Detection of the osmoregulator betaine in methanogens.

Trimethyl glycine (glycine betaine) was detected by 13C nuclear magnetic resonance spectroscopy at high intracellular concentrations in several methanogens (Methanogenium cariaci, "Methanogenium anulus" AN9, Methanohalophilus zhilinae, Methanohalophilus mahii, and Methanococcus voltae) grown on marine media containing yeast extract. 13C labeling studies with Methanogenium cariaci suggested that the betaine which accumulated inside the cells was not synthesized de novo but was transported in from the medium. Proof of such a transport system was provided by growing Methanogenium cariaci on yeast-free medium supplemented with betaine. Under these conditions, betaine was the dominant osmoregulator.     

Free amino acid dynamics in marine methanogens. beta-Amino acids as compatible solutes.

Methanogenic archaebacteria respond to osmotic stress by accumulating a series of organic molecules which function as compatible solutes. In two strains of marine methanogenic archaebacteria, Methanogenium cariaci and Methanococcus thermolithotrophicus, four key organic solutes are observed: L-alpha-glutamate, beta-glutamate, N epsilon-acetyl-beta-lysine, and betaine. The first three of these are synthesized de novo; betaine is transported into the Mg. cariaci cells from the medium. Mesophilic Mg. cariaci will preferentially transport betaine from the extracellular medium if it is present to counterbalance the external NaCl. In its absence it synthesizes N epsilon-acetyl-beta-lysine as the dominant osmolyte. This zwitterionic compound occurs at levels in Mg. cariaci which are considerably greater (based on mumol/mg of protein) than in Mc. thermolithotrophicus grown in media of the same ionic strength. Intracellular potassium ion concentrations, determined by 39K NMR spectroscopy and atomic absorption, differ significantly in the two cells. In Mc. thermolithotrophicus, intracellular K+ is balanced by the total concentration of anionic amino acid species, glutamate, and beta-glutamate. Turnover of the organic solutes has been monitored using 13C-pulse/12C-chase, and 15N-pulse/14N-chase experiments. Both beta-amino acids exhibit slower turnover rates when compared to L-alpha-glutamate or aspartate, consistent with their roles as compatible solutes. Biosynthetic information for the beta-amino acids is also provided by 13C-labeling experiments. beta-Glutamate shows a lag in 13C uptake from 13CO2, indicative of its biosynthesis from a precursor (probably a macromolecule) not in equilibrium with the soluble L-alpha-glutamate pool. Confirmation of a novel route for beta-glutamate synthesis and the production of the beta-lysine moiety from the diaminopimelate pathway is deduced from [13C2]acetate labeling patterns.     

Occurrence of beta-glutamate, a novel osmolyte, in marine methanogenic bacteria.

The unusual compound beta-aminoglutaric acid (beta-glutamate) has been identified by 13C nuclear magnetic resonance spectroscopy in soluble extracts of marine methanogenic bacteria. We examined several methanogen species representing nine genera and found that beta-glutamate occurred in methanococci and two methanogenium strains (Methanogenium cariaci JR1 and "Methanogenium anulus" AN9). The presence of this compound in the methanococci examined was further restricted to thermophilic members of the genus Methanococcus, including Methanococcus thermolithotrophicus strains, Methanococcus jannaschii, and "Methanococcus igneus." The two Methanogenium strains examined were mesophiles. Studies using Methanococcus thermolithotrophicus showed that levels of beta-glutamate in cells of that species were not affected by variation in growth temperature (40 to 65 degrees C), NH4+ (2 to 80 mM), Mg2+ (10 to 50 mM), or K+ (2 to 10 mM) in the medium. In contrast, soluble pools of beta-glutamate and L-alpha-glutamate (the other major free amino acid in all the methanococci) were proportional to NaCl levels in the growth medium. This dependence of beta-glutamate and L-alpha-glutamate concentrations on salt levels in the medium suggests that they function as osmolytes in these cells.     

