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Ghosh, W.

Publications and source records attributed to Ghosh, W..

13 recordsLinked to original sources

Boron-induced microbial filtering delays early rhizosphere establishment in agricultural soil

Excessive application of boron-based fertilizers in agriculture has led to increased boron accumulation in soil, adversely affecting microbial communities and plant species, ultimately contributing to boron-induced desertification. This study presents the first metagenome-based analysis of boron-contaminated agricultural soil in Northern West Bengal, India, providing a comprehensive profile of the soil microbiome under boron stress. Boron-amended and unamended agricultural soil samples were analyzed using metagenomics sequencing approach over 365 days under natural environmental conditions. The results revealed a significant decline in bacterial diversity in boron-amended soil, with Firmicutes emerging as the dominant phylum. Notably, all boron-tolerant bacterial strains belonged to Firmicutes, suggesting that high boron levels impose selective pressure favouring Gram-positive bacteria. The enrichment of metal-resistant and oligotrophic bacterial taxa in boron-amended soil underscores microbial adaptation to boron stress. In addition to microbial community dynamics, we investigated plant succession in boron-enriched soil, offering novel insights into the interplay between above- and below-ground ecosystems. Our findings highlight two key adaptive traits, high boron tolerance and oligotrophic survival strategies, that enable bacterial communities to persist in boron-rich environments. These results enhance our understanding of microbial resilience in chemically stressed soils and have implications for soil health and sustainable agriculture.

microbiology↗

Convergent genomic variation and wild-type composite RNA-seq profiling identify candidate modules associated with 3-nitropropionic acid utilization in Leclercia barmai

3-Nitropropionic acid (3-NPA) is a toxic nitroaliphatic compound, but the genomic basis of bacterial adaptation to 3-NPA remains incompletely resolved, especially in organisms lacking a canonical nitronate monooxygenase. Here, we used phenotype screening, whole-genome resequencing, targeted UHPLC-MS/MRM, and composite RNA-seq profiling to investigate 3-NPA utilization in Leclercia barmai EMC7. Following attempted Tn5-Mob mutagenesis and kanamycin-based recovery, two independently derived mutants, LTM01 and LTM14, showed impaired growth under 3-NPA-dependent minimal conditions. No stable transposon insertion was detected in either mutant. Comparative genome analysis instead revealed convergent loss-of-function (LOF) mutations affecting amino acid metabolism, nitrogen allocation, central carbon metabolism, cofactor-linked functions, transport, and metal-redox homeostasis, while the predicted flavin-dependent nitro-redox candidate and canonical nitrate/nitrite reduction loci were not disrupted. Targeted UHPLC-MS/MRM analysis showed that wild-type EMC7 depleted approximately 50% of 3-NPA within 36 h, whereas the mutants displayed poor 3- NPA-utilization phenotypes under the same growth framework. Wild-type RNA-seq under glucose-3NPA relative to glucose-KNO3 identified a broad expression profile involving flavin-redox functions, nitrogen assimilation, oxidative-stress response, envelope stress, efflux, cofactor metabolism, and iron homeostasis. Integration of mutant LOF profiles with wild-type gene expression data showed that several disrupted genes or functional counterparts belonged to modules showing expression changes during the wild-type glucose-3NPA response. These findings identify candidate adaptive modules associated with 3-NPA utilization in EMC7, including nitrogen redistribution, carbon entry, sulfur-redox support, cofactor supply, transport, envelope remodeling, and metal-redox control. These results extend the landscape of metabolic adaptation beyond canonical pathways in environmental bacteria.

microbiology↗

Sustained presence of metabolically active mesophiles in the boiling vent-water of a low-salinity, slightly-alkaline, sulfate-rich geothermal spring characterized by an inequitable ecology of hyperthermophiles and thermophiles

