Schreckinger José, Mutz Michael, Mendoza-Lera Clara, Frossard Aline
Department of Freshwater Conservation, Brandenburg University of Technology Cottbus-Senftenberg, Bad Saarow, Germany.
Institute of Environmental Sciences, Koblenz-Landau University, Landau, Germany.
Front Microbiol. 2021 Jun 14;12:676615. doi: 10.3389/fmicb.2021.676615. eCollection 2021.
Combined effects of climate change and increasing anthropogenic water demand have increased and extended dry period occurrences in rivers worldwide. Riverbed drying can significantly affect sediment microorganisms, crucial drivers of biogeochemical processes in lotic systems. In this study, we evaluated how sediment bacterial and fungal community structure and composition (based on 16S rRNA gene and ITS metabarcoding) and microbial functions (community respiration and extracellular enzymatic activities) respond to different riverbed drying intensities over 90 days. Riverbed sediment collected in a flowing reach of the Spree river in northeastern Germany was dried under different rates in outdoor mesocosms during the summer months of 2018. Our results demonstrate that drying attributes (duration and intensity) and sediment organic matter (OM) content play a crucial role in sediment microbial community assembly and functioning throughout drying. Milder drying surprisingly triggered a more rapid and drastic change in the microbial community composition and diversity. After 90 days of drying, Bacilli (Firmicutes) became the dominant bacterial class in most treatments, except in sediments with low OM content under the most severe drying treatment. Fungal amplicon sequence variants (ASVs) from Dothideomycetes (Ascomycota) had by far the highest relative abundance in all our treatments at the end of the drying experiment, making up 65.1% to 94.0% of the fungal reads. CO fluxes, a proxy for sediment community respiration, were rapidly and strongly affected by drying in all treatments. Our results imply that even short riverbed drying periods are likely to have significant consequences for the biogeochemical dynamics in recently formed non-perennial temperate rivers.
气候变化和人为需水量增加的综合影响,已导致全球河流干旱期增多且持续时间延长。河床干涸会显著影响沉积物中的微生物,而这些微生物是流水系统中生物地球化学过程的关键驱动因素。在本研究中,我们评估了沉积物细菌和真菌群落结构与组成(基于16S rRNA基因和ITS宏条形码)以及微生物功能(群落呼吸和胞外酶活性)在90天内对不同河床干涸强度的响应。2018年夏季,在德国东北部施普雷河的一段水流区域采集的河床沉积物,在室外中型生态系统中以不同速率进行干燥处理。我们的研究结果表明,干燥属性(持续时间和强度)以及沉积物有机质(OM)含量在整个干燥过程中,对沉积物微生物群落的组装和功能起着至关重要的作用。令人惊讶的是,较温和的干燥引发了微生物群落组成和多样性更快、更剧烈的变化。干燥90天后,芽孢杆菌(厚壁菌门)在大多数处理中成为优势细菌类群,但在最严重干燥处理下OM含量低的沉积物中除外。在干燥实验结束时,座囊菌纲(子囊菌门)的真菌扩增子序列变体(ASVs)在所有处理中的相对丰度最高,占真菌读数的65.1%至94.0%。作为沉积物群落呼吸指标的CO通量,在所有处理中均受到干燥的快速且强烈影响。我们的研究结果表明,即使是短暂的河床干涸期,也可能对新形成的非常年性温带河流中的生物地球化学动态产生重大影响。