Environmental Microbiology

The Deep Chlorophyll Maximum (DCM) is likely the most important feature organizing the marine epipelagic environment. Within this layer, opposing gradients of light and nutrients create a stratified habitat that supports high phytoplankton biomass and a substantial fraction of oceanic primary production. Despite its ecological importance, most studies treat the DCM as a single depth, overlooking its fine-scale heterogeneity. Here we investigated prokaryotic community organization across the DCM in the northwestern Mediterranean Sea through high-resolution sampling of four profiles collected over two days. Free-living (0.2-3 {micro}m) and particle-associated (3-20 {micro}m) communities were characterized using 16S rRNA gene amplicon sequencing. Prokaryotic communities changed progressively along the vertical gradient, revealing the DCM as a microbial coenocline with continuous community turnover. Fuzzy clustering identified distinct assemblages associated with environmental transitions from warm surface waters to the chlorophyll maximum, the nitrite peak below the DCM, and deeper nitrate-rich layers. In both the free-living and particle-associated fractions, most ASVs remained consistently associated with the same depth-defined clusters across all samplings, indicating stable niche partitioning over short timescales. However, these temporally stable ASVs accounted for a substantially smaller fraction of community sequences in particle-associated communities, suggesting higher dynamism, likely driven by particle-mediated transport. Nevertheless, phylogenetic analyses revealed that closely related ASVs tended to occupy similar depth niches, indicating that habitat preferences are phylogenetically conserved in both size fractions. Our results demonstrate prokaryotic niche partitioning over scales of only a few meters within the DCM, highlighting the importance of fine-scale sampling for understanding microbial community structure and responses to ocean change.

Bacteria of the family Endozoicomonadaceae are widely associated with marine animals, yet their in situ metabolism remains mostly unknown. Genomic studies suggest that members of this family engage in extensive metabolic exchange with their hosts, ranging from nutrient provision in mutualistic sponge and coral symbioses to strong dependence on host metabolites like lipids in parasitic associations. Here, we study the lipid phenotype of the parasitic bacterium Candidatus Endonucleibacter childressi in its native tissue environment. The bacterium infects epithelial cells in the gill of the deep-sea mussel Gigantidas childressi and co-occurs with the mussel chemosynthetic symbionts providing a system to compare lipid profiles of symbiotic and parasitic gammaproteobacteria. We linked bacterial identity to metabolic phenotypes by combining mass spectrometry imaging with 16S rRNA fluorescence in situ hybridization. We identified phospholipids characteristic of regions infected with Ca. Endonucleibacter childressi. A subset of these lipids was also detected in symbiont-colonized regions, revealing a partial overlap in the phospholipid profiles of the two gammaproteobacteria. Fatty acids from PEs assigned to Ca. Endonucleibacter childressi contained polyunsaturated fatty acids such as FA 16:3, FA 18:3 or FA 18:4 which have not been reported from cultured close relatives. We hypothesize that the observed fatty acid profile may reflect adaptations to a host-associated lifestyle which involves the acquisition and remodeling of host-derived fatty acids. Our findings demonstrate the value of characterizing bacterial metabolic phenotypes directly in their native tissue environment and highlight the potential of spatial lipidomics to reveal metabolic dependencies in host-microbe associations.

Intertidal mudflats are low hydrodynamic energy environments hosting microphytobenthic communities that experience strong spatiotemporal variability in light regimes, including changes in spectral quality and light intensity that can lead to cellular photooxidative stress. To cope with these fluctuations, autotrophs exhibit diverse and highly plastic adaptations that are often species-dependent and shaped by their ecological niches. This study investigates photophysiological responses and metabolic remodeling in a diatom assemblage originating from a natural winter microphytobenthic biofilm under contrasting red and blue light intensities. To this end, photosynthetic parameters were monitored alongside changes in lipophilic metabolites, including untargeted lipids and lipophilic pigments. While few metabolites showed temporal remodeling, rapid and contrasting changes were observed within 30 minutes in response to both spectral quality and light intensity. Red light treatments induced broader remodeling of lipophilic metabolites than blue light, whereas blue light appeared to have a greater impact on photosynthetic parameters. Moreover, red light induced xanthophyll-cycle responses comparable to those observed under blue light at equivalent incident intensity. We discuss these metabolic responses in relation to diatom photoadaptive strategies, placing these findings within the intertidal environmental framework. This work further underlines the importance of understanding rapid metabolic plasticity in coping with light fluctuations, providing new insights into the photoregulatory strategies of natural microphytobenthic communities.