Geothermal vent-heads exclusively support the proliferation of (hyper)thermophilic microorganisms. However, diverse mesophiles are stochastically thrust into these ecosystems by local geodynamic forces, and their population-level responses to the unfamiliar stressor hold critical implications for lifes intrinsic resilience to biophysical adversities. Here, we report a time-course exploration of the boiling vent-water of a Trans-Himalayan geothermal spring to determine the population dynamics, in situ functionalities, and potential ecological roles of mesophilic incomers in the context of indigenous (hyper)thermophiles. The temporally-consistent (hyper)thermophilic core-community, predominated in turn by a few Aquificia and Thermoproteota, was delineated as metagenome-assembled genomes. Mesophiles/moderate-thermophiles were identified as MAGs and/or pure-cultures, and whether temporally-consistent/inconsistent, had far lower prevalence. Overall, in situ transcriptional activity and prevalence had significant positive correlation; but many species exhibited high activity despite low prevalence and vice versa, implicating the decoupling of global metabolism from growth/proliferation. Bulked metatranscriptomic signatures identified the (hyper)thermophiles as primary producers of the ecosystem. Populations of mesophiles and moderate-thermophiles were apparently active, but not growing, in situ, with some being engaged in environment detoxification, and production of nutrients, metabolites and protective-biomolecules wanting in the (hyper)thermophiles. The findings engender an unprecedented portrayal of geothermal-vents as multi-community ecosystems where unfamiliar immigrants provide critical metabolic services.

microbiology↗

Psychrophilic and cryophilic bacterial copiotrophs from a Trans-Himalayan lake-desert ecosystem as biogeothermometers of warming, mitigators of perturbation, and candidates for biodegradation

A Trans-Himalayan lake-desert ecosystem was explored for the low-to-high temperature adaptations of native copiotrophic psychrophiles that have the potentials for rendering substantive carbon remineralization under natural and/or anthropogenically influenced conditions of high organic matter delivery to the environment. Overall 27 species, classified across 15 genera of Actinomycetota, Bacillota, Bacteroidota, and Pseudomonadota, were isolated from the brackish-water and sediment-surface of Tso Moriri (a massive lacustrine body on the Changthang plateau that remains frozen for approximately one third of the year), and the fine talus covering a lake-side rocky mountain. In Luria broth, all the isolates grew at 4{degrees}C and 15{degrees}C; 13 of them grew, while 14 retained 19-99% cells in metabolically-active state, at -10{degrees}C; 23, 11, and none grew at 28{degrees}C, 37{degrees}C, and 42{degrees}C respectively. A Cryobacterium was most heat-susceptible, whereas some -10{degrees}C-growing Arthrobacter, Microbacterium, Paenarthrobacter, Pseudomonas and Streptomyces were most warming-resilient, among the present isolates. Catabolizing different simple/complex organic compounds, all isolates accomplished low/moderate/high growths at 4{degrees}C; 20 performed low growths at -10{degrees}C. Taxonomy/phylogeny did not determine the isolates growth/survival across the temperature-range tested. Lake-water and rock-dust isolates had the widest, while lake-sediment-dwellers had the narrowest, temperature-window for growth/survival. Rock-dust and lake-water isolates had more genes for low and high temperature adaptations, compared to the lake-sediment isolates. In co-cultures, most actinobacterial isolates inhibited the growth of mesophilic bacteria from warmer ecosystems, plus non-actinobacteria and actinobacteria from native/adjoining habitats. The data hold implications for biodegradation in cold/frigid territories, negative feedback control/reversal of warming, and microbiome protection from infiltration amidst climate change. IMPORTANCEPhylogenetically diverse, cold-adapted copiotrophic bacteria were retrieved from a Trans-Himalayan lake-desert ecosystem, and tested for chemoorganoheterotrophic growth at temperatures between -10{degrees}C and 42{degrees}C. Albeit growth dwindled at [≥]28{degrees}C, most of the isolates thrived on simple as well as complex organic substances under freezing condition, which makes them prospective constituents of biodegradation reactors suitable for high-altitude/latitude deployment. In the natural habitats of the psychrophilic isolates, cessation of organotrophic activities at elevated temperatures would stop simple fatty acids and CO2 production, which in turn would preempt methanogenesis, undo greenhouse effect, and reverse environmental thawing (usher cooling). Such negative feedback control of homeostasis is fraught with the danger of microbiome takeover by thermally-better-adapted foreign organisms. Consequently, ecosystem preservation rests on the native microfloras ability to resist external invasion. At 28{degrees}C, majority of the actinobacterial isolates inhibited bacteria from discrete higher-temperature ecosystems; they can, therefore, be viewed as the defenders of the cold/frigid ecosystem.

