重要的分解者,在调节生物地球化学循环和温室气体排放方面发挥着关键作用。它们通常沿着深度剖面呈现出高度有序的结构。这种分层不仅反映了氧化还原效应,还为历史变迁提供了有价值的见解,因为沉积物是追踪环境历史的重要档案。人类世是候选地质年代,最近受到了广泛关注。然而,在自然氧化还原小生境的掩盖下,人类对沉积物分带的影响仍知之甚少。水坝建设是对水生生态系统影响最深远的人为改造之一。在这里,我们试图确定水坝对淡水沉积物微生物组的生态影响。
我们对中国大型浅水湖巢湖的沉积物剖面进行了全年调查。通过深度离散的 shotgun 宏基因组学、宏分类学和地球物理化学分析,我们揭示了一种由氧化还原状态和历史筑坝(以公元 1963 年的 Cs 峰标记)相互作用塑造的独特的原核层次结构。筑坝引起的初始分化进一步被氮和甲烷代谢放大,形成了一个突然的过渡,控制着硝酸盐-甲烷代谢相互作用和气态甲烷封存深度。使用随机森林算法,我们确定了具有独特代谢策略的筑坝敏感类群,包括节能机制、独特的运动行为和深环境偏好。此外,零模型分析表明,筑坝改变了微生物群落组装,从以选择为导向的确定性过程转变为更随机的、扩散受限的过程。时间调查揭示了快速过渡带作为生态过渡带的特征,具有高物种丰富度、低群落稳定性和新兴随机性。路径分析表明,观察到的新兴随机性主要来自于高代谢灵活性,这可能为生态和统计中立性都做出了贡献。
我们描绘了一幅图景,即筑坝引起的养分可用性和沉积速率的改变影响微生物的代谢活动,并导致淡水沉积物微生物组的群落结构、组装和稳定性发生巨大变化。这些发现反映了人类-地球系统相互作用的深刻生态和生物地球化学后果,并有助于重新审视关于沉积物微生物分层形成的主流观点。视频摘要。