Nitrogen availability is a key factor shaping microbial metabolism, ecological adaptation, and nitrogen cycling in aquatic environments. Members of the genus Vibrio are ubiquitous heterotrophic bacteria in marine and aquaculture ecosystems, yet their responses to different inorganic nitrogen sources remain poorly understood. Here, we systematically compared the growth characteristics, nitrogen transformation capacity, and molecular responses of Vibrio harveyi and Vibrio parahaemolyticus under ammonium (NH4+), nitrate (NO3-), and nitrite (NO2-) conditions using physiological assays, comparative genomic analysis, and transcriptomic profiling. V. harveyi exhibited broader nitrogen utilization capacity and was able to grow under all three nitrogen conditions, whereas V. parahaemolyticus showed a strong preference for NH4+ and limited growth under NO3- and NO2- conditions. Moreover, V. harveyi displayed rapid population expansion accompanied by reduced long-term viability, while V. parahaemolyticus maintained greater population stability. Both species showed NO3- accumulation during growth despite lacking canonical nitrification genes under NH4+ condition, suggesting the potential involvement of non-canonical heterotrophic nitrification processes. Transcriptomic analysis revealed nitrogen source-dependent metabolic specialization in V. harveyi. NH4+ availability promoted motility-associated responses and metabolic overflow, whereas NO3- induced iron acquisition-related pathways and NO2- activated assimilatory nitrite reduction coupled with oxidative stress adaptation. These findings demonstrate that inorganic nitrogen availability drives divergent metabolic and adaptive strategies in Vibrio, providing new insights into their nitrogen metabolic potential and ecological roles in aquatic environments. ImportanceThis study demonstrates that V. harveyi and V. parahaemolyticus exhibit distinct inorganic nitrogen utilization strategies, with V. harveyi displaying broader nitrogen utilization capacity. Transcriptomic and metabolomic analyses revealed that different nitrogen sources drive distinct metabolic and environmental adaptation responses in V. harveyi, including enhanced motility-associated functions and metabolic overflow responses under NH4+ condition, increased iron acquisition pathways under NO3- condition, and activation of assimilatory nitrite reduction coupled with oxidative stress adaptation under NO2- condition. Furthermore, significant nitrate accumulation was observed in both Vibrio strains during ammonium cultivation despite the absence of canonical nitrification genes, suggesting unexplored nitrogen transformation potential in vibrios. This study expands our understanding of how inorganic nitrogen availability shapes microbial adaptation strategies and ecological functions in aquatic environments.

The Southern Ocean harbors diverse marine microbial communities shaped by both local oceanographic conditions and dispersal limitations. However, this knowledge is mainly based on coastal Antarctic sites, whereas circumpolar Antarctic open sea and subantarctic ecosystems remain poorly explored. Here, we characterize marine microbial communities (using 16S rDNA high-throughput sequencing) and marine oceanographic data across two regions: the Subantarctic, involving two localities (the Magellan Strait and the Beagle Channel), and Antarctic open sea, involving two localities (Eastern Indian and Central South Pacific). We found extensive differences across regions and localities, characterized by distinct taxonomic patterns, alpha diversity, microbial composition, and enriched taxa profiles. Despite these differences, Clade Ia, Amylibacter, NS5 marine group, and NS2b marine group exhibited high prevalence across regions. Oceanographic parameters had variable relationships with microbial alpha diversity across regions: Sea surface temperature and salinity had a negative and positive correlation, respectively, in the Magellan Strait during 2024. In the Antarctic region, dissolved oxygen displayed a negative correlation in the Indian Ocean during 2024, whereas salinity displayed a more variable relationship in the Indian Ocean: positively correlated during 2024, while negatively correlated during 2025. Collectively, our results highlight a strong microbiological biogeographic structure in the Southern Ocean, both across broad scales (between Subantarctic and Antarctic regions) and within regions. Furthermore, our results show dynamic relationships between oceanographic variables and marine microbial diversity across Antarctic and Subantarctic regions.