microbiology↗

Extremely oligotrophic and complex organic compounds degrading microaerobic bacteria from Arabian Sea oxygen minimum zone sediments

Sediments underlying marine hypoxic zones are huge sinks of unreacted complex organic matter, where despite acute O2-limitation obligately aerobic bacteria thrive, and steady depletion of organic carbon takes place within a few meters below the seafloor. However, little knowledge exists about the sustenance and complex carbon degradation potentials of aerobic chemoorganotrophs in these sulfidic ecosystems. We isolated and characterized a number of aerobic bacterial chemoorganoheterotrophs from across a [~]3 m sediment horizon underlying the perennial hypoxic zone of the eastern Arabian Sea. High levels of sequence correspondence between the isolates genomes and the habitats metagenomes and metatranscriptomes illustrated that the strains were widespread and active across the sediment-cores explored. The isolates catabolized several complex organic compounds of marine and terrestrial origins in the presence of high or low, but not zero, O2. Some of them could also grow anaerobically on yeast extract or acetate by reducing nitrate and/or nitrite. Fermentation did not support growth, but enabled all the strains to maintain a fraction of their cell populations over prolonged anoxia. Under extreme oligotrophy, limited growth followed by protracted stationary phase was observed for all the isolates at low cell density, amid high or low, but not zero, O2 concentration. While population control and maintenance could be particularly useful for the strains survival in the critically carbon-depleted layers below the explored sediment-depths (core-bottom organic carbon: 0.5-1.0 % w/w), metagenomic data suggested that in situ anoxia could be surmounted via potential supplies of cryptic O2 from previously-reported sources such as Nitrosopumilus species.

microbiology↗

High diversity of Proteobacteria amid the dominance of a few Aquificae species in the vent-water of a Trans-Himalayan sulfur-borax hot spring

Trans-Himalayan hot spring waters rich in boron, chlorine, sodium and sulfur (but poor in calcium and silicon) are known based on PCR-amplified 16S rRNA gene sequence data to harbor high diversities of infiltrating bacterial mesophiles. Yet, little is known about the community structure and functions, primary productivity, mutual interactions, and thermal adaptations of the microorganisms present in the steaming waters discharged by these geochemically peculiar spring systems. We revealed these aspects of a bacteria-dominated microbiome (microbial cell density [~]8.5 x 104 mL-1; live:dead cell ratio 1.7) thriving in the boiling (85{degrees}C) fluid vented by a sulfur-borax spring called Lotus Pond, situated at 4436 m above the mean sea-level, in the Puga valley of eastern Ladakh, on the Changthang plateau. Assembly, annotation, and population-binning of >15-GB metagenomic sequence illuminated the numeral predominance of Aquificae. While members of this phylum accounted for 80% of all 16S rRNA-encoding reads within the metagenomic dataset, 14% of such reads were attributed to Proteobacteria. Post assembly, only 25% of all protein-coding genes identified were attributable to Aquificae, whereas 41% was ascribed to Proteobacteria. Annotation of metagenomic reads encoding 16S rRNAs, and/or PCR-amplified 16S rRNA genes, identified 163 bacterial genera, out of which 66 had been detected in past investigations of Lotus Ponds vent-water via 16S amplicon sequencing. Among these 66, Fervidobacterium, Halomonas, Hydrogenobacter, Paracoccus, Sulfurihydrogenibium, Tepidimonas, Thermus and Thiofaba (or their close phylogenomic relatives) were presently detected as metagenome-assembled genomes (MAGs). Remarkably, the Hydrogenobacter related MAG alone accounted for [~]56% of the entire metagenome, even though only 15 out of the 66 genera consistently present in Lotus Ponds vent-water have strains growing in the laboratory at >45{degrees}C, reflecting the continued existence of the mesophiles in the ecosystem. Furthermore, the metagenome was replete with genes crucial for thermal adaptation in the context of Lotus Ponds geochemistry and topography. In terms of sequence similarity, a majority of those genes were attributable to phylogenetic relatives of mesophilic bacteria, while functionally they rendered functions such as encoding heat shock proteins, molecular chaperones, and chaperonin complexes; proteins controlling/modulating/inhibiting DNA gyrase; universal stress proteins; methionine sulfoxide reductases; fatty acid desaturases; different toxin-antitoxin systems; enzymes protecting against oxidative damage; proteins conferring flagellar structure/function, chemotaxis, cell adhesion/aggregation, biofilm formation, and quorum sensing. The Lotus Pond Aquificae not only dominated the microbiome numerically but also acted potentially as the main primary producers of the ecosystem, with chemolithotrophic sulfur oxidation (Sox) being the fundamental bioenergetic mechanism, and reductive tricarboxylic acid (rTCA) cycle the predominant carbon fixation pathway. The Lotus Pond metagenome contained several genes directly or indirectly related to virulence functions, biosynthesis of secondary metabolites including antibiotics, antibiotic resistance, and multi-drug efflux pumping. A large proportion of these genes being attributable to Aquificae, and Proteobacteria (very few were ascribed to Archaea), it could be worth exploring in the future whether antibiosis helped the Aquificae overcome niche overlap with other thermophiles (especially those belonging to Archaea), besides exacerbating the bioenergetic costs of thermal endurance for the mesophilic intruders of the ecosystem.