Occurrence of beta-glutamate, a novel osmolyte, in marine methanogenic bacteria

The unusual compound beta-aminoglutaric acid (beta-glutamate) has been identified by 13C nuclear magnetic resonance spectroscopy in soluble extracts of marine methanogenic bacteria. We examined several methanogen species representing nine genera and found that beta-glutamate occurred in methanococci and two methanogenium strains (Methanogenium cariaci JR1 and "Methanogenium anulus" AN9). The presence of this compound in the methanococci examined was further restricted to thermophilic members of the genus Methanococcus, including Methanococcus thermolithotrophicus strains, Methanococcus jannaschii, and "Methanococcus igneus." The two Methanogenium strains examined were mesophiles. Studies using Methanococcus thermolithotrophicus showed that levels of beta-glutamate in cells of that species were not affected by variation in growth temperature (40 to 65 degrees C), NH4+ (2 to 80 mM), Mg2+ (10 to 50 mM), or K+ (2 to 10 mM) in the medium. In contrast, soluble pools of beta-glutamate and L-alpha-glutamate (the other major free amino acid in all the methanococci) were proportional to NaCl levels in the growth medium. This dependence of beta-glutamate and L-alpha-glutamate concentrations on salt levels in the medium suggests that they function as osmolytes in these cells.     

Biosynthetic pathways of the osmolytes N epsilon-acetyl-beta-lysine, beta-glutamine, and betaine in Methanohalophilus strain FDF1 suggested by nuclear magnetic resonance analyses.

Methanohalophilus strain FDF1 synthesizes beta-glutamine, betaine, and N epsilon-acetyl-beta-lysine as osmoprotective agents when the cells are grown in high external concentrations of NaCl. Nuclear magnetic resonance spectroscopic analyses of 13CH3OH-12CO2 label incorporation by the cells provide information on the biosynthetic pathways of these organic osmolytes. The labeling studies indicate that Methanohalophilus strain FDF1 produces glutamate and beta-glutamine via a partial oxidative Krebs pathway. 13C labeling of betaine is consistent with methylation of glycine generated from serine (via serine hydroxymethyltransferase). The labeling pattern for N epsilon-acetyl-beta-lysine is consistent with the synthesis of its precursor alpha-lysine occurring by the diaminopimelate pathway in these cells.     

Composition, Variation, and Dynamics of Major Osmotic Solutes in Methanohalophilus Strain FDF1

Methanohalophilus strain FDF1, a member of the halophilic genus of methanogens, can grow over a range of external NaCl concentrations from 1.2 to 2.9 M and utilize methanol, trimethylamine, and dimethyl sulfide as substrates for methanogenesis. It produces the osmolytes glycine betaine, beta-glutamine, and N-acetyl-beta-lysine with increasing external NaCl, but the relative ratio of these zwitterions depends primarily on the methanogenic substrate and less on the external osmolarity. When the cells are grown on methanol in defined medium, accumulation of glycine betaine predominates over the other zwitterionic solutes. The cells also synthesized a carbohydrate which was not detected in cells grown on trimethylamine. This negatively charged compound, identified as alpha-glucosylglycerate from the C and H chemical shifts, does not act as an osmoregulatory solute in the salt range 1.4 to 2.7 M in this methanogen as evidenced by its invariant intracellular concentration. CH(3)OH-pulse/CH(3)OH-chase experiments were used to determine half-lifes for these organic solute pools in the cells. l-alpha-Glutamate showed a rapid loss of heavy isotope, indicating that l-alpha-glutamate functions as a biosynthetic intermediate in these cells. Measurable turnover rates for both beta-glutamine, which acts as an osmolyte, and alpha-glucosylglycerate suggest that they function as metabolic intermediates as well. Molecules which function solely as osmolytes (glycine betaine and N-acetyl-beta-lysine) showed a slower turnover consistent with their roles as osmotic solutes in Methanohalophilus strain FDF1.     

Glycine betaine and potassium ion are the major compatible solutes in the extremely halophilic methanogen Methanohalophilus strain Z7302.

