Cerbin Slawek, Pérez Germán, Rybak Michał, Wejnerowski Łukasz, Konowalczyk Adam, Helmsing Nico, Naus-Wiezer Suzanne, Meima-Franke Marion, Pytlak Łukasz, Raaijmakers Ciska, Nowak Witold, Bodelier Paul L E
Department of Hydrobiology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland.
Department of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands.
Front Microbiol. 2022 Apr 1;13:837198. doi: 10.3389/fmicb.2022.837198. eCollection 2022.
Methane, a potent greenhouse gas produced in freshwater ecosystems, can be used by methane-oxidizing bacteria (MOB) and can therefore subsidize the pelagic food web with energy and carbon. Consortia of MOB and photoautotrophs have been described in aquatic ecosystems and MOB can benefit from photoautotrophs which produce oxygen, thereby enhancing CH oxidation. Methane oxidation can account for accumulation of inorganic carbon (i.e., CO) and the release of exometabolites that may both be important factors influencing the structure of phytoplankton communities. The consortium of MOB and phototroph has been mainly studied for methane-removing biotechnologies, but there is still little information on the role of these interactions in freshwater ecosystems especially in the context of cyanobacterial growth and bloom development. We hypothesized that MOB could be an alternative C source to support cyanobacterial growth in freshwater systems. We detected low δC values in cyanobacterial blooms (the lowest detected value -59.97‰ for ) what could be the result of the use of methane-derived carbon by cyanobacteria and/or MOB attached to their cells. We further proved the presence of metabolically active MOB on cyanobacterial filaments using the fluorescein isothiocyanate (FITC) based activity assay. The PCR results also proved the presence of the gene in several non-axenic cultures of cyanobacteria. Finally, experiments comprising the co-culture of the cyanobacterium with the methanotroph proved that cyanobacterial growth was significantly improved in the presence of MOB, presumably through utilizing CO released by MOB. On the other hand, C-CH labeled incubations showed the uptake and assimilation of MOB-derived metabolites by the cyanobacterium. We also observed a higher growth of MOB in the presence of cyanobacteria under a higher irradiance regime, then when grown alone, underpinning the bidirectional influence with as of yet unknown environmental consequences.
甲烷是淡水生态系统中产生的一种强效温室气体,甲烷氧化细菌(MOB)可以利用它,因此能够为远洋食物网提供能量和碳。在水生生态系统中已发现MOB与光合自养生物的聚生体,MOB可以从产生氧气的光合自养生物中受益,从而增强CH氧化。甲烷氧化可导致无机碳(即CO)的积累以及胞外代谢产物的释放,这两者可能都是影响浮游植物群落结构的重要因素。MOB与光养生物的聚生体主要是针对甲烷去除生物技术进行研究的,但关于这些相互作用在淡水生态系统中的作用,尤其是在蓝藻生长和水华发展背景下的作用,目前仍知之甚少。我们假设MOB可能是支持淡水系统中蓝藻生长的一种替代碳源。我们在蓝藻水华中检测到较低的δC值(检测到的最低值为-59.97‰),这可能是蓝藻和/或附着在其细胞上的MOB利用甲烷衍生碳的结果。我们使用基于异硫氰酸荧光素(FITC)的活性测定法进一步证明了蓝藻丝状体上存在代谢活跃的MOB。PCR结果也证明了在几种非无菌培养的蓝藻中存在该基因。最后,将蓝藻与甲烷营养菌进行共培养实验证明,在有MOB存在的情况下,蓝藻生长显著改善,大概是通过利用MOB释放的CO。另一方面,用C-CH标记的培养实验表明,蓝藻吸收并同化了MOB衍生代谢产物。我们还观察到,在较高辐照条件下,与单独生长相比,有蓝藻存在时MOB的生长更高,这表明两者之间存在双向影响,但其对环境的影响尚不清楚。