Systematic and morphological diversity of endosymbiotic methanogens in anaerobic ciliates

The identities and taxonomic diversity of the endosymbiotic methanogens from the anaerobic protozoaMetopus contortus, Metopus striatus, Metopus palaeformis, Trimyema sp. andPelomyxa palustris were determined by comparative analysis of their 16S ribosomal RNA sequences. Fluorescent oligonucleotide probes were designed to bind to the symbiont rRNA sequences and to provide direct visual evidence of their origins from methanogenic archaea contained within the host cells. Confocal microscopy was used to analyze the morphology of the endosymbionts in whole cells ofMetopus palaeformis, Metopus contortus, Trimyema sp. andCyclidium porcatum. The endosymbionts are taxonomically diverse and are drawn from three different genera;Methanobacterium, Methanocorpusculum andMethanoplanus. In every case the symbionts are closely related to, but different from, free-living methanogens for which sequences are available. It is thus apparent that symbioses have been formed repeatedly and independently. Ciliates which are unrelated to each other (Trimyema sp. andMetopus contortus) may contain symbionts which are closely related, and congeneric ciliates (Metopus palaeformis andM. contortus) may contain symbionts which are distantly related to each other. This suggests that some of the symbiotic associations must be relatively recent. For example, at least one of the symbioses inMetopus must postdate the speciation ofM. palaeformis andM. contortus. Despite this,Metopus contortus, Trimyema sp., Cyclidium porcatum and their respective endosymbionts show sophisticated morphological interactions which probably facilitate the exchange of materials between the partners.     

Functional integration of Methanobacterium formicicum into the anaerobic ciliate Trimyema compressum

Monoxenic cultures of the anaerobic, endosymbiont-free ciliate Trimyema compressum were incubated with low numbers of Bacteroides sp. strain WoCb15 as food bacteria and two strains (DSM 3636 and 3637) of Methanobacterium formicicum, which originally had been isolated from the anaerobic protozoa Metopus striatus and Pelomyxapalustris. The ciliate which had lost its original endosymbiotic methanogens ingested both strains of M. formicicum. The methanogenic bacteria were found intact in large vacuoles in contrast to the food bacteria which were digested. Single methanogens were separated from the vacuoles and appeared surrounded by a membrane in the cytoplasm of the ciliate. After 2 months of incubation, the methanogenic bacteria still exhibited the typical bluish fluorescence and the new symbiotic association of M. formicicum and T. compressum excreted methane. Increasing the growth rate of the ciliates by large numbers of food bacteria resulted in a loss of the methanogenic bacteria, due to statistical outgrowth.     

Methanogenic symbionts of anaerobic ciliates and their contribution to methanogenesis in an anoxic rice field soil

Methanogenesis in rice field soils starts soon after flooding while potentially competing processes like reduction of sulphate and iron take place. Early methanogenesis is mainly driven by hydrogen, while later in the season acetate tends to become more important. Anaerobic ciliates are abundant during this period, and their endosymbionts use hydrogen produced by the ciliates to reduce carbon dioxide to methane. These endosymbiotic methanogens are protected from the competition for substrates with other bacteria that may control methanogenesis outside the protozoan cells. Thus, we focussed on early methanogenesis and on the potential contribution from ciliates and their endosymbionts. Only ciliates of the genus Metopus were found to harbour methanogens, as identified by the F(420)-fluorescence of the endosymbionts. We followed the population dynamics of the ciliates with time, and calculated the ratio of symbiotic methane production to overall methanogenesis. Symbiotic methane production was calculated from the species-specific numbers of methanogenic endosymbionts times the cell-specific methane production of the symbionts. According to this calculation, the symbionts' contribution to overall methane production was only 6.4% at the beginning and decreased with time. In a second experiment, colchicine and cycloheximide were used to inhibit all eukaryotes, comparing the remaining methane production rate to a control without inhibitors. In the inhibition experiment, the contribution from symbionts decreased from 40% to 6% during the first days after flooding, and dropped to near zero within 2 weeks. However, nearly all methane produced from H(2)/CO(2) could be attributed to the ciliates' symbionts between days 5 and 10 after flooding. Both experiments showed that the contribution of methanogenic symbionts to overall methane production is a transient phenomenon, restricted to the first 2 weeks.     

