Jetten, Mike S. M.

AbstractThe NC10 phylum is a candidate phylum of prokaryotes and is considered important in biogeochemical cycles and evolutionary history. NC10 members are as-yet-uncultured and are difficult to enrich and our knowledge regarding this phylum is largely limited to the first species ‘Candidatus Methylomirabilis oxyfera’ (M. oxyfera). Here, we enriched NC10 members from paddy soil and obtained a novel species of the NC10 phylum that mediates the anaerobic oxidation of methane (AOM) coupled to nitrite reduction. By comparing the new 16S rRNA gene sequences with those already in the database, this new species was found to be widely distributed in various habitats in China. Therefore, we tentatively named it ‘Candidatus Methylomirabilis sinica’ (M. sinica). Cells of M. sinica are roughly coccus-shaped (0.7–1.2 μm), distinct from M. oxyfera (rod-shaped; 0.25–0.5 × 0.8–1.1 μm). Notably, microscopic inspections revealed that M. sinica grew in honeycomb-shaped microcolonies, which was the first discovery of microcolony of the NC10 phylum. This finding opens the possibility to isolate NC10 members using microcolony-dependent isolation strategies.

ABSTRACT We present the draft genome of anammox bacterium “ Candidatus Scalindua brodae,” which at 282 contigs is a major improvement over the highly fragmented genome assembly of related species “ Ca. Scalindua profunda” (1,580 contigs) which was previously published.

ABSTRACT “ Candidatus Methylomirabilis oxyfera” is a newly discovered anaerobic methanotroph that, surprisingly, oxidizes methane through an aerobic methane oxidation pathway. The second step in this aerobic pathway is the oxidation of methanol. In Gram-negative bacteria, the reaction is catalyzed by pyrroloquinoline quinone (PQQ)-dependent methanol dehydrogenase (MDH). The genome of “ Ca . Methylomirabilis oxyfera” putatively encodes three different MDHs that are localized in one large gene cluster: one so-called MxaFI-type MDH and two XoxF-type MDHs (XoxF1 and XoxF2). MxaFI MDHs represent the canonical enzymes, which are composed of two PQQ-containing large (α) subunits (MxaF) and two small (β) subunits (MxaI). XoxF MDHs are novel, ecologically widespread, but poorly investigated types of MDHs that can be phylogenetically divided into at least five different clades. The XoxF MDHs described thus far are homodimeric proteins containing a large subunit only. Here, we purified a heterotetrameric MDH from “ Ca . Methylomirabilis oxyfera” that consisted of two XoxF and two MxaI subunits. The enzyme was localized in the periplasm of “ Ca . Methylomirabilis oxyfera” cells and catalyzed methanol oxidation with appreciable specific activity and affinity ( V max of 10 μmol min −1 mg −1 protein, K m of 17 μM). PQQ was present as the prosthetic group, which has to be taken up from the environment since the known gene inventory required for the synthesis of this cofactor is lacking. The MDH from “ Ca . Methylomirabilis oxyfera” is the first representative of type 1 XoxF proteins to be described.

ABSTRACT Methane is an important greenhouse gas and the most abundant hydrocarbon in the Earth's atmosphere. Methanotrophic microorganisms can use methane as their sole energy source and play a crucial role in the mitigation of methane emissions in the environment. “ Candidatus Methylomirabilis oxyfera” is a recently described intra-aerobic methanotroph that is assumed to use nitric oxide to generate internal oxygen to oxidize methane via the conventional aerobic pathway, including the monooxygenase reaction. Previous genome analysis has suggested that, like the verrucomicrobial methanotrophs, “ Ca. Methylomirabilis oxyfera” encodes and transcribes genes for the Calvin-Benson-Bassham (CBB) cycle for carbon assimilation. Here we provide multiple independent lines of evidence for autotrophic carbon dioxide fixation by “ Ca. Methylomirabilis oxyfera” via the CBB cycle. The activity of ribulose-1,5-bisphosphate carboxylase/oxygenase (RubisCO), a key enzyme of the CBB cycle, in cell extracts from an “ Ca. Methylomirabilis oxyfera” enrichment culture was shown to account for up to 10% of the total methane oxidation activity. Labeling studies with whole cells in batch incubations supplied with either 13 CH 4 or [ 13 C]bicarbonate revealed that “ Ca. Methylomirabilis oxyfera” biomass and lipids became significantly more enriched in 13 C after incubation with 13 C-labeled bicarbonate (and unlabeled methane) than after incubation with 13 C-labeled methane (and unlabeled bicarbonate), providing evidence for autotrophic carbon dioxide fixation. Besides this experimental approach, detailed genomic and transcriptomic analysis demonstrated an operational CBB cycle in “ Ca. Methylomirabilis oxyfera.” Altogether, these results show that the CBB cycle is active and plays a major role in carbon assimilation by “ Ca. Methylomirabilis oxyfera” bacteria. Our results suggest that autotrophy might be more widespread among methanotrophs than was previously assumed and implies that a methanotrophic community in the environment is not necessarily revealed by 13 C-depleted lipids.

