RESUMEN
The hot spring microbiome is a complex assemblage of micro- and macro-organisms; however, the understanding and projection of enzymatic repertoire that access earth's integral ecosystem processes remains ambivalent. Here, the Khirganga hot spring characterized with white microbial mat and ions rich in sulfate, chlorine, sodium, and magnesium ions is investigated and displayed the examination of 41 high and medium qualified metagenome-assembled genomes (MAGs) belonged to at least 12 bacterial and 2 archaeal phyla which aids to drive sulfur, oxygen, iron, and nitrogen cycles with metabolic mechanisms involved in heavy metal tolerance. These MAGs possess over 1749 genes putatively involved in crucial metabolism of elements viz. nitrogen, phosphorus, and sulfur and 598 genes encoding enzymes for czc efflux system, chromium, arsenic, and copper heavy metals resistance. The MAGs also constitute 229 biosynthetic gene clusters classified abundantly as bacteriocins and terpenes. The metabolic roles possibly involved in altering linkages in nitrogen biogeochemical cycles and explored a discerned rate of carbon fixation exclusively in archaeal member Methanospirillum hungatei inhabited in microbial mat. Higher Pfam entropy scores of biogeochemical cycling in Proteobacteria members assuring their major contribution in assimilation of ammonia and sequestration of nitrate and sulfate components as electron acceptors. This study will readily improve the understanding of the composite relationship between bacterial species owning metal resistance genes (MRGs) and underline the exploration of adaptive mechanism of these MAGs in multi-metal contaminated environment. KEY POINTS: ⢠Identification of 41 novel bacterial and archaeal species in habitats of hot spring ⢠Genome-resolved metagenomics revealed MRGs (n = 598) against Cr, Co, Zn, Cd, As, and Cu ⢠Highest entropies of N (0.48) and Fe (0.44) cycles were detected within the MAGs.
Asunto(s)
Manantiales de Aguas Termales , Microbiota , Manantiales de Aguas Termales/microbiología , Metagenómica , Bacterias/genética , Bacterias/metabolismo , Archaea/genética , Archaea/metabolismo , Metagenoma , Metales/metabolismo , Azufre/metabolismo , Nitrógeno/metabolismo , FilogeniaRESUMEN
Eukaryotic and archaeal translation initiation factor 2 (e/aIF2) functions as a heterotrimeric complex. It consists of three subunits (α, ß, γ). α- and ß-subunits are bound to γ-subunit by hydrogen bonds and van der Waals interactions, but do not contact each other. Although main functions of the factor are performed by the γ-subunit, reliable formation of αγ and ßγ complexes is necessary for its proper functioning. In this work, we introduced mutations in the recognition part of the ßγ interface and showed that hydrophobic effect plays a crucial role in the recognition of subunits both in eukaryotes and archaea. Shape and properties of the groove on the surface of γ-subunit facilitates transition of the disordered recognition part of the ß-subunit into an α-helix containing approximately the same number of residues in archaea and eukaryotes. In addition, based on the newly obtained data, it was concluded that in archaea and eukaryotes, transition of the γ-subunit to the active state leads to additional contact between the region of switch 1 and C-terminal part of the ß-subunit, which stabilizes helical conformation of the switch.
Asunto(s)
Eucariontes , Factor 2 Procariótico de Iniciación , Sitios de Unión , Factor 2 Procariótico de Iniciación/química , Eucariontes/genética , Eucariontes/metabolismo , Archaea/genética , Archaea/metabolismo , Guanosina TrifosfatoRESUMEN
Iron oxides and sulfate are usually abundant in paddy soil, but their role in reducing methane emissions is little known. In this work, paddy soil was anaerobically cultivated with ferrihydrite and sulfate for 380 days. An activity assay, inhibition experiment, and microbial analysis were conducted to evaluate the microbial activity, possible pathways, and community structure, respectively. The results showed that anaerobic oxidation of methane (AOM) was active in the paddy soil. The AOM activity was much higher with ferrihydrite than sulfate, and an extra 10% of AOM activity was stimulated when ferrihydrite and sulfate coexisted. The microbial community was highly similar to the duplicates but totally different with different electron acceptors. The microbial abundance and diversity decreased due to the oligotrophic condition, but mcrA-carrying archaea increased 2-3 times after 380 days. Both the microbial community and the inhibition experiment implied that there was an intersection between iron and sulfur cycles. A "cryptic sulfur cycle" might link the two cycles, in which sulfate was quickly regenerated by iron oxides, and it might contribute 33% of AOM in the tested paddy soil. Complex links between methane, iron, and sulfur geochemical cycles occur in paddy soil, which may be significant in reducing methane emissions from rice fields.