Methanohalophilus strain Z7302 was previously isolated from a hypersaline environment and grows over a range of NaCl concentrations from 1.7 to 4.4 M. We examined the relationships between cell growth rate, cell volume, and intracellular solute concentrations with increasing salinity. This extremely halophilic methanogen synthesized three zwitterionic compounds, beta-glutamine, N epsilon-acetyl-beta-lysine, and glycine betaine, and also accumulated potassium ion as compatible solutes to balance the external and internal osmotic pressures. Potassium and glycine betaine were the predominant compatible solutes when Methanohalophilus strain Z7302 was grown at high external NaCl concentrations and approached intracellular levels of 3 and 4 M, respectively.     

Glycine betaine transport in the obligate halophilic archaeon Methanohalophilus portucalensis

Transport of the osmoprotectant glycine betaine was investigated using the glycine betaine-synthesizing microbe Methanohalophilus portucalensis (strain FDF1), since solute uptake for this class of obligate halophilic methanogenic Archaea has not been examined. Betaine uptake followed a Michaelis-Menten relationship, with an observed K(t) of 23 microM and a V(max) of 8 nmol per min per mg of protein. The transport system was highly specific for betaine: choline, proline, and dimethylglycine did not significantly compete for [(14)C]betaine uptake. The proton-conducting uncoupler 2, 4-dinitrophenol and the ATPase inhibitor N, N-dicyclohexylcarbodiimide both inhibited glycine betaine uptake. Growth of cells in the presence of 500 microM betaine resulted in faster cell growth due to the suppression of the de novo synthesis of the other compatible solutes, alpha-glutamate, beta-glutamine, and N(epsilon)-acetyl-beta-lysine. These investigations demonstrate that this model halophilic methanogen, M. portucalensis strain FDF1, possesses a high-affinity and highly specific betaine transport system that allows it to accumulate this osmoprotectant from the environment in lieu of synthesizing this or other osmoprotectants under high-salt growth conditions.     

Regulatory Factors Associated with Synthesis of the Osmolyte Glycine Betaine in the Halophilic Methanoarchaeon Methanohalophilus portucalensis

The halophilic methanoarchaeon Methanohalophilus portucalensis can synthesize de novo and accumulate β-glutamine, N-acetyl-β-lysine, and glycine betaine (betaine) as compatible solutes (osmolytes) when grown at elevated salt concentrations. Both in vivo and in vitro betaine formation assays in this study confirmed previous nuclear magnetic resonance ¹³C-labelling studies showing that the de novo synthesis of betaine proceeded from glycine, sarcosine, and dimethylglycine to form betaine through threefold methylation. Exogenous sarcosine (1 mM) effectively suppressed the intracellular accumulation of betaine, and a higher level of sarcosine accumulation was accompanied by a lower level of betaine synthesis. Exogenous dimethylglycine has an effect similar to that of betaine addition, which increased the intracellular pool of betaine and suppressed the levels of N-acetyl-β-lysine and β-glutamine. Both in vivo and in vitro betaine formation assays with glycine as the substrate showed only sarcosine and betaine, but no dimethylglycine. Dimethylglycine was detected only when it was added as a substrate in in vitro assays. A high level of potassium (400 mM and above) was necessary for betaine formation in vitro. Interestingly, no methylamines were detected without the addition of KCl. Also, high levels of NaCl and LiCl (800 mM) favored sarcosine accumulation, while a lower level (400 mM) favored betaine synthesis. The above observations indicate that a high sarcosine level suppressed multiple methylation while dimethylglycine was rapidly converted to betaine. Also, high levels of potassium led to greater amounts of betaine, while lower levels of potassium led to greater amounts of sarcosine. This finding suggests that the intracellular levels of both sarcosine and potassium are associated with the regulation of betaine synthesis in M. portucalensis.     