Marine bryozoans harbor diverse microbial communities, but not much is known about specificity of bacterial symbionts towards different hosts. We identified potential symbionts and described overall microbial communities of three marine bryozoans, Aquiloniella scabra, Rhamphostomella bilaminata (Gymnolaemata: Cheilostomatida), and Patinella verrucaria (Stenolaemata: Cyclostomatida), revealing that each species maintains a distinct microbial assemblage that differs both from the surrounding environmental microbiome and from other hosts. Previously, the bryostatin-producing gammaproteobacterial genus "Candidatus Endobugula" was known from only two bryozoan species in the family Bugulidae. Here, we report its first detection in two more cheilostome bryozoans, A. scabra and R. bilaminata, expanding its known host range to two more families.

Antarctica represents a significant, unresolved, and unstable source of methane to the atmosphere. To advance our understanding of the biological filter of methane in Antarctica, here we identify the taxa and functional genes present during methane oxidation in an Antarctic Methane Seep. Methane oxidation was present in all sediments, including in a non seep control site. Using 16S rRNA analysis alongside metagenomics, we found that ANaerobic MEthane oxidizing (ANME) archaea coupled to Sulfate-Reducing Bacteria (SRB), documented as the most important marine methane sink in other locations, were not present. Instead, we observed the presence of denitrification-dependent methane oxidizers, including the anaerobic genus Candidatus Methylomirabilis, alongside the nitrate reducing archaea Candidatus Methanoperedens through short-read metagenomic classification. In addition, we note the presence of multiple aerobic methanotrophs, with a particularly high abundance of the Methylobacter, Methylomonas, and Methyloprofundus genera. Our results support denitrification-mediated methane oxidation and aerobic methanotrophy as the primary potential methane sinks in the Ross Sea. The widespread methane oxidation, including in control sediment, combined with the possibility of anaerobic methane oxidation linked to denitrification rather than sulfate reduction highlights the ubiquity and uniqueness of the Antarctic methane cycle.

Entomopathogenic Nematodes (EPNs) have a great potential to control various insect crop pests, but their ability to perform their entire life-cycle in insects depends on environmental conditions. The insect killing ability of the endosymbiotic bacterial species (i.e., Xenorhabdus) located in the EPNs' gut (Steinernema) has been described for years. More recently, experimental data have suggested that other bacteria species of the nematode microbiota may also contribute to the parasitic success of the EPNs. EPNs and their associated bacteria should therefore be considered as holobionts. Global change, among its many predicted consequences, is expected to increase temperatures which may impair the parasitic success of these EPNs in the insect. Furthermore, higher environmental temperatures could modify the composition of the EPN-associated microbiota and could therefore also contribute to parasitic impairement. Using a S. carpocapsae strain originating from a French orchard, we investigated these hypotheses by experimentally evolving independent EPNs lineages in vivo in the lepidopteran species Galleria mellonella, at elevated and control temperatures. Several life-history traits of the evolved lineages were measured (insect killing ability, EPN emergence rate, EPN reproduction rate), and the bacterial microbiota of the evolved lineages was characterized by a metabarcoding approach. The EPNs' lineages evolved at higher temperature showed impaired emergence rate and their reproduction rate was lower, when compared to lineages evolved at control temperature. The bacterial microbiota composition of these lineages was modified, with particular enrichment in bacteria of the genera Alcaligenes and Pseudomonas. Our results provide new evidence that modification of the environment (here, the abiotic parameter temperature) during several successive generations can modify the parasitic success of EPNs, concomitantly to a change in the microbiota composition. A better understanding of the life-history traits of these EPNs should help improve the biocontrol efficiency in a context of global warming.