Methanobacterium formicicum,an endosymbiont of the anaerobic ciliateMetopus striatus McMurrich

The Gram-positive methanogenic endosymbiont of the sapropelic ciliateMetopus striatus was isolated and identified asMethanobacterium formicicum. In the ciliate cell the methanogens are in close association with microbody-like organelles. No mitochondria could be detected. The nature of the microbodies and the physiological background of the observed association are discussed.     

Direct conversion of cellulose to methane by anaerobic fungus Neocallimastix frontalis and defined methanogens

Co-cultures of N. frontalis with a formate-utilizing methanogen, Methanobacterium formicicum and/or an aceticlastic methanogen, Methanosaeta concilii, were performed for methane production from cellulose. In the co-culture with M. formicicum, ca. 16 mM CH₄ was produced after 7 days without accumulation of H₂ and formate. In the co-culture with M. concilii, 12 mM CH₄ was produced after 17 days with decreasing acetate production. In the tri-culture of N. frontalis with M. formicicum and M. concilii, 24 mM CH₄ was produced after 17 days where acetate still remained at 23 mM, but production of lactate and ethanol decreased. When a 4-times concentrated culture broth of M. concilii was inoculated in this tri-culture system in a bioreactor, 150 mM CH₄ was produced after 24 days by feeding of cellulose, although 57 mM acetate still accumulated.     

Cultivation of the sapropelic ciliate Plagiopyla nasuta Stein and isolation of the endosymbiont Methanobacterium formicicum

The sapropelic ciliate Plagiopyla nasuta was isolated and cultured in monoculture. Optimal conditions for growth were: 15–20°C, pH about 7, and about 2% of oxygen in the headspace. Cultures of P. nasuta produced methane. Epifluorescence microscopy revealed the presence of methanogenic bacteria as endosymbionts. An endosymbiont of the ciliate was isolated and identified as Methanobacterium formicicum. In the ciliate cell these methanogens were found to be closely associated with microbody-like organelles. No mitochondria could be detected.     

Endosymbiotic Methanogenic Bacteria In Anaerobic Ciliates: Significance For the Growth Efficiency of the Host

ABSTRACT Endosymbiotic methanogenic bacteria of three species of anaerobic ciliates (Plagiopyla frontata, Metopus conforms , and M. palaeformis) were inactivated with the specific methanogen inhibitor 2-bromoethanesulfonic acid. the absence of endosymbiont methanogens reduced growth rate and growth yield by about 30% in P. frontata and M. contortus , while no significant change in fitness was observed in M. palaeformis. In Plagiopyla the growth rate constant is not affected by an artificially increased pH₂ neither in normal nor in methanogen-free ciliates. the energetic advantage conferred by endosymbiont methanogens in Plagiopyla and in Metopus contortus probably is due to excretion of organic material from the bacteria at the expense of bacterial reproduction. It is unlikely that the maintenance of a low pH₂ within the cells due to H₂-consumption by the bacteria is important to the ciliates.     

Electromigration, a tool for studies on anaerobic ciliates

Abstract By applying electric current, anaerobic ciliates could be extracted from sludge samples. All the freshwater ciliates tested had one point of optimal current and voltage where they reached the highest net speed of migration in the electric field. The swimming behavior of Metopus es was tested under different current and voltage conditions. During electromigration the freshwater, marine and rumen ciliates moved from the anode to the cathode. In the anaerobic freshwater ciliates high numbersof methanogenic bacteria of different size were present. At the depth in the sludge with the highest number of Metopus minimus (660 cells ·ml⁻¹, a peak of methane production also occurred.     

Intestinal ciliate composition found in the feces of the Turk rahvan horse Equus caballus, Linnaeus 1758

Species composition and distribution of large intestinal ciliates were investigated in the feces from 15 Turk rahvan horses, living in the vicinity of Izmir, Turkey. Twenty-two ciliate genera consisting of 36 species were identified. This is the first report on intestinal ciliates in Turk rahvan horses and no previously unknown species were observed. The mean number of ciliates was 14.2 ± 13.9 × 10⁴ cells ml⁻¹ of feces and the mean number of ciliate species per host was 9.9 ± 7.1. No ciliates were observed in 2 horses. Bundleia and Blepharocorys were considered to be the major genera since these ciliates were constantly found in high proportions. In contrast, Paraisotricha, Didesmis and Gassovskiella were only observed at low frequencies. The ciliates found in this survey had almost the same characteristics as those described in previous reports, suggesting that there was no significant geographic variation in the intestinal ciliate fauna of equids.     