genomics↗

Thermal endurance by a hot-spring-dwelling phylogenetic relative of the mesophilic Paracoccus

High temperature growth/survival was revealed in a phylogenetic relative (strain SMMA_5) of the mesophilic Paracoccus isolated from the 78-85{degrees}C water of a Trans- Himalayan sulfur-borax spring. After 12 h at 50{degrees}C, or 45 minutes at 70{degrees}C, in mineral salts thiosulfate (MST) medium, SMMA_5 retained [~]2% colony-forming units (CFUs), whereas comparator Paracoccus had 1.5% and 0% CFU left at 50{degrees}C and 70{degrees}C respectively. After 12 h at 50{degrees}C, the thermally-conditioned sibling SMMA_5_TC exhibited [~]1.5 time increase in CFU-count; after 45 minutes at 70{degrees}C, SMMA_5_TC had 7% of the initial CFU-count intact. 1000-times diluted Reasoners 2A medium, and MST supplemented with lithium, boron or glycine-betaine (solutes typical of the SMMA_5 habitat), supported higher CFU-retention/CFU-growth than MST. With or without lithium/boron/glycine-betaine in MST, a higher percentage of cells always remained viable (cytometry data), compared with what percentage remained capable of forming single colonies (CFU data). SMMA_5, compared with other Paracoccus, contained 335 unique genes, mostly for DNA replication/recombination/repair, transcription, secondary metabolites biosynthesis/transport/catabolism, and inorganic ion transport/metabolism. Its also exclusively enriched in cell wall/membrane/envelope biogenesis, and amino acid metabolism, genes. SMMA_5 and SMMA_5_TC mutually possessed 43 nucleotide polymorphisms, of which 18 were in protein-coding genes with 13 nonsynonymous and seven radical amino acid replacements. Such biochemical and biophysical mechanisms could be involved in thermal stress mitigation which streamline the cells energy and resources towards system-maintenance and macromolecule-stabilization, thereby relinquishing cell-division for cell-viability. Thermal conditioning apparently helped memorize those potential metabolic states which are crucial for cell-system maintenance, while environmental solutes augmented the indigenous stability-conferring mechanisms. IMPORTANCEFor a holistic understanding of microbial lifes high-temperature adaptation it is imperative to explore the biology of the phylogenetic relatives of mesophilic bacteria which get stochastically introduced to geographically and geologically diverse hot spring systems by local geodynamic forces. Here, in vitro endurance of high heat up to the extent of growth under special (habitat-inspired) conditions was discovered in a hot- spring-dwelling phylogenetic relative of the mesophilic Paracoccus species. Thermal conditioning, extreme oligotrophy, metabolic deceleration, presence of certain habitat- specific inorganic/organic solutes, and typical genomic specializations were found to be the major enablers of this conditional (acquired) thermophilicity. Feasibility of such phenomena across the taxonomic spectrum can well be paradigm-changing for the established scopes of microbial adaptation to the physicochemical extremes. Applications of conditional thermophilicity in microbial process biotechnology may be far reaching and multi-faceted.