Fusarium head blight (FHB) is driven by co-occurring Fusarium species. Yet the molecular bases of their competitive interactions, particularly at the strain level, remain largely unknown. We performed an integrated multi-omic investigation of four Fusarium isolates cultivated in monoculture, self-confrontation (SC) and inter-specific confrontation (C) assays: two Fusarium graminearum strains FgrI349 and FgrPH-1, and two Fusarium avenaceum strains FaveI494 and FaLH03. Light microscopy and quantitative colorimetry revealed marked phenotypic heterogeneity. the F. graminearum strains formed expansive, red-pigmented colonies with rapid radial growth, whereas the F. avenaceum isolates grew more slowly and displayed distinct colony morphologies and pigmentation patterns. Untargeted LC-HRMS detected 1,008 metabolites in monocultures and 938 metabolites in confrontation zones. Species-level chemical signatures were confirmed, and strain-specific metabolite sets were identified, with FaLH03 producing more than 60 % of the metabolites being made exclusively by a single strain, highlighting its exceptionally unique metabolic profile. RNA-seq uncovered extensive transcriptional reprogramming during competition. In self-confrontations, strain-specific differences persisted but no major morphological or metabolic shifts were observed. Inter-specific confrontations elicited partner-dependent responses: FgrI349 up-regulated 1,492 genes against FaveI494 (including secondary-metabolite biosynthesis, oxidoreductase activity and transport) but only 407 genes against FaLH03, while down-regulating secondary-metabolite genes in the conspecific confrontation. Conversely, the F. avenaceum isolates showed opposite trends; FaLH03 strongly repressed ribosome-biogenesis and cell-wall genes while inducing oxidative-metabolism pathways, whereas FaveI494 displayed a modest transcriptional response dominated by down-regulation of cell-division and chromosome-segregation genes. Gene-ontology enrichment highlighted an opponent-specific reversal of the secondary-metabolite biosynthetic process category in F. graminearum: down-regulated in intra-specific confrontation but up-regulated in both inter-specific encounters. Collectively, our results demonstrate that competitive outcomes are shaped more by strain identity than by species identity, with each strain deploying a distinct molecular arsenal, ranging from metabolite-mediated antagonism to targeted transcriptional shutdown, when confronted with a specific opponent. These findings refine our understanding of Fusarium community dynamics and provide a framework for developing strain-targeted biocontrol strategies against FHB.

Quantitative stable isotope probing (qSIP) allows researchers to calculate taxon-specific carbon incorporation from sequencing of natural microbial communities, which can be used as a proxy for metabolic activity rates and subsequently as an input for biogeochemical modeling. While qSIP is widely utilized in soils to investigate the identity and metabolic activity of largely unculturable microbes, the application of qSIP in marine and aquatic ecosystems is more recent. Here, we investigated how bioreactor type (batch vs. chemostat) and carbon substrate complexity (single vs. multiple substrates) affect the incorporation of {superscript 1}3C-labeled glucose into rRNA after 24 hours using excess atomic fraction (EAF) as a proxy for metabolic activity rate. We found that the growth dynamics and community composition of the {superscript 1}3C-incorporating bacteria differed significantly for each treatment. EAF was positively correlated with both 16S gene copy number and a genomic index of copiotrophy in both batch treatments, but not in the chemostat, suggesting that chemostats dampen the competitive advantage of fast-growing copiotrophic taxa. Our results demonstrate that both substrate complexity and experimental regime influence qSIP-derived metabolic activity estimates and provide guidance for future applications of qSIP in aquatic environments.

Corals associate with many bacteria whose evolutionary histories and holobiont roles are unknown due to a lack of genomic resources. An example is the BD1-7 clade, which is found in some microbial metabarcoding libraries of corals and has been speculated to be phototrophic. To evaluate its phylogenetic position and assess its metabolic capabilities, we assembled and annotated the genome of an octocoral associate classified as BD1-7. Its full genome revealed that it instead represents a distinct and divergent clade of widespread coral associates. We propose the name Ca. Steroidedax gorgoniicola for this associate of Swiftia exserta. Unlike the true BD1-7 clade, its genome encoded no pathways to generate ATP from light and instead reveals that it is likely a heterotroph that can degrade steroids, chitin, and collagen as well as produce toxins or antimicrobial compounds and detoxify several reactive oxygen and nitrogen species. In addition, we identified several genes that were likely horizontally transmitted from Endozoicomonadaceae, including transposases and genes involved in virulence and cell adhesion. This work sheds light on the potential role of horizontal genetransfer in the evolution of symbiosis and highlights the importance of obtaining genomes to resolve coral-associated lineages and their metabolic capabilities.

