Demethylated hopanoids in ‘Ca. Methylomirabilis oxyfera’ as biomarkers for environmental nitrite-dependent methane oxidation

Publication date

2019-11

Authors

Smit, Nadine T.
Rush, Darci
Sahonero-Canavesi, Diana X.
Verweij, Monique
Rasigraf, Olivia
Guerrero Cruz, S.
Jetten, Mike S.M.
Sinninghe Damste, JaapORCID 0000-0002-8683-1854ISNI 0000000390349312
Schouten, StefanISNI 0000000387885288

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Abstract

Hopanoids are lipids that are widespread in the bacterial domain and well established molecular biomarkers in modern and paleo environments. In particular, the occurrence of 13C-depleted 3-methylated hopanoids are characteristic of aerobic bacteria involved in methane oxidation. Previously the intra-aerobic methanotroph ‘Candidatus Methylomirabilis oxyfera’ (‘Ca. M. oxyfera’), which performs nitrite-dependent methane oxidation in anoxic environments, has been shown to synthesize bacteriohopanepolyols (BHPs) and their 3-methylated counterparts. However, since ‘Ca. M. oxyfera’ does not utilize methane as a carbon source, its biomass and lipids do not show the characteristic 13C-depletion. Therefore, the detection of ‘Ca. M. oxyfera’ in various environments is challenging, and still underexplored. Here, we re-investigated the hopanoid content of ‘Ca. M. oxyfera’ bacteria using enrichment cultures. We found the GC-amenable hopanoids of ‘Ca. M. oxyfera’ to be dominated by four demethylated hopanoids of which only one, 22,29,30-trisnorhopan-21-one, had been identified previously. The three novel hopanoids were tentatively identified as 22,29,30-trisnorhopan-21-ol, 3-methyl-22,29,30-trisnorhopan-21-one and 3-methyl-22,29,30-trisnorhopan-21-ol. These unique demethylated hopanoids are most likely biosynthesized directly by ‘Ca. M. oxyfera’ bacteria. Bioinformatical analysis of the ‘Ca. M. oxyfera’ genome revealed potential candidate genes responsible for the demethylation of hopanoids. For the sensitive detection of the four trisnorhopanoid biomarkers in environmental samples, a multiple reaction monitoring (MRM) method was developed and used to successfully detect the trisnorhopanoids in a peatland where the presence of ‘Ca. M. oxyfera’ had been confirmed previously by DNA-based analyses. These new biomarkers may be a novel tool to trace nitrite-dependent methane oxidation in various (past) environments.

Keywords

3-Methyl 22,29,30-trisnorhopan-21-one, Candidatus Methylomirabilis oxyfera, Demethylated hopanoids, Methylation, Nitrite-dependent methane oxidation, Trisnorhopanoids, Geochemistry and Petrology

Citation

Smit, N T, Rush, D, Sahonero-Canavesi, D X, Verweij, M, Rasigraf, O, Guerrero Cruz, S, Jetten, M S M, Sinninghe Damsté, J S & Schouten, S 2019, 'Demethylated hopanoids in ‘ Ca. Methylomirabilis oxyfera’ as biomarkers for environmental nitrite-dependent methane oxidation', Organic Geochemistry, vol. 137, 103899. https://doi.org/10.1016/j.orggeochem.2019.07.008