The ISME Journal

Abstract The majority of marine nitrite-oxidising bacteria (NOB) belong to three uncultured genera within the Nitrospinaceae family and thus the ecophysiology of these main nitrate producing microorganisms in the ocean remains poorly resolved. Here, we report on the environmental characterization of one of these genera, which we name Candidatus Nitromaricola. A single species within this genus, Candidatus Nitromaricola pontica, comprises >95% of the nitrite-oxidising community in the permanently stratified Black Sea. This provided a unique opportunity to study this globally abundant genus in situ, across pronounced environmental gradients of oxygen and inorganic nitrogen concentrations. We show that Ca. Nitromaricola pontica is capable of oxidising nitrite at similar rates in both oxic and apparently anoxic waters, although it had a higher abundance in the more oxygenated waters of the Black Sea. The genome of Ca. Nitromaricola pontica indicates that like other NOB, it is a chemolithoautotroph, oxidising nitrite, and fixing inorganic carbon. However, Ca. Nitromaricola pontica and other members of the Ca. Nitromaricola genus lack canonical high affinity terminal oxidases found in some other NOB genera. Single-cell analyses confirmed active autotrophic growth and showed that ammonium and urea, rather than nitrite, were the main nitrogen sources for biomass production. Our findings identify Ca. Nitromaricola as a globally abundant marine NOB and highlight its cosmopolitan lifestyle.

Abstract Sulfoquinovose, a sulfonated sugar derived from the thylakoid membrane lipid sulfoquinovosyl diacylglycerol, is abundant in photosynthetic organisms and plays a key role in global sulfur cycling. Its degradation in nature is mediated by specialized bacteria, many of which rely on the enzyme sulfoquinovosidase (YihQ) to release sulfoquinovose from sulfoquinovosyl (diacyl)glycerol. Despite its ecological importance, the diversity and functional roles of sulfoquinovose-degrading microorganisms remain poorly characterized in natural environments. Here, we developed a yihQ-targeted amplicon sequencing approach to investigate the richness and distribution of SQ-degrading bacteria across selected environments. We revealed high richness of yihQ-containing microorganisms in the analyzed cow rumen samples, far exceeding that observed in human and mouse gut microbiomes, suggesting an important role of sulfoquinovose metabolism in ruminant digestion. Anoxic microcosm experiments with sulfoquinovose-amended rumen fluid revealed cooperative microbial degradation of sulfoquinovose to sulfide via isethionate cross-feeding. Amplicon sequencing and genome-resolved metagenomics and metatranscriptomics identified yet undescribed and uncultured sulfoquinovose-degrading taxa. Members of Caproiciproducens (Acutalibacteraceae), Candidatus Limivicinus (Oscillospiraceae), and Sphaerochaetaceae transcribed the isethionate-producing sulfo-transketolase pathway, whereas isethionate was likely respired by a Candidatus Mailhella bacterium (Desulfovibrionaceae). This study presents a functional gene-based assay for tracking environmental yihQ richness, highlights sulfoquinovose degradation as a central metabolic process in the cow rumen, describes previously unknown sulfoquinovose-metabolizing bacteria, and advances understanding of sulfur physiology in complex microbial communities.

Abstract Multicellular magnetotactic prokaryotes represent a unique group of obligately marine multicellular bacteria known for their ability to navigate along magnetic field lines thanks to ferrimagnetic nanocrystals. To date, two distinct spherical and ellipsoidal morphotypes have been described, typically ranging from 3 to 6 μm in diameter and comprising approximately 50 cells of the same species. Although widespread in highly reduced marine sediments, they are represented by solely three genera clustering into a monophyletic group within the Desulfobacterota. In this study, we report a third morphotype in reduced sediments of the Mediterranean Sea in Carry-le-Rouet, France, that is approximately 30 times more voluminous than any previously described form. Because their large size, we designated these multicellular bacteria as “giant” and explored their cell ultrastructure, ecological niche and physiology using magnetic enrichment and a combination of microscopy techniques and single-consortium genomics. Transmission electron microscopy and confocal microscopy images of several individual consortia revealed that they contain an average of 130 cells, each producing over 100 greigite magnetosomes arranged to optimize the overall magnetic moment. Phylogenomic analyses positioned giant multicellular magnetotactic prokaryotes, together with other morphotypes, in a previously undescribed genus and species within the Candidatus Magnetomoraceae family, named Magnetogigantoglobus mediterraneus. Although genetically divergent with a different ultrastructure, all multicellular magnetotactic prokaryotes seem to rely on sulfate reduction coupled to heterotrophy or autotrophy. We further discuss the significance of these findings in the context of the evolutionary history of multicellularity and magnetotaxis in prokaryotes.