Plasmids contribute to virulence and antimicrobial resistance in Shiga toxin-producing Escherichia coli (STEC). Here, the mobility, gene content, and evolutionary context of four plasmids carried by an O111:H8 STEC strain designated UTAK-22: pUTAK-22.1-MDR, pUTAK-22.2-MDR, pUTAK-22.3-P1, and pUTAK-22.4-pO111 were characterized. Conjugation experiments, phenotype-based selective readouts, and comparative genomics together showed that pUTAK-22.1-MDR is self-transmissible, whereas pUTAK-22.2-MDR and pUTAK-22.4-pO111 are most consistent with mobilization in trans, making use of the strain's native helper plasmid background, while pUTAK-22.3-P1 represents a conjugation-deficient IncY phage-derived replicon. Genome annotation and comparative analyses further highlighted the structural diversity and mosaic composition of these plasmids, including P1-like phage remnants, virulence loci, and distinct antimicrobial resistance modules. Phenotypic profiling of the native wild-type plasmid complement and selected transconjugants in the recipient E. coli strain WG5 further showed that the presence of co-resident plasmids and redundant resistance determinants results in dosage-dependent streptomycin tolerance. Together, these findings expand our understanding of the mobility landscape, evolutionary dynamics, and resistance potential of STEC plasmids, while underscoring the importance of interpreting resistance phenotypes in the context of a strain's natural plasmid composition.

Sinorhizobium meliloti is a nitrogen-fixing soil bacterium that forms a facultative mutualism with its host alfalfa. S. meliloti strains exhibit diverse colony morphologies on solid culture media that span a continuum from dry to mucoid. Studies on how this trait affects symbiosis rely on mutations in exopolysaccharide II production genes; however, whether natural variation in morphology confers a selective advantage on rhizobia in their natural habitats remains unknown. Here, we used 90 mucoid and 27 dry natural isolates to test whether colony morphology is associated with rhizobial fitness in the soil and in the host, or with the nitrogen-fixation benefits they provide to the plant. Colony morphologies were widely distributed across a phylogenetic tree, suggesting that morphological shifts occurred repeatedly and no single genetic variant was strongly associated with this trait. We inoculated soil mesocosms and plants with a mixture of dry and mucoid bacteria. We observed that dry rhizobia have higher fitness, particularly at 22{degrees}C and 32{degrees}C, but not under cold or drought conditions, independent of the initial rhizobial load. Conversely, mucoid bacteria have a modestly higher relative fitness in host nodules, and single inoculations showed that they tend to confer greater benefits to all three alfalfa varieties. Over time, we also observed rare, repeated conversion from mucoid to dry morphologies in soil and host plants. Taken together, our study reveals that morphological variation within a species in a single agricultural field is important for bacterial fitness in the soil and can have cascading effects on the rhizobia's plant benefits.

Stratified benthic deposits offer crucial modern analogs for Precambrian biogeochemical dynamics, yet whether the vertical organization of deep sedimentary columns reflects depositional history, present-day geochemical conditions, or both remains poorly understood, particularly under extreme oligotrophy. Here, we present a depth-resolved exploratory survey of a continuous 34-cm sediment core partitioned into 11 discrete horizons (L1 to L11) from Poza Roja 2, an alkaline, sub-hypersaline pond in the Cuatro Cienegas Basin, Mexico. Integrating physical stratigraphy, organic carbon and nutrient stoichiometry, and 16S rRNA gene metabarcoding, we evaluated down-core microbial community structure alongside acute phosphorus scarcity. Molar C:Po and N:Po ratios exceeded canonical Redfield proportions (106:16:1) in every layer, by up to 48.5-fold and 87.8-fold, respectively, both peaking in layer L4. Unconstrained ordination (PCoA) and hierarchical clustering grouped the layers into three compositional zones: upper (L2-L4), intermediate (L5-L6), and basal (L8-L11), with L1 and L7 occupying transitional positions. Archaea accounted for 31.0% of prokaryotic reads, ranging from 8.3% (L5) to 43.7% (L9), and were dominated by SM1-50 (Thermoplasmatota) and Halobacteriota. The phototrophic heliobacterium Heliorestis peaked in the intermediate zone (47.6% of bacterial reads in L6). Constrained Redundancy Analysis models lacked statistical significance (P >= 0.12), highlighting the exploratory nature of a single core (n = 11). This pilot characterization provides a baseline for understanding deep biogenic archives under severe nutrient limitation.