microbiology↗

Sedimentation rate and organic matter dynamics shape microbiomes across a continental margin

Marine sedimentation rate and bottom-water O2 concentration control the remineralization/sequestration of organic carbon across continental margins; but whether/how they shape microbiome architecture (the ultimate effector of all biogeochemical phenomena), across shelf/slope sediments, is unknown. Here we reveal distinct microbiome structures and functions, amidst comparable pore-fluid chemistries, along ~3 m sediment-horizons underlying the seasonal (shallow coastal) and perennial (deep sea) oxygen minimum zones (OMZs) of the Arabian Sea, situated across the western-Indian margin (water-depths: 31 m and, 530 and 580 m, respectively). Along the perennial- and seasonal-OMZ sediment-cores microbial communities were predominated by Gammaproteobacteria/Alphaproteobacteria and Euryarchaeota/Firmicutes respectively. As a perennial-OMZ signature, a cryptic methane production-consumption cycle was found to operate near the sediment-surface; overall diversity, as well as the relative abundances of simple-fatty-acids-requiring anaerobes (methanogens, anaerobic methane-oxidizers, sulfate-reducers and acetogens), peaked in the topmost sediment-layer and then declined via synchronized fluctuations until the sulfate-methane transition zone was reached. The entire microbiome profile was reverse in the seasonal-OMZ sediment-horizon. We discerned that in the perennial-OMZ sediments organic carbon deposited was higher in concentration, and marine components-rich, so it potentially degraded readily to simple fatty acids; lower sedimentation rate afforded higher O2 exposure time for organic matter degradation despite perennial hypoxia in the bottom-water; thus, the resultant abundance of reduced metabolites sustained multiple inter-competing microbial processes in the upper sediment-layers. Remarkably, the whole geomicrobial scenario was opposite in the sediments of the seasonal/shallow-water OMZ. Our findings create a microbiological baseline for understanding carbon-sulfur cycling across distinct marine depositional settings and water-colum n oxygenation regimes.

microbiology↗

Metabolically-active obligate aerobes in anoxic (sulfidic) marine sediments

Metabolically-active obligate aerobes are unheard-of in tightly-anoxic environments. Present culture-independent and culture-dependent investigations revealed aerobic microbial communities along two, ~3-meter-long sediment-cores underlying the eastern Arabian Sea oxygen minimum zone, where high H2S disallows O2 influx from the water-column. While genes for aerobic respiration by aa3-/cbb3-type cytochrome-c oxidases and cytochrome-bd ubiquinol oxidase, and aerobic oxidation of methane/ammonia/alcohols/thiosulfate/sulfite/organosulfur-compounds, were present across the cores, so were live aerobic, sulfur-chemolithoautotrophs and chemoorganoheterotrophs. The 8820-years-old, highly-sulfidic, methane-containing sediment-sample from 275 cmbsf of 530 mbsl yielded many such obligately-aerobic bacterial-isolates that died upon anaerobic incubation with alternative electron-acceptors/fermentative-substrates. Several metatranscriptomic reads from this sediment-sample matched aerobic-respiration-/oxidase-reaction-/transcription-/translation-/DNA-replication-/membrane-transport-/cell-division-related genes of the obligately-aerobic isolates, thereby corroborating their active aerobic metabolic-status in situ. Metagenomic and metatranscriptomic detection of perchlorate-/chlorate-reduction genes, plus anaerobic growth of an obligately-aerobic Halothiobacillus isolate in the presence of perchlorate and perchlorate-reducing-consortia, suggested that cryptic O2 produced by perchlorate-respirers could be sustaining obligately-aerobes in this environment.