Studies on ciliated protozoa in eutrophic lakes: 2. Field and laboratory studies on the effects of oxygen and other chemical gradients on ciliate distribution

An investigation into the spatial distribution of hypolimnetic ciliates in three small eutrophic lakes during the period of summer stratification was carried out. Peak ciliate densities were found to occur at the oxic/anoxic boundary, ciliate numbers declining with increasing depth within the hypolimnion. The ciliates only occurred in aerobic water where oxygen levels were less than about 0.5 mgl^–1 Laboratory experiments demonstrated that the ciliates swim upwards under anaerobic conditions but swim rapidly downwards under aerobic conditions. Further laboratory experiments showed that although the bulk of the population occured within anaerobic water, the hypolimnetic ciliates are aerobes and cannot survive indefinite anoxia. Despite the demonstrable toxicity of high levels of ammonia and sulphide, it was probably excesive distance from an available source of oxygen that excluded the ciliates from the lowest levels of the hypolimnion. Possible mechanisms which allowed these aerobic ciliates to colonise anaerobic water are considered.     

Microbial and enzymatic improvement of anaerobic digestion of waste biomass

Metabolic activities of different microorganisms (Bacillus subtilis, B. licheniformis and Aspergillus niger) and hydrolytic enzymes (concentrations: 1 to 200 mg enzyme solids g^–1 feed) were studied individually and in combinations with respect to H₂ and methane production from damaged wheat grains. Bacillus subtilis, B. licheniformis and pre-existing hydrogen producers (control) produced 45 to 64 l H₂ kg^–1 total solids and subsequently, with the help of added methanogens, 155 to 220 l methane kg^–1 total solids could be produced. H₂ production from damaged wheat grains could be decreased to 28% or enhanced up to 152% with respect to control, by employing various microbial and enzymatic treatments. Similarly, it has been made possible to vary methane production capacities from as low as 17% to as high as 110% with respect to control.     

Emission and oxidation of methane in Equisetum fluviatile stands growing on organic sediment and sand bottoms

Methane emission and rhizospheric CH₄ oxidation were studied in stands of Equisetum fluviatile, a common cryptogam in boreal lakes. The experiment was performed in mesocosms with organic sediment or sand bottoms under natural variation of temperature and light using the light-oxic – dark-anoxic chamber (LO/DA) technique. Net CH₄ emission from the organic sediment during the growing season varied between 3.4 and 19.0 mg m^–2 h^–1, but from sand the net CH₄ emission was only 3–10% of that measured from the organic sediment. In the organic sediment net CH₄ emission was very significantly correlated with sediment temperature (r² = 0.92). In the sand mesocosms the variation of net CH₄ emission was better correlated with the shoot biomass than with sediment temperature variation during the growing season, indicating that methanogens were severely limited by substrate availability and were probably dependent on substrates produced by E. fluviatile. The proportion of the methane oxidized of the potential CH₄ emission in summer did not differ significantly between the bottom types. The net CH₄ emission during the growing season as a proportion of the seasonal maximum of the shoot biomass was significantly higher in the organic sediment mesocosms (6.5%) than in sand (1.7%). The high CH₄ emissions observed from dense well-established E. fluviatile stands in the field appear to be more related to temperature-regulated turnover of detritus in the anaerobic sediment and less to CH₄ oxidation and seasonal variation in plant growth dynamics     

Methanogenesis: surprising molecules,microorganisms and ecosystems

Methanogenesis involves a novel set of coenzymes as one-carbon and electron carriers. Consequently, metabolic processes of methanogens deviate from those present in non-methanogenic bacteria. Methanogenic bacteria can be classified on the basis of substrate utilization. Group I (24 species) grows at the expense of hydrogen plus CO₂ and/or formate and group II (7 species) uses methanol and/or acetate. Hydrogen-consuming methanogens are found as epi- or endosymbionts of anaerobic ciliates.     