Accelerated retreat of the Greenland Ice Sheets is increasing freshwater discharge to coastal fjords and promoting transitions from marine-terminating glacier (MTG) regimes to land-terminating (LTG) ones. These changes strongly affect the physical and chemical features of the water column, which in turn impact the structure and functioning of fjord ecosystems. We used high-throughput imaging and DNA metabarcoding approaches to investigate seasonal (spring vs summer) differences in the structure of pelagic microbial communities in two contrasting fjord systems (MTG vs LTG) in southwest Greenland, with focus on the bacterial and heterotrophic protist components, which to date remain understudied in Greenland fjords. Our analyses revealed a marked seasonal restructuring in the microbial communities, especially in the surface layers. In spring, heterotrophic community composition in both fjords manifested a strong link with the diatom spring bloom, being dominated by typical phytoplankton-associated and copiotroph bacterial groups that can utilize algal-derived organic matter, and protists grazing on phytoplankton. In summer, heterotroph communities strongly diverged between the two fjords, most likely caused by the differential impact of MTG vs LTG glaciers on water column structure and chemistry. There was a marked increase in pico- and nano-sized heterotrophs, parasitic protists (dinoflagellate Syndiniales), and bacterial groups indicative of low-nutrient environments. In addition, bacterial, phytoplankton and heterotrophic protist communities become more strongly coupled, either through stronger interactions and/or stronger environmental filtering acting on all groups simultaneously. These observations are indicative of a shift from resource-replete systems in spring to more resourced-depleted systems in summer. However, this shift was less pronounced in the MTG fjord, where subglacial upwelling enabled the persistence of diatom bloom related communities into summer. Finally, we uncovered the presence of a unique, ice melange associated inner fjord microbial community, which shows similarities with both supraglacial and sea-ice associated communities, in the inner part of the MTG impacted fjord.

The Eboliang Hu saline lakes in the hyper-arid Qaidam Basin is a high-altitude, weakly acidic hypersaline system with strong environmental gradients and limited nitrogen availability. To resolve its microbial ecology and evolutionary context, we performed genome-resolved metagenomic sequencing across four distinct habitats, reconstructing 46 medium- to high-quality metagenome-assembled genomes (MAGs) and a comprehensive gene catalog. The community shows pronounced spatial heterogeneity and is dominated by Thermodesulfobacteriota, Pseudomonadota, Bacteroidota, and archaeal lineages. Phylogenomic placement and large-scale sequence comparisons indicate that multiple dominant taxa exhibit affinity to marine- and subsurface-associated reference lineages, consistent with long-term isolation of a marine-derived ecosystem about 10-11 million years ago. Functional reconstruction reveals a distributed metabolic system in which carbon, nitrogen, and sulfur cycling are partitioned across taxa. Notably, hydrogen oxidation and arsenite oxidation are recurrent energy-producing strategies across dominant lineages, indicating redox flexibility under oligotrophic conditions. Comparative genomics further suggests lineage-specific adaptations to osmotic stress, UV exposure, and nutrient limitation. Horizontal gene transfer and phylogenetic incongruence among key metabolic genes indicate that co-evolutionary processes and gene exchange have contributed to functional innovation. These findings provide a framework for understanding microbial persistence and evolution in isolated extreme environments and offer potential analogs for extraterrestrial habitability.

The haloalkaline maar lake at Rincon de Parangueo, in central Mexicos volcanic belt, is a doubly extreme habitat where high salinity and high alkalinity co-occur. Unlike the long-lived soda lakes that dominate the literature, it is a young system undergoing rapid desiccation, its salinity and pH intensifying over decades. Its microbes have been surveyed only by 16S amplicons, with no genome or mobilome reported from the site, and the wider soda-lake mobilome is known almost entirely from host-unlinked, short-read viromes. Using long-read sequencing, we recovered high-quality genomes for six isolates that dereplicate to three independent, bona fide haloalkaliphilic lineages spanning two distant families (Halomonadaceae, Bacillaceae). Each lineages closest relative is not its type strain but an isolate from another distant extreme habitat, including two other Mexican hypersaline systems. All three are aerobic, facultatively fermentative heterotrophs that meet high pH and salinity with the canonical toolkit -- multisubunit Mrp/Mnh Na+/H+ antiporters and a "salt-out" compatible-solute strategy -- whose distribution tracks phylogeny, with only complementary lineage-specific elaboration. In contrast, the isolates carry an unexpectedly rich and apparently active mobilome: a novel plasmid, multiple intact prophages, and multiple other mobile genetic elements alongside an above-average antiviral defense arsenal, including an 89-spacer CRISPR array. Horizontal transfer is thus likely active at Rincon de Parangueo but is not the vehicle of haloalkaliphily. Intensifying extremes like this one are tractable natural laboratories for dissecting how inherited toolkits and recent innovation shape microbial survival at the limits of life.