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 Ferdinand Cohn observed abundant filamentous bacteria in drinking water wells in 1870 that he named Crenothrix polyspora. Subsequent research has revealed the methanotrophic metabolism of Crenothrix bacteria and their disproportionately high activity in stratified lakes compared to unicellular methanotrophs, yet laboratory cultivation has proven elusive, leaving the ecophysiology of Crenothrix bacteria largely unknown. Here we report the isolation of two methanotrophic strains of the “lacustrine Crenothrix” clade from an iron-rich wetland and reveal their unique cell biology and ecology. We demonstrate that the strains are microaerobic and grow as filaments of cells, which are connected by unidirectionally oriented structures. The strains have broad genomic repertoires for addressing O2 limitation that are uniquely associated with lacustrine Crenothrix compared to related clades based on genome data. Aligning with laboratory observations, we identify lacustrine Crenothrix bacteria along potential redox gradients in the wetland at iron-rich snow sites, and we also detect such bacteria in diverse global ecosystems based on public metagenome searches. Together, our data strongly point to an ecophysiology of lacustrine Crenothrix bacteria that is tightly linked to O2 limitation, and we propose that the strains uniquely store or share metabolic intermediates between cells in filaments to thrive under such conditions. Our cultivation-based findings for these strains, which we name Allocrenothrix methanica, provide new insights into the diversity, evolution, and ecology of filamentous methanotrophs, connecting over 150 years of microbiology research and opening vast new opportunities to investigate bacteria contributing to the global methane cycle under O2 limitation.

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 Dermatophilaceae polyphosphate-accumulating organisms (PAOs), formerly classified as Tetrasphaera PAOs, play pivotal roles in enhanced biological phosphorus removal (EBPR). However, their phylogenetic diversity, ecological preferences, and metabolic traits remain poorly characterized, and a robust marker gene for their classification is lacking. Here, we performed an extensive phylogenomic and metabolic analysis of Dermatophilaceae PAOs utilizing 46 newly recovered metagenome-assembled genomes from a laboratory-scale EBPR reactor treating high-strength wastewater and full-scale wastewater treatment plants. These analyses revealed a previously uncharacterized PAO genus, named here as Candidatus Dermatophostum, which shows specific preference for high-phosphorus environments. Its representative species, Ca. Dermatophostum ammonifactor, was enriched in the EBPR reactor and its PAO phenotype was confirmed by polyphosphate staining and fluorescence in situ hybridization. Integrative meta-omics combining genomic, transcriptomic, and protein structure analyses revealed its specialized metabolic capabilities for phosphate metabolism, glycogen synthesis, and dissimilatory nitrate reduction to ammonium. Moreover, Ca. Dermatophostum was found to be widely distributed across wastewater treatment plants worldwide, underscoring both its diverse metabolic capabilities and potential engineering implications for mitigating nitrous oxide (N2O) emissions for EBPR system. Finally, we propose a ppk1-based classification framework that resolves Dermatophilaceae PAOs into six distinct clades, consistent with whole-genome phylogeny, and demonstrates that ppk1 can serve as a reliable marker gene for tracking these populations. Together, these findings expand the ecological and functional understanding of Dermatophilaceae PAOs and highlight their promise for advancing sustainable wastewater treatment and resource recovery.