Asunto(s)
Fertilizantes , Suelo , Metano/metabolismo , Sulfatos/metabolismo , Anaerobiosis , Archaea/metabolismo , Hierro/metabolismo , Oxidación-Reducción , Óxidos de Azufre , Azufre/metabolismoRESUMEN
Cyclic dimeric AMP (c-di-AMP) is a widespread second messenger that controls such key functions as osmotic homeostasis, peptidoglycan biosynthesis, and response to various stresses. C-di-AMP is synthesized by diadenylate cyclases that contain the DAC (DisA_N) domain, which was originally characterized as the N-terminal domain in the DNA integrity scanning protein DisA. In other experimentally studied diadenylate cyclases, DAC domain is typically located at the protein C termini and its enzymatic activity is controlled by one or more N-terminal domains. As in other bacterial signal transduction proteins, these N-terminal modules appear to sense environmental or intracellular signals through ligand binding and/or protein-protein interactions. Studies of bacterial and archaeal diadenylate cyclases also revealed numerous sequences with uncharacterized N-terminal regions. This work provides a comprehensive review of the N-terminal domains of bacterial and archaeal diadenylate cyclases, including the description of five previously undefined domains and three PK_C-related domains of the DacZ_N superfamily. These data are used to classify diadenylate cyclases into 22 families, based on their conserved domain architectures and the phylogeny of their DAC domains. Although the nature of the regulatory signals remains obscure, the association of certain dac genes with anti-phage defense CBASS systems and other phage-resistance genes suggests that c-di-AMP might also be involved in the signaling of phage infection.
Asunto(s)
Archaea , Liasas de Fósforo-Oxígeno , Humanos , Archaea/genética , Archaea/metabolismo , Liasas de Fósforo-Oxígeno/metabolismo , Proteínas Bacterianas/metabolismo , Bacterias/genética , Bacterias/metabolismo , Sistemas de Mensajero Secundario , AMP Cíclico/metabolismo , Fosfatos de Dinucleósidos/metabolismoRESUMEN
BACKGROUND: Microbes produce diverse secondary metabolites (SMs) such as signaling molecules and antimicrobials that mediate microbe-microbe interaction. Archaea, the third domain of life, are a large and diverse group of microbes that not only exist in extreme environments but are abundantly distributed throughout nature. However, our understanding of archaeal SMs lags far behind our knowledge of those in bacteria and eukarya. RESULTS: Guided by genomic and metabolic analysis of archaeal SMs, we discovered two new lanthipeptides with distinct ring topologies from a halophilic archaeon of class Haloarchaea. Of these two lanthipeptides, archalan α exhibited anti-archaeal activities against halophilic archaea, potentially mediating the archaeal antagonistic interactions in the halophilic niche. To our best knowledge, archalan α represents the first lantibiotic and the first anti-archaeal SM from the archaea domain. CONCLUSIONS: Our study investigates the biosynthetic potential of lanthipeptides in archaea, linking lanthipeptides to antagonistic interaction via genomic and metabolic analyses and bioassay. The discovery of these archaeal lanthipeptides is expected to stimulate the experimental study of poorly characterized archaeal chemical biology and highlight the potential of archaea as a new source of bioactive SMs. Video Abstract.
