Publications

4861

Abstract Microbes are the most abundant form of life on Earth and play crucial roles in carbon and nutrient cycling. Despite their crucial role, our understanding of microbial diversity and physiology on the ocean floor is limited. To address this gap in knowledge, we obtained 55 novel bacterial metagenome-assembled genomes (MAGs) from coastal and deep sea sediments. Phylogenomic analyses revealed they belong to four new and one poorly described bacterial phyla. Comparison of their rRNA genes with public databases revealed they are all globally distributed. These novel bacteria are capable of the anaerobic degradation of polysaccharides and proteins, and the respiration of sulfur and nitrogen. These genomes code for an unusually high proportion (~ 9, and up to 20% per genome) of protein families lacking representatives in public databases. Hundreds of these protein families are predicted to be co-localized with genes for sulfur reduction, nitrogen cycling, energy conservation, and the degradation of organic compounds. These findings expand our understanding of microbial diversity and link previously overlooked gene families with key metabolic processes in the oceans.

Summary Uncultivated microbial clades (‘microbial dark matter’) are inferred to play important but uncharacterized roles in nutrient cycling. Using Antarctic lake (Ace Lake, Vestfold Hills) metagenomes, 12 metagenome‐assembled genomes (MAGs; 88%–100% complete) were generated for four ‘dark matter’ phyla: six MAGs from Candidatus Auribacterota (=Aureabacteria, SURF‐CP‐2), inferred to be hydrogen‐ and sulfide‐producing fermentative heterotrophs, with individual MAGs encoding bacterial microcompartments (BMCs), gas vesicles, and type IV pili; one MAG (100% complete) from Candidatus Hinthialibacterota (=OLB16), inferred to be a facultative anaerobe capable of dissimilatory nitrate reduction to ammonia, specialized for mineralization of complex organic matter (e.g. sulfated polysaccharides), and encoding BMCs, flagella, and Tad pili; three MAGs from Candidatus Electryoneota (=AABM5‐125‐24), previously reported to include facultative anaerobes capable of dissimilatory sulfate reduction, and here inferred to perform sulfite oxidation, reverse tricarboxylic acid cycle for autotrophy, and possess numerous proteolytic enzymes; two MAGs from Candidatus Lernaellota (=FEN‐1099), inferred to be capable of formate oxidation, amino acid fermentation, and possess numerous enzymes for protein and polysaccharide degradation. The presence of 16S rRNA gene sequences in public metagenome datasets (88%–100% identity) suggests these ‘dark matter’ phyla contribute to sulfur cycling, degradation of complex organic matter, ammonification and/or chemolithoautotrophic CO 2 fixation in diverse global environments.