Publications

4795

Abstract The candidate phylum Cloacimonadota is frequently detected in anoxic environments such as anaerobic digestion (AD) reactors, hydrothermal vents, and deep-sea sediments, yet its metabolism remains poorly understood. Metagenomic evidence suggests capacities for amino acid fermentation, carbohydrate degradation, as well as a potential role in syntrophic propionate oxidation (SPO), a key bottleneck in AD. However, a complete methylmalonyl-CoA (mmc) pathway, central to SPO, has not been previously identified in Cloacimonadota genomes. Here, we report results from an acidified lab-scale anaerobic baffled reactor fed with sugar beet pulp, where an increase in the relative abundance of Cloacimonadota correlated with recovery of methanogenesis, resulting in increased methane content in the produced biogas. Metagenomic and metatranscriptomic analyses enabled metabolic reconstruction of the dominant Cloacimonadota operational taxonomic unit (OTU). Furthermore, using a curated database of 204 genome-resolved Cloacimonadota species, we characterized the phylum-level metabolic potential. Comparative genomics revealed alternative proteins, including 2-oxoglutarate:ferredoxin oxidoreductase and aspartate aminotransferase, likely to substitute for missing enzymes in the classical mmc pathway. These proteins were widely distributed and highly conserved across the analyzed Cloacimonadota genomes, suggesting that this variant of the SPO pathway could represent a phylum-specific trait. Moreover, we hypothesize that these alternative pathway steps may link propionate metabolism to protein degradation and poly-γ-glutamate biosynthesis. Network analysis identified the methanogenic archaeon Methanothrix as a potential syntrophic partner, an interaction further supported by propionate-fed enrichment cultures showing co-occurrence of Cloacimonadota and Methanothrix species. Our study sheds light on the Cloacimonadota metabolism, advancing our understanding of their ecological roles and potential for biotechnological applications.

Abstract Extreme acidic environments represent natural laboratories for investigating the mechanisms of microbial community assembly, yet the ecological processes structuring these communities remain incompletely understood. Here, we investigate how spatial partitioning, hydrodynamics, and colonization history shape microbial succession in a unique sulfur-rich, acidic river of volcanic origin in northern Patagonia. We combined 16S rRNA gene profiling and shotgun metagenomics with a multi-scale experimental framework encompassing water column fractionation and colonization assays under native and controlled conditions. Microbial diversity was strongly influenced by spatial fractionation, with free-living communities exhibiting higher richness and temporal variability than particle-associated assemblages. Water flow modulated community structure, increasing evenness in free-living fractions under high-flow conditions, but had limited impact on particle-attached communities. Colonization of sulfur-beads followed a structured successional trajectory, with autotrophic sulfur oxidizers dominating early stages and heterotrophs adapted to biofilm lifestyles increasing over time. Ex situ recolonization assays revealed strong priority effects, with initial colonizers determining successional trajectories. Turnover analyses revealed that the balance among stochastic and deterministic assembly processes shifted across communities with pronounced stochasticity in the water column and flow-dependent effects in free-living communities, while biofilm associated communities on sulfur-beads exhibited stronger contribution of deterministic selection. These ecological patterns were mirrored by functional differentiation, with gene enrichment analyses revealing adaptive signatures of substrate attachment and resource acquisition. By integrating fine-scale environmental variation with colonization dynamics, this study reveals how microscale habitat structure and temporal fluxes jointly modulate microbial community assembly rules, offering a nuanced framework to dissect ecological processes in extreme systems.

Abstract Nitrobacter strain NHB1 is a nitrite-oxidizing bacterium previously demonstrated to form a consortium capable of nitrification under acidic conditions when cocultivated with a neutrophilic ammonia-oxidizing bacterium. Here, we characterize the growth of isolated NHB1 under different pH and nitrite (NO2−) concentrations, as well as its influence on the activity of obligately acidophilic soil ammonia-oxidizing archaea (AOA) isolated from acidic soils when grown in coculture. NHB1 is acidotolerant with optimal growth at pH 6.0 (range: 5.0–7.5) at an initial NO2− concentration of 500 μM. However, at lower NO2− concentrations, closer to those found in soil, its pH optimum decreases to 5.0 and with detectable growth extended to pH 3.5. In coculture, NHB1 enhances the growth of the acidophilic AOA Nitrosotalea devaniterrae Nd1 and Nitrosotalea sinensis Nd2, which are highly sensitive to NO2-derived compounds and typically oxidize only ~200 to 300 μM ammonia (NH3) when grown in batch cultures as isolates. However, in coculture with NHB1, both strains oxidized up to ~3 mM NH3, limited only by the buffering capacity of the medium, and their pH range was also extended downward by ~0.5 units. NHB1 also possesses a cyanase, enabling reciprocal cross-feeding through cyanate-derived NH3 production while utilizing AOA-derived NO2−. These findings suggest that NO2− removal is essential for ammonia oxidizer growth in acidic soils and emphasize the importance of considering substrate and metabolic product concentrations when characterizing ecophysiology. Genome analysis reveals that NHB1 is distinct from validated species, and we propose the name “Nitrobacter laanbroekii.”