Asunto(s)
Archaea , Proteínas Arqueales , Archaea/genética , Archaea/metabolismo , Proteínas Arqueales/genética , Proteínas Arqueales/metabolismo , Bacterias/genética , Genómica , Interacciones MicrobianasRESUMEN
This study proposes a novel method to enhance methane production from anaerobic digestion using an amino acid-derived ionic liquid, glycine hydrochloride, ([Gly][Cl]), as an exogenous additive. After 40 days of digestion with 5% [Gly][Cl], the cumulative methane production was 115.56 mL/g VS, which was 73% higher than that of the control group (without additive). Specifically, the peak activities of cellulase, xylanase, and lignin peroxidase were significantly higher than those of the control group. The addition of [Gly][Cl] increased bacterial diversity and reduced archaeal diversity. Synergistota represented by Syner-01, Fibrobacterota represented by BBMC-4, Bacteroides, and unclassified_f__Lachnospiraceae significantly increased in relative abundance. It suggested that [Gly][Cl] stimulated the activities of protein-hydrolyzing and acid-producing bacteria. [Gly][Cl] also increased the abundance of methanogens and archaea, converting more lignocellulose to methane. Methanobacterium, that metabolizes H2 and CO2 to CH4, was more abundant. Therefore, [Gly][Cl] can improve methane yield as an anaerobic digestion additive.
Asunto(s)
Líquidos Iónicos , Oryza , Anaerobiosis , Oryza/metabolismo , Líquidos Iónicos/farmacología , Aminoácidos/metabolismo , Bacterias/metabolismo , Archaea/metabolismo , Clostridiales/metabolismo , Metano , Reactores Biológicos/microbiologíaRESUMEN
Methane-producing archaea play a crucial role in the global carbon cycle and are used for biotechnological fuel production. Methanogenic model organisms such as Methanococcus maripaludis and Methanosarcina acetivorans have been biochemically characterized and can be genetically engineered by using a variety of existing molecular tools. The anaerobic lifestyle and autofluorescence of methanogens, however, restrict the use of common fluorescent reporter proteins (e.g., GFP and derivatives), which require oxygen for chromophore maturation. Recently, the use of a novel oxygen-independent fluorescent activation and absorption-shifting tag (FAST) was demonstrated with M. maripaludis. Similarly, we now describe the use of the tandem activation and absorption-shifting tag protein 2 (tdFAST2), which fluoresces when the cell-permeable fluorescent ligand (fluorogen) 4-hydroxy-3,5-dimethoxybenzylidene rhodanine (HBR-3,5DOM) is present. Expression of tdFAST2 in M. acetivorans and M. maripaludis is noncytotoxic and tdFAST2:HBR-3,5DOM fluorescence is clearly distinguishable from the autofluorescence. In flow cytometry experiments, mixed methanogen cultures can be distinguished, thereby allowing for the possibility of high-throughput investigations of the characteristic dynamics within single and mixed cultures. IMPORTANCE Methane-producing archaea play an essential role in the global carbon cycle and demonstrate great potential for various biotechnological applications, e.g., biofuel production, carbon dioxide capture, and electrochemical systems. Oxygen sensitivity and high autofluorescence hinder the use of common fluorescent proteins for studying methanogens. By using tdFAST2:HBR-3,5DOM fluorescence, which functions under anaerobic conditions and is distinguishable from the autofluorescence, real-time reporter studies and high-throughput investigation of the mixed culture dynamics of methanogens via flow cytometry were made possible. This will further help accelerate the sustainable exploitation of methanogens.
Asunto(s)
Archaea , Metano , Archaea/metabolismo , Citometría de Flujo , Metano/metabolismo , Methanosarcina/metabolismoRESUMEN
Methanogenic archaea possess diverse metabolic characteristics and are an ecologically and biotechnologically important group of anaerobic microorganisms. Although the scientific and biotechnological value of methanogens is evident with regard to their methane-producing physiology, little is known about their amino acid excretion, and virtually nothing is known about the lipidome at different substrate concentrations and temperatures on a quantitative comparative basis. Here, we present the lipidome and a comprehensive quantitative analysis of proteinogenic amino acid excretion as well as methane, water, and biomass production of the three autotrophic, hydrogenotrophic methanogens Methanothermobacter marburgensis, Methanothermococcus okinawensis, and Methanocaldococcus villosus under varying temperatures and nutrient supplies. The patterns and rates of production of excreted amino acids and the lipidome are unique for each tested methanogen and can be modulated by varying the incubation temperature and substrate concentration, respectively. Furthermore, the temperature had a significant influence on the lipidomes of the different archaea. The water production rate was much higher, as anticipated from the rate of methane production for all studied methanogens. Our results demonstrate the need for quantitative comparative physiological studies connecting intracellular and extracellular constraints of organisms to holistically investigate microbial responses to environmental conditions. IMPORTANCE Biological methane production by methanogenic archaea has been well studied for biotechnological purposes. This study reveals that methanogenic archaea actively modulate their lipid inventory and proteinogenic amino acid excretion pattern in response to environmental changes and the possible utilization of methanogenic archaea as microbial cell factories for the targeted production of lipids and amino acids.