Effects of Osmolyte Precursors on the Distribution of Compatible Solutes in Methanohalophilus portucalensis

The halophilic methanogen Methanohalophilus portucalensis synthesizes three distinct zwitterions, (beta)-glutamine, N(sup(epsilon))-acetyl-(beta)-lysine (NA(beta)Lys), and glycine betaine, as osmolytes when it is grown at high concentrations of external NaCl. The selective distribution of these three species was determined by growing cells in the presence of osmolyte biosynthetic precursors. Glycine betaine is formed by the stepwise methylation of glycine. Exogenous glycine (10 mM) and sarcosine (10 mM), although internalized, do not bias the cells to accumulate any more betaine. However, exogenous N,N-dimethylglycine (10 mM) is available to the appropriate methyltransferase and the betaine generated from it suppresses the synthesis of other osmolytes. Precursors of the two zwitterionic (beta)-amino acids ((beta)-glutamate for (beta)-glutamine and (alpha)-lysine and diaminopimelate for NA(beta)Lys) have only small effects on (beta)-amino acid accumulation. The largest effect is provided by L-(alpha)-glutamine, suggesting that nitrogen assimilation is a key factor in osmolyte distribution.     

Utilization of phosphocholine from extracellular complex polysaccharide as a source of cytoplasmic choline derivatives in Penicillium fellutanum.

Penicillium fellutanum produces a phosphorylated, choline-containing extracellular polysaccharide, peptidophosphogalactomannan (pP(x)GM) [where x is the number of phosphodiester residues]). The 13C-methyl-labeled pP(x)GM ([methyl-13C]pP(x)GM) was prepared from the cultures supplemented with L-[methyl-13C]methionine and was used as a probe to monitor the fate of phosphocholine in this polymer. The addition of [methyl-13C]pP(x)GM to growing cultures in low-phosphate medium resulted in the disappearance within 5 days of [methyl-13C]phosphocholine and N,N'-dimethylphosphoethanolamine from the added [methyl-13C]pP(x)GM. Two 13C-methyl-enriched cytoplasmic solutes, choline-O-sulfate and glycine betaine, were found in mycelial extracts, suggesting that phosphocholine-containing extracellular pP(x)GM of P. fellutanum is a precursor of intracellular choline-O-sulfate and glycine betaine. The mycelia cultured in low-phosphate (2 mM) medium contained glycine betaine and 1.5-fold more choline-O-sulfate than those grown in high-phosphate (20 mM) medium. The high levels of extracellular nonspecific phosphocholine:phosphocholine hydrolase and acid phosphomonoesterase observed in the low-phosphate culture medium are likely related to the release of phosphocholine from pP(x)GM and hydrolysis of phosphocholine, respectively. These results suggest that extracellular pP(x)GM of P. fellutanum provides phosphate needed as the environment becomes depleted of this nutrient. Choline, in excess of that needed immediately, is stored in the cytoplasm in forms that can be reutilized.     

13C NMR study of the interrelation between synthesis and uptake of compatible solutes in two moderately halophilic eubacteria. Bacterium Ba1 and Vibro costicola

The synthesis and uptake of intracellular organic osmolytes (compatible solutes) were studied with the aid of natural abundance 13C NMR spectroscopy in two unrelated, moderately halophilic eubacteria: Ba1 and Vibrio costicola. In minimal media containing 1 M NaCl, both microorganisms synthesized the cyclic amino acid, 1,4,5,6-tetrahydro-2-methyl-4-pyrimidinecarboxylic acid (trivial name, ectoine) as the predominant compatible solute, provided that no glycine betaine was present in the growth medium. When, however, the minimal medium was supplemented with glycine betaine or the latter was a component of a complex medium, it was transported into the cells and the accumulating glycine betaine replaced the ectoine. In Ba1, grown in a defined medium containing glucose as the single carbon source, ectoine could only be detected if the NaCl concentration in the medium was higher than 0.6 M; the ectoine content increased with the external salt concentration. At NaCl concentrations below 0.6 M, alpha,alpha-trehalose was the major organic osmolyte. The concentration of ectoine reached its peak during the exponential phase and declined subsequently. In contrast, the accumulation of glycine betaine continued during the stationary phase. The results presented here indicate that, at least in the two microorganisms studied, ectoine plays an important role in haloadaptation.     

