Systems analysis of the effect of hydrogen sulfide on the growth of Methylococcus capsulatus Bath.

Methanotrophs are bacteria capable on growing on methane as their sole carbon source. They may provide a promising route for upgrading natural gas into more valuable fuels and chemicals. However, natural gas may contain significant quantities of hydrogen sulfide. Little is known about how hydrogen sulfide affects the growth and physiology of methanotrophs aside from a few studies showing that it is inhibitory. This study investigated how hydrogen sulfide affects the growth and physiology of the model methanotroph, Methylococcus capsulatus Bath. Growth studies demonstrated that hydrogen sulfide inhibits the growth of M. capsulatus Bath when the concentration exceeds 0.5% (v/v). To better understand how hydrogen sulfide is inhibiting the growth of M. capsulatus Bath, transcription and metabolite concentrations were profiled using RNA sequencing and gas chromatography-mass spectrometry, respectively. Our analysis of the differentially expressed genes and changes in metabolite concentrations suggests that hydrogen sulfide inhibits cellular respiration. The cells respond to sulfide stress in part by increasing the rate of sulfide oxidation and by increasing the expression of sulfide quinone reductase and a putative persulfide dioxygenase. In addition, they reduce the expression of the native calcium-dependent methanol dehydrogenase and increase the expression of XoxF, a lanthanide-dependent methanol dehydrogenase. While the reason of this switch in unknown, XoxF has previously been shown to be induced by lanthanides or nitric oxide in methanotrophs. Collectively, these results further our understanding of how methanotrophs respond to sulfide stress and may aid in the engineering of strains resistant to hydrogen sulfide. KEY POINTS: • Hydrogen sulfide inhibits growth of Methylococcus capsulatus Bath • Sulfide stress inhibits cellular respiration • Sulfide stress induces XoxF, a lanthanide-dependent methanol dehydrogenase.

Effects of dosing non-toxigenic Clostridia on the bacterial populations and immunological responses in the intestinal tract of lactating dairy cows.

Understanding the effects of dosing non-toxigenic Clostridia to cows is rare and has received little attention so far. In the present study, a total of eight lactating dairy cows were divided in two groups: control (n = 4) or Clostridia challenged (oral supplementation of five diverse strains of Paraclostridium bifermentans, n = 4). Bacterial communities were analyzed by qPCR and next-generation sequencing (NGS) in the buccal mucosa as well as digesta and mucosal samples of the gastrointestinal (GI) tract from rumen to rectum (10 compartments), as well as fecal samples. Transcriptomic analysis of barrier and immune-related gene expression was performed on rumen, jejunum, and liver samples. We observed increased microbial populations with the Clostridial challenge in the buccal tissues and the proximal GI tract (forestomach), correlating with Clostridial loads in the feed. Otherwise, there were no significant differences in microbial populations (p > 0.05) throughout the distal part of the GI tract. The NGS approach, however, revealed that the Clostridial challenge changed the relative abundance of gut and fecal microbiota. In particular, in the challenge group, no Bifidobacterium was observed in the mucosa-associated microbiota and abundance of Pseudomonadota increased in the feces. These results indicated potential adverse effects of Clostridia to cow health. In general, immune responses to the Clostridial challenge were weak. However, transcriptional analysis revealed the down-regulation of junction adhesion molecule encoding gene (-1.44 of log2 fold-change), which might impact intestinal permeability.

Genome Sequence of a Thermoacidophilic Methanotroph Belonging to the Verrucomicrobiota Phylum from Geothermal Hot Springs in Yellowstone National Park: A Metagenomic Assembly and Reconstruction.

Verrucomicrobiotal methanotrophs are thermoacidophilic methane oxidizers that have been isolated from volcanic and geothermal regions of the world. We used a metagenomic approach that entailed obtaining the whole genome sequence of a verrucomicrobiotal methanotroph from a microbial consortium enriched from samples obtained from Nymph Lake (89.9 °C, pH 2.73) in Yellowstone National Park in the USA. To identify and reconstruct the verrucomicrobiotal genome from Illumina NovaSeq 6000 sequencing data, we constructed a bioinformatic pipeline with various combinations of de novo assembly, alignment, and binning algorithms. Based on the marker gene (pmoA), we identified and assembled the Candidatus Methylacidiphilum sp. YNP IV genome (2.47 Mbp, 2392 ORF, and 41.26% GC content). In a comparison of average nucleotide identity between Ca. Methylacidiphilum sp. YNP IV and Ca. Methylacidiphilum fumariolicum SolV, its closest 16S rRNA gene sequence relative, is lower than 95%, suggesting that Ca. Methylacidiphilum sp. YNP IV can be regarded as a different species. The Ca. Methylacidiphilum sp. YNP IV genome assembly showed most of the key genes for methane metabolism, the CBB pathway for CO2 fixation, nitrogen fixation and assimilation, hydrogenases, and rare earth elements transporter, as well as defense mechanisms. The assembly and reconstruction of a thermoacidophilic methanotroph belonging to the Verrucomicrobiota phylum from a geothermal environment adds further evidence and knowledge concerning the diversity of biological methane oxidation and on the adaptation of this geochemically relevant reaction in extreme environments.