Pierangeli Gabrielle Maria Fonseca, Domingues Mercia Regina, de Jesus Tatiane Araujo, Coelho Lúcia Helena Gomes, Hanisch Werner Siegfried, Pompêo Marcelo Luiz Martins, Saia Flávia Talarico, Gregoracci Gustavo Bueno, Benassi Roseli Frederigi
Institute of Marine Sciences, Federal University of São Paulo, Santos, Brazil.
Center of Engineering, Modeling and Applied Social Sciences, Federal University of ABC, Santo André, Brazil.
Front Microbiol. 2021 Mar 17;12:647921. doi: 10.3389/fmicb.2021.647921. eCollection 2021.
Freshwater reservoirs emit greenhouse gases (GHGs) such as methane (CH) and carbon dioxide (CO), contributing to global warming, mainly when impacted by untreated sewage and other anthropogenic sources. These gases can be produced by microbial organic carbon decomposition, but little is known about the microbiota and its participation in GHG production and consumption in these environments. In this paper we analyzed the sediment microbiota of three eutrophic tropical urban freshwater reservoirs, in different seasons and evaluated the correlations between microorganisms and the atmospheric CH and CO flows, also correlating them to limnological variables. Our results showed that deeper water columns promote high methanogen abundance, with predominance of acetoclastic spp. and hydrogenotrophs spp. and spp. The aerobic methanotrophic community was affected by dissolved total carbon (DTC) and was dominated by spp. However, both relative abundance of the total methanogenic and aerobic methanotrophic communities in sediments were uncoupled to CH and CO flows. Network based approach showed that fermentative microbiota, including spp. and spp., which produces substrates for methanogenesis, influence CH flows and was favored by anthropogenic pollution, such as untreated sewage loads. Additionally, less polluted conditions favored probable anaerobic methanotrophs such as Bathyarchaeota, , , and , which promoted lower gaseous flows, confirming the importance of sanitation improvement to reduce these flows in tropical urban freshwater reservoirs and their local and global warming impact.
淡水水库会排放甲烷(CH₄)和二氧化碳(CO₂)等温室气体,这主要是在受到未经处理的污水和其他人为来源影响时,会加剧全球变暖。这些气体可由微生物对有机碳的分解产生,但对于这些环境中的微生物群及其在温室气体产生和消耗中的作用却知之甚少。在本文中,我们分析了三个富营养化热带城市淡水水库在不同季节的沉积物微生物群,并评估了微生物与大气中CH₄和CO₂通量之间的相关性,还将它们与湖沼学变量相关联。我们的结果表明,较深的水柱会促进产甲烷菌的高丰度,以乙酸营养型菌属和氢营养型菌属为主。需氧甲烷氧化菌群落受溶解总碳(DTC)的影响,以某菌属为主。然而,沉积物中产甲烷菌和需氧甲烷氧化菌群落的相对丰度均与CH₄和CO₂通量无关。基于网络的方法表明,包括某菌属和某菌属在内的发酵微生物群会产生甲烷生成的底物,影响CH₄通量,且受到诸如未经处理的污水负荷等人为污染的青睐。此外,污染较轻的条件有利于可能的厌氧甲烷氧化菌,如深古菌门、某菌属、某菌属和某菌属,它们会促进较低的气体通量,这证实了改善卫生条件对于减少热带城市淡水水库中的这些通量及其对当地和全球变暖影响的重要性。