Bioenergetics and anaerobic respiratory chains of aceticlastic methanogens

Methane-forming archaea are strictly anaerobic microbes and are essential for global carbon fluxes since they perform the terminal step in breakdown of organic matter in the absence of oxygen. Major part of methane produced in nature derives from the methyl group of acetate. Only members of the genera Methanosarcina and Methanosaeta are able to use this substrate for methane formation and growth. Since the free energy change coupled to methanogenesis from acetate is only − 36 kJ/mol CH₄, aceticlastic methanogens developed efficient energy-conserving systems to handle this thermodynamic limitation. The membrane bound electron transport system of aceticlastic methanogens is a complex branched respiratory chain that can accept electrons from hydrogen, reduced coenzyme F₄₂₀ or reduced ferredoxin. The terminal electron acceptor of this anaerobic respiration is a mixed disulfide composed of coenzyme M and coenzyme B. Reduced ferredoxin has an important function under aceticlastic growth conditions and novel and well-established membrane complexes oxidizing ferredoxin will be discussed in depth. Membrane bound electron transport is connected to energy conservation by proton or sodium ion translocating enzymes (F₄₂₀H₂ dehydrogenase, Rnf complex, Ech hydrogenase, methanophenazine-reducing hydrogenase and heterodisulfide reductase). The resulting electrochemical ion gradient constitutes the driving force for adenosine triphosphate synthesis. Methanogenesis, electron transport, and the structure of key enzymes are discussed in this review leading to a concept of how aceticlastic methanogens make a living. This article is part of a Special Issue entitled: 18th European Bioenergetic Conference.     

Isolation and characterization of Methanoplanus endosymbiosus sp. nov., an endosymbiont of the marine sapropelic ciliate Metopus contortus quennerstedt

Epifluorescence microscopy revealed the presence of a methanogenic bacterium as an endosymbiont in the sapropelic marine ciliate Metopus contortus. The in situ methanogenic activity of the symbiont could be demonstrated. The isolated endosymbiont was an irregular, disc-shaped bacterium with a diameter of 1.6–3.4 m. It had a generation time of 7 or 12 hours on growth on H₂/CO₂ or formate, respectively. The temperature range for growth was between 16 and 36°C with an optimum at 32°C. The optimal pH range for growth was 6.8 to 7.3. Salts, with an optimum concentration of 0.25 M, and tungsten were required for growth. The mol% G+C was 38.7%. The cell envelope consisted of proteins and a glycoprotein with an apparent molecular weight of 110,000. Morphology, antigenic relationship and the G+C content established the isolate MC1 as a new species of the genus Methanoplanus, and the name Methanoplanus endosymbiosus is proposed.Abbreviations G+C Guanine+cytosine - SDS sodium dodecylsulfate - PIPES piperazine-N,N-bis (2-ethane) sulfonic acid     

Selectivity of food bacteria for the growth of anaerobic ciliate Trimyema compressum

The anaerobic ciliate Trimyema compressum was cultivated on various food bacteria. Significant growth was observed when Lactobacillus sp., Escherichia coli, Enterobacter aerogenes, Desulfovibrio vulgaris, Methanoculleus bourgense, or Pelobacter propionicus cells were fed to the ciliates. The highest cell yield which we obtained was ca. 9,000 cells/ml when feeding D. vulgaris. However, no growth of the ciliates was observed on the culture with Clostridium novyi, Propionibacterium sp., Desulfobulbus propionicus, Methanobrevibacter arboriphilicus, Methanobacterium sp., Methanosarcina barkeri, or Methanothrix soehngenii cells. The ciliates produced acetate and methane as major end products in any cultures and small amounts of propionate, butyrate and hydrogen were also detected in some cultures. Physiological studies on the food bacteria which we tested indicated that the growth of T. compressum depended on the bacterial species, but there was no apparent correlation between the digestibility and the basic properties of those bacteria (i.e. size of the bacteria, gram-staining properties, susceptibility to the known lytic enzymes, Archaea or Bacteria).     

Ethane production by Methanosarcina barkeri during growth in ethanol supplemented medium

Methanosarcina barkeri strain 227 produced ethane during growth on H₂/CO₂ when ethanol was added to the medium in concentrations of 89–974 mM; ethane production varied from 14 to 38 nmoles per tube (20 ml gas phase, 5.7 ml liquid) with increasing ethanol concentrations. Cells grown to mid-logarithmic phase (A₆₀₀ 0.46, protein = 64 g/ml) on H₂/CO₂, thoroughly flushed with H₂/CO₂, then exposed to ethanol, produced maximal ethane levels (at 585 and 974 mM ethanol) of about 215 nmoles per tube, with an ethane/methane ratio of 1×10^-3. Mid-logarithmic-phase cultures of Methanosarcina barkeri strain Fusaro also produced ethane (up to 20 nmoles per tube) when exposed to ethanol. Cultures of strain 227 growing on methanol in the absence of H₂ produced 6 nmoles per tube of ethane when supplemented with ethanol whereas those lacking ethanol but containing H₂ and/or methanol produced 1.6 nmoles per tube. Cultures of Methanococcus deltae strains LH and RC, Methanospirillum hungatei or Methanobacterium thermoautotrophicum produced 5 nmoles ethane per tube when grown in medium containing ethanol. Ethanol concentrations of 177–886 mM were inhibitory to growth of all methanogens examined. Production of ethane by Methanosarcina was inhibited by >62 mM methanol, and both methanogenic inhibitors tested, CCl₄ and Br–CH₂–CH₂–SO _inf3 ^sup- , inhibited ethane and methane production concurrently. The data suggest that ethanol is converted to ethane by Methanosarcina species using the terminal portion of the methanol-to-methane pathway.     