Influence of interactions between temperature,ferric ammonium citrate and glycine betaine on the growth of Listeria monocytogenes in a defined medium

AIMS: To investigate interactions, if any, between temperature, ferric ammonium citrate and glycine betaine on the growth of Listeria monocytogenes in modified Pine's medium (Pine et al. 1989). METHODS AND RESULTS: Modified Pine's medium containing 0, 0.044, 0.088 or 0.176 g l(-1) ferric ammonium citrate, and 0 or 1 mM glycine betaine, was inoculated with each of two L. monocytogenes strains and incubated at 4, 25 or 37 degrees C. The optical density at 600 nm, and cell numbers, were determined at appropriate time intervals. At 4 degrees C, but not other temperatures, increasing ferric ammonium citrate resulted in improved growth in the absence, but not the presence, of glycine betaine. The presence of glycine betaine was inhibitory at 25 and 37 degrees C, but not at 4 degrees C. CONCLUSIONS: Interactions affecting the growth kinetics of L. monocytogenes were apparent between the parameters investigated. SIGNIFICANCE AND IMPACT OF THE STUDY: Limitations on the use of modified Pine's medium, and the significance of iron metabolism at lower temperatures, were revealed.     

Variations in the response of salt-stressed Rhizobium strains to betaines

A total of 15 rhizobial strains representing Rhizobium meliloti, Rhizobium japonicum, Rhizobium trifolii, Rhizobium leguminosarum, Rhizobium sp. (Sesbania rostrata) and Rhizobium sp. (Hedysarum coronarium), were studied with regard to growth rate under salt stress in defined liquid media. In the presence of inhibitory concentrations of NaCl, enhancement of growth resulting from added glycine betaine was observed for R. meliloti strains and Rhizobium sp. (Hedysarum coronarium) but not for other Rhizobium species. The concentration of glycine betaine required for maximal growth stimulation was very low (1 mM) in comparison with the osmolarity of the medium. The stimulation was shown to be independent of any specific solutes. Other related compounds like proline betaine, carnitine, choline, -butyrobetaine and pipecolate betaine were also effective compounds in restoring the growth rate of cells grown in medium of elevated osmolarity. High rate of glycine betaine uptake was demonstrated in R. meliloti cells grown in media of increased osmotic strength. The intracellular concentration of this solute was found to be 308 mM in 0.3 M NaCl-grown cells and 17 times lower in minimal medium-grown cells. Glycine betaine was used for growth under conditions of low osmolarity but could not serve as sole carbon or nitrogen source in medium of increased osmotic strength. Experiments with [¹⁴C]glycine betaine showed that this molecule was not metabolized by cells subjected to osmotic stress, whereas it was rapidly converted to dimethylglycine, sarcosine and glycine in minimal medium-grown cells.Abbreviations LAS lactate-aspartate-salts - LGS lactate-glutamate-salts - LS lactate-succinate - MSY mannitol-salts-yeast - YLS yeast-lactate-succinate     

The effects of osmotic upshock on the intracellular solute pools of Bacillus subtilis

The effects of hypersaline treatment (osmotic upshock) on solute accumulation have been studied in the Gram-positive bacterium Bacillus subtilis. Natural abundance 13C NMR spectroscopy studies revealed only proline as a major organic osmoticum in cells grown in defined medium (no exogenous organic solutes) and this finding was confirmed by amino acid analysis. Intracellular concentrations of both K+ and proline rose markedly after osmotic upshock. K+ influx from the medium was rapid (less than 1 h) but proline synthesis was a slower process (5-9 h). Proline synthesis appeared to be dependent on the prior accumulation of K+ and it is possible that K+ serves in some manner as the signal for increased proline synthesis. In cells upshocked in medium enriched in glycine betaine the endogenous synthesis of proline was repressed and glycine betaine served as the sole organic osmoticum. K+ was also accumulated under these conditions.     

