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Khanongnuch, R.

Publications and source records attributed to Khanongnuch, R..

2 recordsLinked to original sources

Characterization and genome analysis of a psychrophilic methanotroph representing a ubiquitous Methylobacter spp. cluster in boreal lake ecosystems

Lakes and ponds are considered as a major natural source of CH4 emissions, particularly during the ice-free period in boreal ecosystems. Aerobic methane oxidizing bacteria (MOB), which utilize CH4 using oxygen as an electron acceptor, are one of dominant microorganisms in the CH4-rich water columns. The metagenome-assembled genomes (MAGs) have revealed the genetic potential of MOB from boreal aquatic ecosystems for various microaerobic/anaerobic metabolic functions; however, the experimental validation of the process has not been succeeded. Additionally, psychrophilic (i.e., cold loving) MOB isolates and their CH4 oxidizing process have rarely been investigated. In this study, we isolated, provided taxonomic description, and analyzed the genome of Methylobacter sp. S3L5C, a psychrophilic MOB, from a boreal lake in Finland. Based on phylogenomic comparisons to MAGs, Methylobacter sp. S3L5C represented a ubiquitous cluster of Methylobacter spp. in boreal aquatic ecosystems. At optimal temperatures (3-12 {degrees}C) and pH (6.8-8.3), the specific growth rates () and CH4 utilization rate were in the range of 0.018-0.022 h-1 and 0.66-1.52 mmol l-1 d-1, respectively. In batch cultivation, the isolate could produce organic acids and the concentrations were elevated after replenishing CH4 and air into headspace. The highest concentrations of 4.1 mM acetate, 0.02 mM malate and 0.07 mM propionate were observed at the end of the cultivation period under the optimal operational conditions. The results herein highlight the key role of Methylobacter spp. in regulating CH4 emissions and their potential to provide CH4-derived organic carbon compounds to surrounding heterotrophic microorganisms in cold ecosystems.

microbiology↗

A two-staged bacterial process coupling methanotrophic and heterotrophic bacteria for 1-alkene production from methane

Methane (CH4) is a sustainable carbon feedstock source for aerobic CH4-oxidizing bacteria (methanotrophs) to produce value-added chemicals. Under substrate-limited (e.g., CH4, oxygen and nitrogen) conditions, CH4 oxidation results in the production of various short-chain organic acids and platform chemicals. These CH4-derived products could be broadened by utilizing them as a feedstock for heterotrophic bacteria. As a proof of concept, a two-stage system for CH4 abatement and 1-alkene production was developed in this study. Types I and II methanotrophs, i.e., Methylobacter tundripaludum SV96 and Methylocystis rosea SV97, respectively, were investigated in batch tests under different CH4 and air supplementation schemes. CH4 oxidation under either microaerobic or aerobic conditions induced the production of formate, acetate, succinate, and malate in M. tundripaludum SV96, accounting for 4.8-7.0% of consumed CH4-carbon while M. rosea SV97 produced the same compounds except for malate, and with lower efficiency than M. tundripaludum SV96, accounting for 0.7-1.8% of consumed CH4-carbon For the first time, the organic acids-rich spent media of methanotrophs were successfully used for 1-alkene production using engineered Acinetobacter baylyi ADP1 tesA-undA cells. The highest yield of 1-undecene was obtained from spent medium of M. tundripaludum SV96 at 68.9 {+/-} 11.6 mol mol Csubstrate-1.

microbiology↗