Asunto(s)
Archaea , Euryarchaeota , Archaea/metabolismo , Temperatura , Lipidómica , Euryarchaeota/metabolismo , Metano , Agua/metabolismoRESUMEN
Terpenoids, also known as isoprenoids, are the largest and most diverse class of organic compounds in nature and are involved in many membrane-associated cellular processes, including membrane organization, electron transport chain, cell signaling, and phototrophy. Terpenoids are ancient compounds with their origin presumably before the last universal common ancestor. However, Bacteria and Archaea are known to possess two distinct terpenoid repertoires and utilize terpenoids differently. Most notably, archaea constitute their cellular membrane solely made of terpenoid-based phospholipids, contrary to the bacterial membrane that consists of fatty acid-based phospholipids. Thus, the composition of ancestral membranes at the beginning of cellular life and the diversification of terpenoids in early life remain enigmatic. This review addresses these key issues through comprehensive phylogenomic analyses of extant terpenoid biosynthesis enzymes in Bacteria and Archaea. We aim to infer the basal components of terpenoid biosynthesis machinery that have an ancient origin before the divergence of the two domains and shed light on the deep evolutionary connection between terpenoid biochemistry and early life.
Asunto(s)
Archaea , Bacterias , Bacterias/metabolismo , Archaea/metabolismo , Filogenia , Fosfolípidos/metabolismo , Terpenos/metabolismo , Evolución MolecularRESUMEN
The ocean is a net source of the greenhouse gas and ozone-depleting substance, nitrous oxide (N2O), to the atmosphere. Most of that N2O is produced as a trace side product during ammonia oxidation, primarily by ammonia-oxidizing archaea (AOA), which numerically dominate the ammonia-oxidizing community in most marine environments. The pathways to N2O production and their kinetics, however, are not completely understood. Here, we use 15N and 18O isotopes to determine the kinetics of N2O production and trace the source of nitrogen (N) and oxygen (O) atoms in N2O produced by a model marine AOA species, Nitrosopumilus maritimus. We find that during ammonia oxidation, the apparent half saturation constants of nitrite and N2O production are comparable, suggesting that both processes are enzymatically controlled and tightly coupled at low ammonia concentrations. The constituent atoms in N2O are derived from ammonia, nitrite, O2, and H2O via multiple pathways. Ammonia is the primary source of N atoms in N2O, but its contribution varies with ammonia to nitrite ratio. The ratio of 45N2O to 46N2O (i.e., single or double labeled N) varies with substrate ratio, leading to widely varying isotopic signatures in the N2O pool. O2 is the primary source for O atoms. In addition to the previously demonstrated hybrid formation pathway, we found a substantial contribution by hydroxylamine oxidation, while nitrite reduction is an insignificant source of N2O. Our study highlights the power of dual 15N-18O isotope labeling to disentangle N2O production pathways in microbes, with implications for interpretation of pathways and regulation of marine N2O sources.