Abstract Members of the bacterial family Endozoicomonadaceae are ubiquitous marine symbionts associated with diverse hosts, including corals, sponges, molluscs, and fishes. Despite their ecological pervasiveness, inhabiting hosts in deep-sea vents and sunlit coral reefs, their taxonomy remains inconsistent, largely due to reliance on 16S rRNA gene phylogenies that fail to fully resolve evolutionary relationships. Here, we integrate phylogenomics, comparative genomics, and overall genome relatedness indices across 63 high-quality genomes to re-define genus boundaries within the Endozoicomonadaceae family. Among the metrics, the core-proteome average amino acid identity proved the most robust for genus-level resolution, with a proposed identity cutoff of 76%, aligning with phylogenomic structure and maintaining taxonomic robustness across the family. Phylogenomic reconstructions further revealed that the taxon Endozoicomonas is paraphyletic, forming two well-supported but distinct clades. This prompts a taxonomic revision, dividing Endozoicomonas into Endozoicomonas sensu stricto and Neoendozoicomonas gen. nov., with Neoendozoicomonas montiporae designated as the type species. Furthermore, the sister clade to Endozoicomonas sensu stricto—comprising the genera Endonucleibacter and Sororendozoicomonas—is characterized by genomic streamlining, including reduced genome size, lower GC content, reduced number of orthogroups, and potential functional divergences consistent with host specialization. Functional annotations highlighted secretion and conjugation systems as key differentiators between genera, emphasizing potential distinct host-interaction strategies. This genome-based framework refines the taxonomy of the Endozoicomonadaceae, provides additional criteria for genus delimitation, and strengthens the evolutionary and ecological interpretation of these widespread marine bacterial symbionts.

An anaerobic, salt-tolerant, rod-shaped bacterium, strain JL216-2 T , was isolated from the shell of the hydrothermal gastropod Alviniconcha marisindica in the Tianxiu hydrothermal field on the Carlsberg Ridge, Indian Ocean. Cells of strain JL216-2 T were motile and 0.5×3–6 µm in size. Strain JL216-2 T grew at 10–32 °C (optimal 28 °C), pH 6.0–9.0 (optimal pH 7.0) and 0.5–12.0% (w/v) sodium chloride(NaCl, optimal 2.5%). Strain JL216-2 T exhibited metabolic versatility, being capable of heterotrophic growth on complex organic compounds. It also performed autotrophic growth by utilizing carbon dioxide (CO₂) fixation or sodium bicarbonate (NaHCO 3 ) as the sole carbon source, driven by hydrogen oxidation coupled with Fe(III) reduction. Phylogenetic analysis based on 16S rRNA gene sequences indicated that the strain was most closely related to Helicovermis profundi S502 T (90.43% sequence similarity). The genome size of strain JL216-2 T was 4.91 Mb, with a G+C content of 39.54 mol%. Phylogenomic analysis and overall genome relatedness indices values indicated a close relatedness of strain JL216-2 T to H. profundi S502 T and Fusibacter spp. The combined genotypic and phenotypic data showed that strain JL216-2 T represents a novel genus within the order Eubacteriales . The type strain is JL216-2 T (=MCCC M30262 T =KACC 23553 T ).

Abstract The Genome Taxonomy Database (GTDB; https://gtdb.ecogenomic.org) provides a phylogenetically consistent and rank normalized genome-based taxonomy for prokaryotic genomes sourced from the NCBI Assembly database. GTDB release 10 (R10-RS226) spans 715 230 bacterial and 17 245 archaeal genomes organized into 136 646 bacterial and 6968 archaeal species clusters. Fewer new major branches of prokaryotic life are being discovered with each release of GTDB, suggesting that we are beginning to saturate readily discoverable microbial diversity through culture-independent analyses. However, species discovery continues unabated as >95% of bacterial and archaeal species remain to be genomically elucidated based on conservative projections. We present additions to the GTDB website, methodological improvements, policy changes, notable nomenclatural updates, and user applications. We conclude with a summary of future plans for the resource including a fungal taxonomy and a nomenclatural extension to classify pathogens.