Methane-Derived Carbon as a Driver for Cyanobacterial Growth

Frontiers in Microbiology

Suzanne Naus-Wiezer¹  Nico Helmsing¹  Adam Konowalczyk²  Łukasz Wejnerowski²  Slawek Cerbin²  Germán Pérez³  Paul L. E. Bodelier³  Marion Meima-Franke³  Ciska Raaijmakers⁴  Michał Rybak⁵  Witold Nowak⁶  Łukasz Pytlak⁷ 

[1] Department of Aquatic Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands;Department of Hydrobiology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland;Department of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands;Department of Terrestrial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands;Department of Water Protection, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland;Molecular Biology Techniques Laboratory, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland;Montanuniversität Leoben, Applied Geosciences and Geophysics, Leoben, Austria;

关键词: methane;    methane oxidation;    isotopes;    co-culture;    lakes;    greenhouse gases;   

DOI  :  10.3389/fmicb.2022.837198

来源: DOAJ

【 摘 要 】

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 CH4 oxidation. Methane oxidation can account for accumulation of inorganic carbon (i.e., CO2) 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 δ13C values in cyanobacterial blooms (the lowest detected value −59.97‰ for Planktothrix rubescens) 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 pmoA gene in several non-axenic cultures of cyanobacteria. Finally, experiments comprising the co-culture of the cyanobacterium Aphanizomenon gracile with the methanotroph Methylosinus sporium proved that cyanobacterial growth was significantly improved in the presence of MOB, presumably through utilizing CO2 released by MOB. On the other hand, 13C-CH4 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.

【 授权许可】

Unknown