Asunto(s)
Amoníaco , Archaea , Archaea/metabolismo , Amoníaco/metabolismo , Nitrificación , Nitritos/metabolismo , Marcaje Isotópico , Oxígeno/metabolismo , Oxidación-Reducción , Óxido Nitroso/metabolismoRESUMEN
Heliorhodopsin (HeR) is a seven-helical transmembrane protein with a retinal chromophore that corresponds to a new rhodopsin family. HeR from the archaebacterium Thermoplasmatales archaeon (TaHeR) exhibits unique features, such as the inverted protein orientation in the membrane compared to other rhodopsins and a long photocycle. Here, we used solid-state nuclear magnetic resonance (NMR) spectroscopy to investigate the 13C and 15N NMR signals of the retinal chromophore and protonated Schiff base (RPSB) in TaHeR embedded in POPE/POPG membrane. Although the 14- and 20-13C retinal signals indicated 13-trans/15-anti (all-trans) configurations, the 20-13C chemical shift value was different from that of other microbial rhodopsins, indicating weakly steric hinderance between Phe203 and the C20 methyl group. 15N RPSB/λmax plot deviated from the linear correlation based on retinylidene-halide model compounds. Furthermore, 15N chemical shift anisotropy (CSA) suggested that Ser112 and Ser234 polar residues distinguish the electronic environment tendencies of RPSB from those of other microbial rhodopsins. Our NMR results revealed that the retinal chromophore and the RPSB in TaHeR exhibit unique electronic environments.
Asunto(s)
Retinaldehído , Thermoplasmales , Retinaldehído/química , Retinaldehído/metabolismo , Bases de Schiff/química , Rodopsina/química , Rodopsina/metabolismo , Rodopsinas Microbianas/química , Espectroscopía de Resonancia Magnética/métodos , Thermoplasmales/metabolismo , Archaea/metabolismoRESUMEN
Ammonia oxidation carried out by ammonia-oxidizing microorganisms (AOMs) is a central step in the global nitrogen cycle. Aerobic AOMs comprise conventional ammonia-oxidizing bacteria (AOB), novel ammonia-oxidizing archaea (AOA), which could exist in complex and extreme conditions, and complete ammonia oxidizers (comammox), which directly oxidize ammonia to nitrate within a single cell. Anaerobic AOMs mainly comprise anaerobic ammonia-oxidizing bacteria (AnAOB), which can transform NH4+-N and NO2--N into N2 under anaerobic conditions. In this review, the unique metabolic characteristics, microbial community of AOMs and the influencing factors are discussed. Process applications of nitrification/denitrification, nitritation/denitrification, nitritation/anammox and partial denitrification/anammox in wastewater treatment systems are emphasized. The future development of nitrogen removal processes using AOMs is expected, enrichment of comammox facilitates the complete nitrification performance, inhibiting the activity of comammox and NOB could achieve stable nitritation, and additionally, AnAOB conducting the anammox process in municipal wastewater is a promising development direction.
Asunto(s)
Microbiota , Aguas Residuales , Amoníaco/metabolismo , Oxidación-Reducción , Bacterias/metabolismo , Archaea/metabolismo , Nitrificación , Nitrógeno/metabolismo , Reactores Biológicos/microbiologíaRESUMEN
Three inhibitors targeting different microorganisms, both from Archaea and Bacteria domains, were evaluated for their effect on CO2 biomethanation: sodium ionophore III (ETH2120), carbon monoxide (CO), and sodium 2-bromoethanesulfonate (BES). This study examines how these compounds affect the anaerobic digestion microbiome in a biogas upgrading process. While archaea were observed in all experiments, methane was produced only when adding ETH2120 or CO, not when adding BES, suggesting archaea were in an inactivated state. Methane was produced mainly via methylotrophic methanogenesis from methylamines. Acetate was produced at all conditions, but a slight reduction on acetate production (along with an enhancement on CH4 production) was observed when applying 20 kPa of CO. Effects on CO2 biomethanation were difficult to observe since the inoculum used was from a real biogas upgrading reactor, being this a complex environmental sample. Nevertheless, it must be mentioned that all compounds had effects on the microbial community composition.
