bioRxiv Science⌕ Search

Biology subjects

Kawaichi, S.

Publications and source records attributed to Kawaichi, S..

3 recordsLinked to original sources

Extracellular RNA drives Electromethanogenesis in a Methanogenic Archaeon

Methanogenic archaea account for two-thirds of global methane emissions. Some species, including Methanosarcina barkeri, reduce CO2 by directly acquiring electrons from solid substrates. However, the mechanism of electron acquisition in M. barkeri has remained unclear because this archaeon lacks the multiheme c-type cytochromes that drive extracellular electron transfer in many other microbes. Here we show that M. barkeri releases abundant extracellular nucleic acids during early growth, primarily short RNAs (78%). These extracellular nucleic acids assemble into G-quadruplexes (G4s) and B-DNA architectures that decorate cell surfaces and link aggregates. Surface-associated G4s are folded in vivo in a conformation compatible with cofactor binding and redox chemistry. Enzymatic degradation of extracellular nucleic acids abolished electron uptake and electromethanogenesis, whereas addition of synthetic G4-RNAs doubled methane yields and lowered cell-electrode interfacial resistance. These effects were not observed when cells were grown on soluble substrates. Together, these findings identify eRNA as a previously unrecognized electron conduit in methanogens, raising the possibility that RNA-based electron transfer may predate more elaborate protein-based electron conduits, with implications for models of early earth metabolism and for the design of next-generation bioenergy systems.

microbiology↗

Aerotolerant methanogens use seaweed and seagrass metabolites to drive marine methane emissions

Methanogenesis is classically thought to be limited to strictly anoxic environments. While oxygenated oceans are a known methane source, it is argued that methanogenesis is driven by methylphosphonate-degrading bacteria or potentially is associated to zooplankton gut microbiomes rather than by methanogenic archaea. Here we show through in situ monitoring and ex situ manipulations that methane is rapidly produced by archaea in frequently oxygenated sandy sediments. By combining biogeochemical, metagenomic, and culture-based experiments, we show this activity is driven by aerotolerant methylotrophic methanogens (Methanococcoides spp.) broadly distributed in surface layers of sandy sediments, providing evidence of a hidden process contributing to marine methane emissions. Moreover, we show that methane emissions are driven by methylated seaweed and seagrass metabolites, revealing an unexpected feedback loop between eutrophication-driven algal blooms and greenhouse gas emissions.

microbiology↗

Adaptation of a methanogen to the constructed environment

Due to unique genomic adaptations, Methanococcus maripaludis Mic1c10 exhibits severe corrosive behavior when in direct contact with Fe0. These adaptations are linked to attachment and effective growth on constructed surfaces. One such adaptation is that of a specific [NiFe]-hydrogenase that may anchor on the cell surface via glycosyl-glycosyl interactions to receive Fe0-electrons directly. Such an evolutionary response to constructed environments requires us to rethink methane cycling in human-altered ecosystems.

microbiology↗