Subcuticular bacteria (SCB) are widespread symbionts of echinoderms and often dominate the body-wall microbiome, suggesting important roles in host physiology. However, their diversity, metabolic properties, and host associations remain poorly characterized. Here, we report a novel dominant SCB lineage associated with deep-sea holothurians, Scotoplanes spp. collected from the Northwest Pacific. We recovered two high-quality genomes, including a 649-kb complete circular genome, and propose a new genus and species, "Candidatus Abyssoplasma scotoplanesicola", within Mycoplasmatota. The two genomes showed a highly reduced metabolic repertoire, lacking central pathways including glycolysis. In contrast, acidic cell-surface-associated proteins, including large proteins exceeding 5,000 amino acids, accounted for 27.6% of the complete genome and clustered near defense islands. Localized genome plasticity in these regions, revealed by comparison between the two closely related genomes, suggests a possible mechanism for diversification of cell-surface proteins at the host-symbiont interface. "Candidatus Abyssoplasma scotoplanesicola" occupied 76.4-98.9% of the body-wall microbiome of the Scotoplanes specimens. Fluorescence in situ hybridization analysis confirmed that these bacteria formed aggregates on the epidermal side of the body wall. Overall, this study provides genome-and spatially resolved views of dominant SCB in holothurians and offers evolutionary insights into host-interface diversification in the deep-sea holothurian body wall.

Fucoidan is the second most abundant polysaccharide in brown macroalgae, contributing up to 50% of the dissolved organic matter released daily from these algae into the ocean, substantially influencing the marine carbon cycle. Due to its complex chemical structure, fucoidan is highly resistant to microbial degradation and accumulates on the surface of macroalgae, where it contributes to regulating their microbiome. Here, we used a range of microfluidic assays to quantify the chemotactic and physiological responses of marine bacteria to fucoidan. Our results reveal that all the strains tested (14 out of 14) are attracted to fucoidan produced by two different species of brown macroalgae. Attraction occurred only at high fucoidan concentrations (0.1 to 1 mg/mL), such as those expected in the immediate vicinity of algal surfaces, whereas low concentrations elicited no response or modest chemorepulsion. Although fucoidan did not support bacterial growth under our experimental conditions, it did not impair the utilization of other carbon sources. Together, these findings suggest that fucoidan gradients can act as chemical cues guiding marine bacteria toward the nutrient-rich microenvironment of macroalgal surfaces, pointing to a potential ecological role of fucoidan in shaping macroalgal microbiota, bacterial behavior, and ultimately carbon cycling in the ocean.

The foundation of coral reef ecosystems centered around the nutritional relationship between corals and intracellular algal symbionts. Although these symbioses are highly obligate for coral hosts, many partnerships are re-established anew with each coral generation. Furthermore, climate change destabilizes the symbiosis, and the cellular mechanisms underlying successful symbiont colonization of hosts and host development, and how they are affected by thermal stress are poorly understood. Here, we explored the effect of algal species and thermal treatments on symbiont and host cell proliferation by offering Acropora tenuis larvae one of four algal species pre-exposed to elevated or ambient temperature. In addition, we characterized the cell-surface glycome of each species-temperature combination to understand its role in symbiont recognition and proliferation. We found that thermal pre-treatment negatively affected algal photosynthetic efficiency and initial symbiont density in hosts, but did not affect symbiont colonization rate or cell proliferation. In contrast, host cell proliferation was affected in a species-specific manner. Thermal pre-treatment of B. minutum and D. trenchii negatively affected host cell proliferation compared to control symbionts, whereas thermal treatment of S. microadriaticum did not affect developmental outcomes. Further, uptake of thermally pre-treated D. trenchii decreased host cell proliferation below that of larvae not offered any symbionts, indicating that this relationship is costly to host development despite the high thermal tolerance of this species. Algal surface glycan composition varied across species but not by thermal pre-treatment, suggesting reductions in density of thermally pre-treated algae may be due to changes in physiology rather than altered surface chemistry. Further, variation in glycan abundance across species did not track differences in colonization rate or symbiont density, hinting towards a smaller role of glycans in host-symbiont specificity.