Asunto(s)
Biocombustibles , Dióxido de Carbono , Biocombustibles/microbiología , Dióxido de Carbono/metabolismo , Prevalencia , Archaea/metabolismo , Acetatos , Metano/metabolismo , Reactores Biológicos/microbiología , AnaerobiosisRESUMEN
Traditionally produced fish sauce can contain significant amounts of histamine. In some instances, the histamine concentration may be well above the limit recommended by the Codex Alimentarius Commission. The aim of this study was to discover new bacterial strains capable of growing under the stressful environmental conditions of fish sauce fermentation and metabolizing histamine. In this study, 28 bacterial strains were isolated from Vietnamese fish sauce products based on their ability to grow at high salt concentrations (23% NaCl) and tested for their ability to degrade histamine. Strain TT8.5 showed the highest histamine-degradation (45.1 ± 0.2% of initially 5 mM histamine within 7 days) and was identified as Virgibacillus campisalis TT8.5. Its histamine-degrading activity was shown to be localized intracellularly and the enzyme is a putative histamine dehydrogenase. The strain exhibited optimal growth and histamine-degrading activity at 37°C, pH 7%, and 5% NaCl in halophilic archaea (HA) histamine broth. It also showed pronounced histamine-degrading activity in HA histamine broth when cultivated at temperatures of up to 40 °C as well as in the presence of up to 23% NaCl. After treatment with immobilized cells, 17.6-26.9% of the initial histamine in various fish sauce products were reduced within 24 h of incubation, while no significant changes in other parameters of fish sauce quality were observed after this treatment. Our results indicate that V. campisalis TT8.5 is of potential interest to be applied in histamine degradation of traditional fish sauce.
Asunto(s)
Histamina , Virgibacillus , Animales , Histamina/metabolismo , Cloruro de Sodio/farmacología , Virgibacillus/metabolismo , Peces/metabolismo , Fermentación , Archaea/metabolismoRESUMEN
The adaptation of microbial community to the long-term contamination of hexabromocyclododecanes (HBCDs) has not been well studied. Our previous study found that the HBCDs contamination in the microcosms constructed of sediments from two different mangrove forests in 8 months resulted in serious acidification (pH2-3). This study reanalyzed previous sequencing data and compared them with data after 20 months to investigate the adaptive properties of microbial communities in the stress of HBCDs and acidification. It hypothesized that the reassembly was based on the fitness of taxa. The results indicated that eukaryotes and fungi might have better adaptive capacity to these deteriorated habitats. Eukaryotic taxa Eufallia and Syncystis, and fungal taxa Wickerhamomyces were only detected after 20 months of contamination. Moreover, eukaryotic taxa Caloneis and Nitzschia, and fungal taxa Talaromyces were dominant in most of microbial communities (14.467-95.941%). The functional compositions were sediment-dependent and more divergent than community reassemblies. Network and co-occurrence analysis suggested that acidophiles such as Acidisoma and Acidiphilium were gaining more positive relations in the long-term stress. The acidophilic taxa and genes involved in resistance to the acidification and toxicity of HBCDs were enriched, for example, bacteria Acidisoma and Acidiphilium, archaea Thermogymnomonas, and eukaryotes Nitzschia, and genes kdpC, odc1, polA, gst, and sod-2. These genes involved in oxidative stress response, energy metabolism, DNA damage repair, potassium transportation, and decarboxylation. It suggested that the microbial communities might cope with the stress from HBCDs and acidification via multiple pathways. The present research shed light on the evolution of microbial communities under the long-term stress of HBCDs contamination and acidification.