microbiology↗

Molecular mechanism of sulfur chemolithotrophy in the betaproteobacterium Pusillimonas ginsengisoli

Molecular mechanism of chemolithotrophic sulfur oxidation in Betaproteobacteria is less explored than that in Alphaproteobacteria. Here we carried out whole genome sequencing and analysis of a new betaproteobacterial isolate Pusillimonas ginsengisoli SBSA which oxidizes thiosulfate via formation tetrathionate as an intermediate. The 4.7-Mb SBSA genome was found to encompass a complete soxCDYZAXOB operon, plus one thiosulfate dehydrogenase (tsdA) and sulfite:acceptor oxidoreductase (sorAB) genes. Recombination-based knock-out of tsdA revealed that the entire thiosulfate oxidized by SBSA is first converted to tetrathionate, and no thiosulfate is directly converted to sulfate as typical of the Alphaproteobacterial Sox pathway whereas its tetrathionate-oxidizing ability was as good as that of the wild-type. The {triangleup}soxYZ knock-out mutant exhibited wild-type-like phenotype for thiosulfate/tetrathionate oxidation, whereas {triangleup}soxB oxidized thiosulfate only up to tetrathionate and had complete impairment of tetrathionate oxidation. However, substrate-dependent O2-consumption rate of whole cells, and sulfur-oxidizing enzyme activities of cell-free extracts, measured in the presence/absence of thiol-inhibitors/glutathione, indicated that glutathione plays a key role in SBSA tetrathionate oxidation. All the present findings collectively indicated that glutathione:tetrathionate coupling in Pusillimonas ginsengisoli may involve some unknown proteins other than thiol dehydrotransferase(ThdT), while subsequent oxidation of the potential glutathione:sulfodisulfane and sulfite molecules produced may proceed via soxBCD action.

microbiology↗

Cryptic role of tetrathionate in the sulfur cycle: A study from Arabian Sea oxygen minimum zone sediments

To explore the potential role of tetrathionate in the sulfur cycle of marine sediments, the population ecology of tetrathionate-forming, oxidizing, and respiring microorganisms was revealed at 15-30 cm resolution along two, [~]3-m-long, cores collected from 530- and 580-mbsl water-depths of Arabian Sea, off Indias west coast, within the oxygen minimum zone (OMZ). Metagenome analysis along the two sediment-cores revealed widespread occurrence of the structural genes that govern these metabolisms; high diversity and relative-abundance was also detected for the bacteria known to render these processes. Slurry-incubation of the sediment-samples, pure-culture isolation, and metatranscriptome analysis, corroborated the in situ functionality of all the three metabolic-types. Geochemical analyses revealed thiosulfate (0-11.1 M), pyrite (0.05-1.09 wt %), iron (9232-17234 ppm) and manganese (71-172 ppm) along the two sediment-cores. Pyrites (via abiotic reaction with MnO2) and thiosulfate (via oxidation by chemolithotrophic bacteria prevalent in situ) are apparently the main sources of tetrathionate in this ecosystem. Tetrathionate, in turn, can be either converted to sulfate (via oxidation by the chemolithotrophs present) or reduced back to thiosulfate (via respiration by native bacteria); 0-2.01 mM sulfide present in the sediment-cores may also reduce tetrathionate abiotically to thiosulfate and elemental sulfur. Notably tetrathionate was not detected in situ - high microbiological and geochemical reactivity of this polythionate is apparently instrumental in the cryptic nature of its potential role as a central sulfur cycle intermediate. Biogeochemical roles of this polythionate, albeit revealed here in the context of OMZ sediments, may well extend to the sulfur cycles of other geomicrobiologically-distinct marine sediment horizons.

microbiology↗

Two pathways for thiosulfate oxidation in the alphaproteobacterial chemolithotroph Paracoccus thiocyanatus SST

