Evolutionary ecology of denitrifying methanotrophic NC10 bacteria in the deep‐sea biosphere

Abstract

AbstractThe NC10 phylum links anaerobic methane oxidation to nitrite denitrification through a unique O2‐producing intra‐aerobic methanotrophic pathway. Although numerous amplicon‐based studies revealed the distribution of this phylum, comprehensive genomic insights and niche characterization in deep‐sea environments were still largely unknown. In this study, we extensively surveyed the NC10 bacteria across diverse deep‐sea environments, including waters, sediments, cold seeps, biofilms, rocky substrates, and subseafloor aquifers. We then reconstructed and analysed 38 metagenome‐assembled genomes (MAGs), and revealed the extensive distribution of NC10 bacteria and their intense selective pressure in these harsh environments. Isotopic analyses combined with gene expression profiling confirmed that active nitrite‐dependent anaerobic methane oxidation (n‐DAMO) occurs within deep‐sea sediments. In addition, the identification of the Wood–Ljungdahl (WL) and 3‐hydroxypropionate/4‐hydroxybutyrat (3HB/4HP) pathways in these MAGs suggests their capability for carbon fixation as chemoautotrophs in these deep‐sea environments. Indeed, we found that for their survival in the oligotrophic deep‐sea biosphere, NC10 bacteria encode two branches of the WL pathway, utilizing acetyl‐CoA from the carbonyl branch for citric acid cycle‐based energy production and methane from the methyl branch for n‐DAMO. The observed low ratios of non‐synonymous substitutions to synonymous substitutions (pN/pS) in n‐DAMO‐related genes across these habitats suggest a pronounced purifying selection that is critical for the survival of NC10 bacteria in oligotrophic deep‐sea environments. These findings not only advance our understanding of the evolutionary adaptations of NC10 bacteria but also underscore the intricate coupling between the carbon and nitrogen cycles within deep‐sea ecosystems, driven by this bacterial phylum.