Summary Anaerobic ammonium‐oxidizing (anammox) bacteria are responsible for a significant portion of the loss of fixed nitrogen from the oceans, making them important players in the global nitrogen cycle. To date, marine anammox bacteria found in marine water columns and sediments worldwide belong almost exclusively to the ‘ Candidatus Scalindua’ species, but the molecular basis of their metabolism and competitive fitness is presently unknown. We applied community sequencing of a marine anammox enrichment culture dominated by ‘ Candidatus Scalindua profunda’ to construct a genome assembly, which was subsequently used to analyse the most abundant gene transcripts and proteins. In the S. profunda assembly, 4756 genes were annotated, and only about half of them showed the highest identity to the only other anammox bacterium of which a metagenome assembly had been constructed so far, the freshwater ‘ Candidatus Kuenenia stuttgartiensis’. In total, 2016 genes of S. profunda could not be matched to the K. stuttgartiensis metagenome assembly at all, and a similar number of genes in K. stuttgartiensis could not be found in S. profunda . Most of these genes did not have a known function but 98 expressed genes could be attributed to oligopeptide transport, amino acid metabolism, use of organic acids and electron transport. On the basis of the S. profunda metagenome, and environmental metagenome data, we observed pronounced differences in the gene organization and expression of important anammox enzymes, such as hydrazine synthase (HzsAB), nitrite reductase (NirS) and inorganic nitrogen transport proteins. Adaptations of Scalindua to the substrate limitation of the ocean may include highly expressed ammonium, nitrite and oligopeptide transport systems and pathways for the transport, oxidation, and assimilation of small organic compounds that may allow a more versatile lifestyle contributing to the competitive fitness of Scalindua in the marine realm.

ABSTRACT The recently described bacterium “ Candidatus Methylomirabilis oxyfera” couples the oxidation of the important greenhouse gas methane to the reduction of nitrite. The ecological significance of “ Ca . Methylomirabilis oxyfera” is still underexplored, as our ability to identify the presence of this bacterium is thus far limited to DNA-based techniques. Here, we investigated the lipid composition of “ Ca . Methylomirabilis oxyfera” to identify new, gene-independent biomarkers for the environmental detection of this bacterium. Multiple “ Ca . Methylomirabilis oxyfera” enrichment cultures were investigated. In all cultures, the lipid profile was dominated up to 46% by the fatty acid (FA) 10-methylhexadecanoic acid (10MeC 16:0 ). Furthermore, a unique FA was identified that has not been reported elsewhere: the monounsaturated 10-methylhexadecenoic acid with a double bond at the Δ7 position (10MeC 16:1Δ7 ), which comprised up to 10% of the total FA profile. We propose that the typical branched fatty acids 10MeC 16:0 and 10MeC 16:1Δ7 are key and characteristic components of the lipid profile of “ Ca . Methylomirabilis oxyfera.” The successful detection of these fatty acids in a peatland from which one of the enrichment cultures originated supports the potential of these unique lipids as biomarkers for the process of nitrite-dependent methane oxidation in the environment.

Summary ‘ Candidatus Methylomirabilis oxyfera’ is a denitrifying methanotroph that performs nitrite‐dependent anaerobic methane oxidation through a newly discovered intra‐aerobic pathway. In this study, we investigated the response of a M. oxyfera enrichment culture to oxygen. Addition of either 2% or 8% oxygen resulted in an instant decrease of methane and nitrite conversion rates. Oxygen exposure also led to a deviation in the nitrite to methane oxidation stoichiometry. Oxygen‐uptake and inhibition studies with cell‐free extracts displayed a change from cytochrome c to quinol as electron donor after exposure to oxygen. The change in global gene expression was monitored by deep sequencing of cDNA using Illumina technology. After 24 h of oxygen exposure, transcription levels of 1109 (out of 2303) genes changed significantly when compared with the anoxic period. Most of the genes encoding enzymes of the methane oxidation pathway were constitutively expressed. Genes from the denitrification pathway, with exception of one of the putative nitric oxide reductases, norZ2 , were severely downregulated. The majority of known genes involved in the vital cellular functions, such as nucleic acid and protein biosynthesis and cell division processes, were downregulated. The alkyl hydroperoxide reductase, ahpC , and genes involved in the synthesis/repair of the iron–sulfur clusters were among the few upregulated genes. Further, transcription of the pmoCAB genes of aerobic methanotrophs present in the non‐ M. oxyfera community were triggered by the presence of oxygen. Our results show that oxygen‐exposed cells of M. oxyfera were under oxidative stress and that in spite of its oxygenic capacity, exposure to microoxic conditions has an overall detrimental effect.