Chemolithotrophic bacteria oxidize various sulfur species for energy and electrons, thereby operationalizing biogeochemical sulfur cycles in nature. The best-studied pathway of bacterial sulfur-chemolithotrophy, involving direct oxidation of thiosulfate to sulfate (without any free intermediate) by the SoxXAYZBCD multienzyme system, is apparently the exclusive mechanism of thiosulfate oxidation in facultatively chemolithotrophic alphaproteobacteria. Here we explore the molecular mechanisms of sulfur oxidation in the thiosulfate- and tetrathionate-oxidizing alphaproteobacterium Paracoccus thiocyanatus SST, and compare them with the prototypical Sox process characterized in Paracoccus pantotrophus. Our results revealed the unique case where, an alphaproteobacterium has Sox as its secondary pathway of thiosulfate oxidation, converting [~]10% of the thiosulfate supplied whilst 90% of the substrate is oxidized via a Tetrathionate-Intermediate pathway. Knock-out mutation, followed by the study of sulfur oxidation kinetics, showed that thiosulfate-to-tetrathionate conversion, in SST, is catalyzed by a thiosulfate dehydrogenase (TsdA) homolog that has far-higher substrate-affinity than the Sox system of this bacterium, which, remarkably, is also less efficient than the P. pantotrophus Sox. soxB-deletion in SST abolished sulfate-formation from thiosulfate/tetrathionate while thiosulfate-to-tetrathionate conversion remained unperturbed. Physiological studies revealed the involvement of glutathione in SST tetrathionate oxidation. However, zero impact of the knock-out of a thiol dehydrotransferase (thdT) homolog, together with no production of sulfite as an intermediate, indicated that tetrathionate oxidation in SST is mechanistically novel, and distinct from its betaproteobacterial counterpart mediated by glutathione, ThdT, SoxBCD and sulfite:acceptor oxidoreductase. All the present findings collectively highlight extensive functional diversification of sulfur-oxidizing enzymes across phylogenetically close, as well as distant, bacteria.

microbiology↗

Inorganic salts and compatible solutes help mesophilic bacteria inhabit the high temperature waters of a Trans-Himalayan sulfur-borax spring

While geographically-/geologically-distinct hot springs harbor different levels of microbial diversity, some of them encompass several such taxa which have no strain reported for laboratory growth at >45{degrees}C. We, therefore, hypothesized that native geomicrobial factors could be potent determinants of the microbial habitability of hot spring environments. To test this hypothesis, aquatic microbial communities were revealed metataxonomically, and considered in the context of spring-water chemistry, along the 85-14{degrees}C hydrothermal gradient of a sulfur-boron spring named Lotus Pond located at 4,436 m, within the Puga geothermal area of the Indian Trans-Himalayan region of Ladakh. Water samples were studied from four distinct sites along Lotus Ponds spring-water transit from the vent to an adjacent river called Rulang. Insinuations obtained from geomicrobiological data were tested via pure-culture growth experiments in habitat-inspired media. Microbial diversities were found to be high at all the sample-sites; majority of the genera identified at the 70-85{degrees}C sites were found to have no report of laboratory growth at >45{degrees}C; concurrently, these sample-sites had high concentrations of the kosmotropic solutes boron, lithium, sodium, sulfide, thiosulfate and sulfate, which are known to biophysically stabilize macromolecules. Based on the universal thermodynamic status of these solutes, we conjectured that they may be instrumental in helping mesophiles withstand high in situ temperatures. Corroboratively, growth experiments with a mesophilic, 80{degrees}C-isolate, Paracoccus SMMA_5 showed that at 50{degrees}C and 70{degrees}C, depending on the incubation-time, lithium/boron/sulfate/sodium/glycine-betaine either increases the number of colony-forming units present in the culture or arrests decline of the same. Incubations at 70{degrees}C, followed by fluorescein diacetate staining and flow cytometry, showed that these solutes keep more cells under viable condition than in ready-to-divide state. We concluded that kosmotropes and compatible solutes help mesophiles overcome the chaotropic effects of heat by augmenting such indigenous, entropy-minimizing biophysical mechanisms that apparently trade-off cell division for cell viability.

microbiology↗