Asunto(s)
Hidrocarburos Bromados , Microbiota , Hidrocarburos Bromados/análisis , Eucariontes/metabolismo , Archaea/genética , Archaea/metabolismoRESUMEN
Exploring nitrifiers in extreme environments is vital to expanding our understanding of nitrogen cycle and microbial diversity. This study presents that complete ammonia oxidation (comammox) Nitrospira, together with acidophilic ammonia-oxidizing archaea (AOA), dominate in the nitrifying guild in sediments of an acid mine lake (AML). The lake water was characterized by acidic pH below 5 with a high ammonium concentration of 175 mg-N/liter, which is rare on the earth. Nitrification was active in sediments with a maximum nitrate production potential of 70.5 µg-N/(g-dry weight [dw] day) for mixed sediments. Quantitative PCR assays determined that in AML sediments, comammox Nitrospira and AOA amoA genes had relative abundances of 52% and 41%, respectively, among the total amoA genes. Further assays with 16S rRNA and amoA gene amplicon sequencing and metagenomics confirmed their dominance and revealed that the comammox Nitrospira found in sediments belonged to comammox Nitrospira clade A.2. Metagenomic binning retrieved a metagenome-assembled genome (MAG) of the comammox Nitrospira from sediments (completeness = 96.76%), and phylogenomic analysis suggested that it was a novel comammox Nitrospira. Comparative genomic investigation revealed that this comammox Nitrospira contained diverse metal resistance genes and an acidophile-affiliated F-type ATPase. Moreover, it had a more diverse genomic characteristic on nitrogen metabolism than the AOA in sediments and canonical AOB did. The results suggest that comammox Nitrospira is a versatile nitrifier that can adapt to acidic environments even with high ammonium concentrations. IMPORTANCE Ammonia-oxidizing archaea (AOA) was previously considered the sole dominant ammonia oxidizer in acidic environments. This study, however, found that complete ammonia oxidation (comammox) Nitrospira was also a dominant ammonia oxidizer in the sediments of an acidic mine lake, which had an acidic pH < 5 and a high ammonium concentration of 175 mg-N/liter. In combination with average nucleotide identity analysis, phylogenomic analysis suggested it is a novel strain of comammox Nitrospira. Moreover, the adaption of comammox Nitrospira to the acidic lake had been comprehensively investigated based on genome-centric metagenomic approaches. The outcomes of this study significantly expand our understanding of the diversity and adaptability of ammonia oxidizers in the acidic environments.
Asunto(s)
Compuestos de Amonio , Leucemia Mieloide Aguda , Humanos , Archaea/metabolismo , Amoníaco/metabolismo , Compuestos de Amonio/metabolismo , Lagos , ARN Ribosómico 16S/genética , ARN Ribosómico 16S/metabolismo , Oxidación-Reducción , Bacterias , Nitrificación , FilogeniaRESUMEN
Tetramethylammonium hydroxide (TMAH) is a known toxic chemical used in the photolithography process of semiconductor photoelectronic processes. Significant amounts of wastewater containing TMAH are discharged from electronic industries. It is therefore attractive to apply anaerobic treatment to industrial wastewater containing TMAH. In this study, a novel TMAH-degrading methanogenic archaeon was isolated from the granular sludge of a psychrophilic upflow anaerobic sludge blanket (UASB) reactor treating synthetic wastewater containing TMAH. Although the isolate (strain NY-STAYD) was phylogenetically related to Methanomethylovorans uponensis, it was the only isolated Methanomethylovorans strain capable of TMAH degradation. Strain NY-STAYD was capable of degrading methylamine compounds, similar to the previously isolated Methanomethylovorans spp. While the strain was able to grow at temperatures ranging from 15 to 37°C, the cell yield was higher at lower temperatures. The distribution of archaeal cells affiliated with the genus Methanomethylovorans in the original granular sludge was investigated by fluorescence in situ hybridization (FISH) using specific oligonucleotide probe targeting 16S rRNA. The results demonstrated that the TMAH-degrading cells associated with the genus Methanomethylovorans were not intermingled with other microorganisms but rather isolated on the granule's surface as a lone dominant archaeon. KEY POINTS: ⢠A TMAH-degrading methanogenic Methanomethylovorans strain was isolated ⢠This strain was the only known Methanomethylovorans isolate that can degrade TMAH ⢠The highest cell yield of the isolate was obtained at psychrophilic conditions.
