Abstract
Background: ‘Ca. Aenigmarchaeota’ represents an evolutionary branch within the DPANN superphylum. However, their ecological roles and potential host-symbiont interactions are poorly understood.Results: Here, we analyze eight metagenomic-assembled genomes from hot spring habitats and reveal their functional potentials. Although they have limited metabolic capacities, they harbor substantial carbohydrate metabolizing abilities. Further investigation suggests that horizontal gene transfer might be the main driver that endows these abilities to ‘Ca. Aenigmarchaeota’, including enzymes involved in glycolysis. Additionally, members from the TACK superphylum and Euryarchaeota contribute substantially to the niche expansion of ‘Ca. Aenigmarchaeota’, especially genes related to carbohydrate metabolism and stress responses. Based on co-occurrence network analysis, we conjecture that ‘Ca. Aenigmarchaeota’ may be symbionts associated with TACK archaea and Euryarchaeota, though host-specificity might be wide and variable across different ‘Ca. Aenigmarchaeota’ genomes. Conclusion: This study provides significant insights into possible host-symbiont interactions and ecological roles of ‘Ca. Aenigmarchaeota’.
Abstract
Several recent studies have shown the presence of genes for the key enzyme associated with archaeal methane/alkane metabolism, methyl-coenzyme M reductase (Mcr), in metagenome-assembled genomes (MAGs) divergent to existing archaeal lineages. Here, we study the mcr-containing archaeal MAGs from several hot springs, which reveal further expansion in the diversity of archaeal organisms performing methane/alkane metabolism. Significantly, an MAG basal to organisms from the phylum Thaumarchaeota that contains mcr genes, but not those for ammonia oxidation or aerobic metabolism, is identified. Together, our phylogenetic analyses and ancestral state reconstructions suggest a mostly vertical evolution of mcrABG genes among methanogens and methanotrophs, along with frequent horizontal gene transfer of mcr genes between alkanotrophs. Analysis of all mcr-containing archaeal MAGs/genomes suggests a hydrothermal origin for these microorganisms based on optimal growth temperature predictions. These results also suggest methane/alkane oxidation or methanogenesis at high temperature likely existed in a common archaeal ancestor.
A thermophilic, filamentous, heterotrophic bacterium, designated strain JAD2T, a member of an as-yet uncultivated lineage that is present and sometimes abundant in some hot springs worldwide, was isolated from sediment of Great Boiling Spring in Nevada, USA. Cells had a mean diameter of 0.3 µm and length of 4.0 µm, and formed filaments that typically ranged in length from 20 to 200 µm. Filaments were negative for the Gram stain reaction, spores were not formed and motility was not observed. The optimum temperature for growth was 72.5–75 °C, with a range of 67.5–75 °C, and the optimum pH for growth was 6.75, with a range of pH 6.5–7.75. Peptone, tryptone or yeast extract were able to support growth when supplemented with vitamins, but no growth was observed using a variety of defined organic substrates. Strain JAD2T was microaerophilic and facultatively anaerobic, with optimal growth at 1 % (v/v) O2 and an upper limit of 8 % O2. The major cellular fatty acids (>5 %) were C16 : 0, C19 : 0, C18 : 0, C20 : 0 and C19 : 1. The genomic DNA G+C content was 69.3 mol%. Phylogenetic and phylogenomic analyses using sequences of the 16S rRNA gene and other conserved genes placed JAD2T within the phylum
Chloroflexi
, but not within any existing class in this phylum. These results indicate that strain JAD2T is the first cultivated representative of a novel lineage within the phylum
Chloroflexi
, for which we propose the name Thermoflexus hugenholtzii gen. nov., sp. nov., within Thermoflexia classis nov., Thermoflexales ord. nov. and Thermoflexaceae fam. nov. The type strain of Thermoflexus hugenholtzii is JAD2T ( = JCM 19131T = CCTCC AB-2014030T).