Cellular Choline and Glycine Betaine Pools Impact Osmoprotection and Phospholipase C Production in Pseudomonas aeruginosa

Choline is abundantly produced by eukaryotes and plays an important role as a precursor of the osmoprotectant glycine betaine. In Pseudomonas aeruginosa, glycine betaine has additional roles as a nutrient source and an inducer of the hemolytic phospholipase C, PlcH. The multiple functions for glycine betaine suggested that the cytoplasmic pool of glycine betaine is regulated in P. aeruginosa. We used (13)C nuclear magnetic resonance ((13)C-NMR) to demonstrate that P. aeruginosa maintains both choline and glycine betaine pools under a variety of conditions, in contrast to the transient glycine betaine pool reported for most bacteria. We were able to experimentally manipulate the choline and glycine betaine pools by overexpression of the cognate catabolic genes. Depletion of either the choline or glycine betaine pool reduced phospholipase production, a result unexpected for choline depletion. Depletion of the glycine betaine pool, but not the choline pool, inhibited growth under conditions of high salt with glucose as the primary carbon source. Depletion of the choline pool inhibited growth under high-salt conditions with choline as the sole carbon source, suggesting a role for the choline pool under these conditions. Here we have described the presence of a choline pool in P. aeruginosa and other pseudomonads that, with the glycine betaine pool, regulates osmoprotection and phospholipase production and impacts growth under high-salt conditions. These findings suggest that the levels of both pools are actively maintained and that perturbation of either pool impacts P. aeruginosa physiology.     

Utilization of osmoprotective compounds by hybridoma cells exposed to hyperosmotic stress

A search was undertaken for osmoprotective compounds for mouse hybridoma cell line 6H11 grown in culture. When the osmolality of the growth medium was increased above the normal osmolality of 330 mOsmol/kg, growth rates were decreased in a dose-dependent fashion, reaching zero when the osmolality of the medium reached approx. 435 mOsmol/kg through the addition of KCl (60 mM), or 510 mOsmol/kg through the addition of NaCl (100 mM), or sucrose (175 mM). For NaCl or sucrose-stressed cultures, the inclusion of glycine betaine, sarcosine, proline, glycine, or asparagine in the growth medium gave a moderate to strong osmoprotective effect, measured as the ability of these compounds to enhance cell growth rates under hyperosmotic conditions. Inclusion of dimethylglycine may also give a strong osmoprotective effect under these stress conditions.In KCl-stressed cell cultures, addition of glycine betaine, sarcosine, or dimethylglycine gave strong osmoprotective effects. Of 38 compounds tested during NaCl stress, 7 gave weak osmoprotective effects and 25 gave no osmoprotective effect. The osmoprotective compounds accumulated inside the stressed cells. Accumulation was completed after 4 to 8 h, reaching intracellular concentrations of approx. 0.27 pmol/cell, or 0.15 M, in NaCl stressed cells (100 mM NaCl added).Glycine betaine, dimethylglycine, and sarcosine accumulation was observed only when these protectants were included in the medium. For all osmoprotectants, a growth medium concentration between 5 and 30 mM gave the maximal protective effect, with the exception of dimethylglycine, for which the optimum concentration was approx. 65 mM. Osmoprotective effects obtained with glycine, sarcosine, dimethylglycine, and glycine betaine, indicate that the more methylated compounds are the most effective protectants.The cellular content of glycine betaine and the glycine betaine uptake rate increased with medium osmolality in a linear fashion. Glycine betaine uptake was described by a model comprising a saturable component obeying Michaelis-Menten kinetics and a nonsaturable component. K(m) and V(max) for glycine betaine uptake were determined at 420 mOsmol/kg (50 mM NaCl added) and 510 mOsmol/kg (100 mM NaCl added). A K(m) value of approx. 2.5 mM was obtained at both medium osmolalities, while V(max) increased from 0.010 pmol/cell . h to 0.018 pmol/cell . h as the osmolality of the growth medium was increased, indicating an effect of medium osmolality on the maximal rate of transport rather than on the affinity of the transporters for glycine betaine. Hybridoma cells were not able to utilize the glycine betaine precursors choline or glycine betaine aldehyde for osmoprotection, suggesting that the cells lack part, or all, of the choline-glycine betaine pathway or the appropriate uptake mechanism.The uptake rate for glycine in NaCl-stressed hybridoma cells was approx. four times higher than the uptake rate for glycine betaine. Furthermore, if equimolar amounts of glycine betaine, glycine, sarcosine, and proline were simultaneously added to NaCl-stressed cell cultures, the intracellular concentrations of glycine, proline, and sarcosine were significantly higher than the concentration of glycine betaine.A 40% increase in hybridoma cell volume was observed when the growth medium osmolality was increased from 300 to 520 mOsmol/kg. (c) 1994 John Wiley & Sons, Inc.     