Asunto(s)
Archaea , Euryarchaeota , Archaea/genética , Archaea/metabolismo , Aguas Residuales , Aguas del Alcantarillado/química , Hibridación Fluorescente in Situ , ARN Ribosómico 16S/genética , ARN Ribosómico 16S/metabolismo , Reactores Biológicos , Euryarchaeota/metabolismo , Methanosarcinaceae/genética , Anaerobiosis , Eliminación de Residuos Líquidos/métodosRESUMEN
Nitrate-driven anaerobic oxidation of methane (AOM), catalyzing by Candidatus Methanoperedens-like archaea, is a new addition in the global CH4 cycle. This AOM process acts as a novel pathway for CH4 emission reduction in freshwater aquatic ecosystems; however, its quantitative importance and regulatory factors in riverine ecosystems are nearly unknown. Here, we examined the spatio-temporal changes of the communities of Methanoperedens-like archaea and nitrate-driven AOM activity in sediment of Wuxijiang River, a mountainous river in China. These archaeal community composition varied significantly among reaches (upper, middle, and lower reaches) and between seasons (winter and summer), but their mcrA gene diversity showed no significant spatial or temporal variations. The copy numbers of Methanoperedens-like archaeal mcrA genes were 1.32 × 105-2.47 × 107 copies g-1 (dry weight), and the activity of nitrate-driven AOM was 0.25-1.73 nmol CH4 g-1 (dry weight) d-1, which could potentially reduce 10.3% of CH4 emissions from rivers. Significant spatio-temporal variations of mcrA gene abundance and nitrate-driven AOM activity were found. Both the gene abundance and activity increased significantly from upper to lower reaches in both seasons, and were significantly higher in sediment collected in summer than in winter. In addition, the variations of Methanoperedens-like archaeal communities and nitrate-driven AOM activity were largely impacted by the sediment temperature, NH4+ and organic carbon contents. Taken together, both time and space scales need to be considered for better evaluating the quantitative importance of nitrate-driven AOM in reducing CH4 emissions from riverine ecosystems.
Asunto(s)
Archaea , Nitratos , Archaea/genética , Archaea/metabolismo , Nitratos/metabolismo , Ecosistema , Ríos , Metano/metabolismo , Anaerobiosis , Oxidación-ReducciónRESUMEN
ESCRT-III family proteins form composite polymers that deform and cut membrane tubes in the context of a wide range of cell biological processes across the tree of life. In reconstituted systems, sequential changes in the composition of ESCRT-III polymers induced by the AAA-adenosine triphosphatase Vps4 have been shown to remodel membranes. However, it is not known how composite ESCRT-III polymers are organized and remodeled in space and time in a cellular context. Taking advantage of the relative simplicity of the ESCRT-III-dependent division system in Sulfolobus acidocaldarius, one of the closest experimentally tractable prokaryotic relatives of eukaryotes, we use super-resolution microscopy, electron microscopy, and computational modeling to show how CdvB/CdvB1/CdvB2 proteins form a precisely patterned composite ESCRT-III division ring, which undergoes stepwise Vps4-dependent disassembly and contracts to cut cells into two. These observations lead us to suggest sequential changes in a patterned composite polymer as a general mechanism of ESCRT-III-dependent membrane remodeling.
Asunto(s)
Archaea , Complejos de Clasificación Endosomal Requeridos para el Transporte , Complejos de Clasificación Endosomal Requeridos para el Transporte/metabolismo , Archaea/metabolismo , Polímeros , División CelularRESUMEN
Northern lakes disproportionately influence the global carbon cycle, and may do so more in the future depending on how their microbial communities respond to climate warming. Microbial communities can change because of the direct effects of climate warming on their metabolism and the indirect effects of climate warming on groundwater connectivity from thawing of surrounding permafrost, especially at lower landscape positions. Here we used shotgun metagenomics to compare the taxonomic and functional gene composition of sediment microbes in 19 peatland lakes across a 1600-km permafrost transect in boreal western Canada. We found microbes responded differently to the loss of regional permafrost cover than to increases in local groundwater connectivity. These results suggest that both the direct and indirect effects of climate warming, which were respectively associated with loss of permafrost and subsequent changes in groundwater connectivity interact to change microbial composition and function. Archaeal methanogens and genes involved in all major methanogenesis pathways were more abundant in warmer regions with less permafrost, but higher groundwater connectivity partly offset these effects. Bacterial community composition and methanotrophy genes did not vary with regional permafrost cover, and the latter changed similarly to methanogenesis with groundwater connectivity. Finally, we found an increase in sugar utilization genes in regions with less permafrost, which may further fuel methanogenesis. These results provide the microbial mechanism for observed increases in methane emissions associated with loss of permafrost cover in this region and suggest that future emissions will primarily be controlled by archaeal methanogens over methanotrophic bacteria as northern lakes warm. Our study more generally suggests that future predictions of aquatic carbon cycling will be improved by considering how climate warming exerts both direct effects associated with regional-scale permafrost thaw and indirect effects associated with local hydrology.