End Products of Anaerobic Chitin Degradation by Salt Marsh Bacteria as Substrates for Dissimilatory Sulfate Reduction and Methanogenesis

The anaerobic pathway of chitin decomposition by chitinoclastic bacteria was examined with an emphasis on end product coupling to other salt marsh bacteria. Actively growing chitinoclastic bacterial isolates produced primarily acetate, H₂, and CO₂ in broth culture. No sulfate-reducing or methanogenic isolates grew on chitin as sole carbon source or produced any measurable degradation products. Mixed cultures of chitin degraders with sulfate reducers resulted in positive sulfide production. Mixed cultures of chitin-degrading isolates with methanogens resulted in the production of CH₄ with reductions in headspace CO₂ and H₂. The combination of all three metabolic types resulted in the simultaneous production of methane and sulfide, with more methane being produced in mixed cultures containing CO₂-reducing methanogens and acetoclastic sulfate reducers because of less interspecific H₂ competition.     

An anaerobic protozoon, with symbiotic methanogens, living in municipal landfill material

Abstract We have established that anaerobic protozoa do live in municipal landfill material although they probably spend much of the time encysted, especially in the drier (< 40% water) site. At least eight species were observed; they were readily isolated by adding anoxic water to dry landfill samples. The ciliate Metopus palaeformis was frequently i isolated; it appears to be ubiquitous in anaerobic landfills. It has a polymorphic life cycle, it is positive for hydrogenase, each ciliate contains about 500 bromoethanesulfonate-sensitive methanogen symbionts (probably Methanobacterium formicicum ), and maximum cell densities in culture exceed 3000 per ml. The methanogens are not attached to the hydrogenosomes, neither do they undergo morphological transformation; the ciliate receives no measurable energetic advantage from its symbionts. The ciliate encysts in response to a shortage of food or water, and the methanogens remain viable within the cysts. When the protozoon excysts, the methanogens resume growth and cell division within the trophic form of the ciliate. Unlike free-living methanogens, the M. palaeformis -methanogen consortium is not particularly sensitive to oxygen; the symbiotic methanogens remain viable following exposure of the consortium to atmospheric oxygen for several days. Dispersal of methanogen-bearing protozoan cysts through oxygenated environments is a potential mechanism of transfer between landfill sites and other anaerobic environments. Anaerobic protozoan consortia are theoretically capable of making a significant contribution to methane generation from wet landfill sites.     

Identification of sulphate-reducing ectosymbiotic bacteria from anaerobic ciliates using 16S rRNA binding oligonucleotide probes

The identity of ectosymbiotic bacteria of some marine, free-living anacrobic ciliates (Metopus contortus, Caenomorpha levanderi and Parablepharisma sp.) was studied using fluorescent-dye-conjugated oligonucleotides complementary to short sequence elements of 16S ribosomal RNA. The ectosymbiotic bacteria of all species hybridized with a eubacterial probe and those of the two former mentioned species hybridized with a general probe for sulphate-reducing bacteria, but not to a probe specific for Desulfobacter. The results support indirect evidence suggesting that ectosymbiotic bacteria of anaerobic ciliates are sulphate-reducers which depend on host metabolites for substrates.Abbreviations DMSO dimethyl sulfoxide - PBS phosphate-buffered saline, 137 mM NaCl, 2.7 mM KCl, 4.3 mM Na₂HPO₄, 1.4 mM KH₂PO₄, pH: 7.3 - TEAA triethylamonium acetate - 1 x SSC standard sodium citrate buffer, 150 mM NaCl, 15 mM Na₂ citrate, pH: 7.0 - 1 x Denh Denhardts solution, 0.02% ficoll, 0.02% bovine serum albumine, 0.02% polyvinol-pyralidone