Abstract Deciphering the genomic basis of ecological diversification in activated sludge microbiomes is essential for optimizing treatment technology and advancing microbial ecology. Here, we present a global genome-resolved investigation of Candidatus Accumulibacter, the primary functional agent of enhanced biological phosphorus removal, based on 828 metagenomes from wastewater treatment plants across six continents. We recovered 104 high-quality Candidatus Accumulibacter metagenome-assembled genomes, discovering a new clade (Clade IV), substantially expanding the known phylogenetic diversity and revealing a ubiquitous yet geographically heterogeneous global distribution. Phylogenomic and pangenome analyses uncovered extensive clade-specific gene gain and loss, particularly in nitrogen metabolism, suggesting divergent evolutionary trajectories shaped by relaxed selection and niche adaptation. Genome-wide patterns of convergent streamlining and enriched antiviral defense systems indicate selective pressures from strong competition and viral predation. Constraint-based metabolic modeling revealed pervasive amino acid autotrophies and metabolic complementarity, coupled with distinct carbon utilization strategies that support ecological specialization across operational settings. Experimental validation reconciled model-phenotype discrepancies, highlighting the importance of transporter promiscuity and gene regulation in carbon substrate assimilation. Collectively, our findings redefine Candidatus Accumulibacter as a dynamic model of microbial genome plasticity, metabolic adaptation, and ecological resilience, providing an insight for understanding how microbial communities adapt and respond under engineered environmental conditions.

Abstract Phytoplankton are the base of marine food webs. They form intricate interactions with heterotrophic bacteria ranging from mutualistic to pathogenic that together impact oceanic carbon and nutrient cycling. Our understanding of these interactions in marine environments remains primarily limited to laboratory-based studies of model organisms. Here, we report the discovery and characterization of Ekhidna algicida sp. nov. strain To15, isolated from the oligotrophic Pacific Ocean (16°N, 140°W) based on its algicidal effect on the pelagic diatom Thalassiosira oceanica. Subsequent co-culture experiments demonstrate that E. algicida is lethal within days to a diverse array of diatoms, including diatoms isolated from similar locations, with the effect mediated by bacterial exudates produced during co-culture with susceptible diatoms. Exudates of E. algicida monoculture are not algicidal, suggesting a pathogenic shift upon interaction with susceptible diatoms. The genome of E. algicida To15 encodes for a type IX secretion system (T9SS), together with candidate secreted proteases, suggesting a potential protein-mediated pathogenicity. Twenty additional algicidal Ekhidna strains were subsequently isolated from the Pacific Ocean. All these algicidal bacteria pass through 0.2 μm pore-size filters, highlighting the importance of the often-overlooked group of “filterable” marine bacteria. Our findings reveal E. algicida as a Pacific Ocean diatom pathogen, with potential impacts on microbial community composition dynamics in pelagic ecosystems.

Abstract Analysing the nitrogen (15ε) and oxygen (18ε) isotope effects of anaerobic ammonium oxidation (anammox) is essential for accurately assessing its potential contribution to fixed-N losses in the ocean, yet the 18ε of anammox remains unexplored. Here, we determined the previously unexplored 18ε of anammox using a highly enriched culture of the marine anammox species “Ca. Scalindua sp”. Because Scalindua significantly accelerated oxygen isotope exchange between NO2− and H2O, we introduced a new rate constant for anammox-mediated oxygen isotope exchange (keq, AMX = 8.44 ~ 13.56 × 10−2 h−1), which is substantially faster than abiotic oxygen isotope exchange (keq, abio = 1.13 × 10−2 h−1), into a numerical model to estimate the 18ε during anammox. Based on our experimental results, we successfully determined the 18ε associated with: (1) conversion of NO2− to N2 (18εNO2- → N2 = 10.6 ~ 16.1‰), (2) NO2− oxidation to NO3− (18εNO2- → NO3- = −2.9 ~ −11.0‰, inverse fractionation), (3) incorporation of oxygen from water during NO2− oxidation to NO3− (18εH2O = 16.4 ~ 19.2‰). Our study underscores the possibility that unique anammox oxygen isotope signals may be masked due to substantial anammox-mediated oxygen isotope exchange between NO2− and H2O. Therefore, careful consideration is required when utilizing δ18ONO3- and δ18ONO2- as geochemical markers to assess the potential contribution of anammox to fixed-N losses in the ocean.