Osmoregulation in Agrobacterium tumefaciens: accumulation of a novel disaccharide is controlled by osmotic strength and glycine betaine.

We have investigated the mechanism of osmotic stress adaptation (osmoregulation) in Agrobacterium tumefaciens biotype I (salt-tolerant) and biotype II (salt-sensitive) strains. Using natural-abundance 13C nuclear magnetic resonance spectroscopy, we identified all organic solutes that accumulated to significant levels in osmotically stressed cultures. When stressed, biotype I strains (C58, NT1, and A348) accumulated glutamate and a novel disaccharide, beta-fructofuranosyl-alpha-mannopyranoside, commonly known as mannosucrose. In the salt-sensitive biotype II strain K84, glutamate was observed but mannosucrose was not. We speculate that mannosucrose confers the extra osmotic tolerance observed in the biotype I strains. In addition to identifying the osmoregulated solutes that this species synthesizes, we investigated the ability of A. tumefaciens to utilize the powerful osmotic stress protectant glycine betaine when it is supplied in the medium. Results from growth experiments, nuclear magnetic resonance spectroscopy, and a 14C labeling experiment demonstrated that in the absence of osmotic stress, glycine betaine was metabolized, while in stressed cultures, glycine betaine accumulated intracellularly and conferred enhanced osmotic stress tolerance. Furthermore, when glycine betaine was taken up in stressed cells, its accumulation caused the intracellular concentration of mannosucrose to drop significantly. The possible role of osmoregulation of A. tumefaciens in the transformation of plants is discussed.     

Identification of glycine betaine as compatible solute in Synechococcus sp. WH8102 and characterization of its N-methyltransferase genes involved in betaine synthesis

Biosynthesis of glycine betaine from simple carbon sources as compatible solute is rare among aerobic heterotrophic eubacteria, and appears to be almost exclusive to the non-halophilic and slightly halophilic phototrophic cyanobacteria. Although Synechococcus sp. WH8102 (CCMP2370), a unicellular marine cyanobacterium, could grow up to additional 2.5% (w/v) NaCl in SN medium, natural abundance ¹³C nuclear magnetic resonance spectroscopy identified glycine betaine as its major compatible solute. Intracellular glycine betaine concentrations were dependent on the osmolarity of the growth medium over the range up to additional 2% NaCl in SN medium, increasing from 6.8 ± 1.5 to 62.3 ± 5.5 mg/g dw. The ORFs SYNW1914 and SYNW1913 from Synechococcus sp. WH8102 were found as the homologous genes coding for glycine sarcosine N-methyltransferase and sarcosine dimethylglycine N-methyltransferase, heterologously over-expressed respectively as soluble fraction in Escherichia coli BL21(DE3)pLysS and purified by Ni-NTA His•bind resins. Their substrate specificities and the values of the kinetic parameters were determined by TLC and ¹H NMR spectroscopy. RT-PCR analysis revealed that the two ORFs were both transcribed in cells of Synechococcus sp. WH8102 growing in SN medium without additional NaCl, which confirmed the pathway of de novo synthesizing betaine from glycine existing in these marine cyanobacteria.