INTRODUCTION

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The lactic acid bacterium (LAB) Tetragenococcus halophila is a tetrad-forming gram-positive coccus. Formerly known as Pediococcus halophilus, the bacterium was reclassified in the genus Tetragenococcus, based on 16S rRNA studies (5). T. halophila, the type species of this new genus, was shown to be from a distinct line of descent quite separate from those of both aerococci and pediococci (5). Recently, the existence of a second species, Tetragenococcus muriaticus, has been proposed (30). This bacterium, isolated from traditionally fermented Japanese fish sauce, is closely related to the halotolerant species T. halophila and shows a closer phylogenetic relationship to other LAB of the enterococci and lactobacilli (30).

T. halophila contributes to the biopreservation of vegetable products, such as soybeans during the manufacturing of soy sauce, a well-known condiment in southeast Asia, China, and Japan. The bacterium grows during brine fermentation, where the salt concentration ranges from 12 to 26% (26). T. halophila is also associated with other foods processed under reduced water activities, such as cured anchovies, where it becomes the dominant bacterium at the end of the curing process; this organism can grow under both aerobic and anaerobic conditions (36).

The Tetragenococcus genus like other genera of gram-positive moderately halophilic bacteria (Halobacillus, Marinicoccus, Salinicoccus, and Nesterenkonia) includes only species requiring 0.5 to 30% salt, with an NaCl optimum of 10% (35). Raising the salt concentration of the medium presumably increases osmotic stress, which requires bacteria from various ecological niches to cope with the high and often changing salinity of their environment. The moderately halophilic bacteria, similar to all other microorganisms, need to maintain an osmotic equilibrium between inside and outside of the cells. They can achieve osmotic balance by the accumulation of salts and/or organic molecules (35). Among this heterogenous group of bacteria, T. halophila can tolerate high salt concentrations, which suggests that it has a high osmotic adjustment capacity in order to maintain positive cell turgor. Osmoregulation has been studied extensively in nonhalophilic bacteria such as Escherichia coli, Sinorhizobium meliloti, and Bacillus subtilis (1, 6, 7, 17, 32, 33). Unlike the halophiles, they do not have a strict sodium requirement. Both halophilic and nonhalophilic bacteria have evolved mechanisms that enable them to adapt to high salinity. They protect themselves against deleterious hyperosmotic injury by the uptake or synthesis of a limited number of compounds, termed compatible solutes (7, 17). These are not inhibitory to most cellular processes even at near molar concentrations and may even stabilize the native state of proteins and lipids (38). These compatible solutes include sugars and polyols such as trehalose and glycerol, amino acids such as glutamate and proline, and amino acid derivatives such as betaines and ectoines (7, 12, 17). In the LAB family, the identification and the role of compatible solutes have been investigated for Lactobacillus casei subsp. rhamnosus (10), Lactococcus lactis (22), and Lactobacillus plantarum (9, 18, 19). Glycine betaine is reported to serve as the major effective osmoprotectant in these bacteria. It is not synthesized de novo but accumulates from an exogenous supply. In LAB, all transport systems involved in glycine betaine uptake are not induced but appear to be activated by exposure of the cells to high osmotic pressure. Most of the bacteria studied, e.g., Escherichia coli and B. subtilis, can also accumulate glycine betaine through the conversion of its precursor, choline (6, 7, 17). This contrasts with the studied LAB, which do not convert choline to betaine (20, 22, 34). Carnitine has also been identified as a compatible solute in L. plantarum, where it can be accumulated simultaneously with glycine betaine (19).

Like other LAB, T. halophila is characterized by complex nutritional requirements, including a certain number of growth factors such as nicotinic acid, panthothenic acid, and biotin (5). Sakaguchi (28, 29) reported that T. halophila cannot grow in ordinary synthetic media for LAB but rather requires glycine betaine and carnitine as specific growth factors. However, no further investigations have been made to analyze to what extent uptake or synthesis of these osmolytes or both contribute to osmoprotection in T. halophila. To understand this phenomenon, we determined the nutritional requirements of this organism in a chemically defined medium and show that betaines are not required to support growth of T. halophila. In this article, we also report on the role of glycine betaine, carnitine, and choline in the osmoregulation of T. halophila. Data on the accumulation and transformation of each in the cells are presented and provide evidence that T. halophila is the first LAB which is able to convert choline into glycine betaine under aerobic conditions to be identified.

	MATERIALS AND METHODS

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Bacteria and growth conditions. T. halophila ATCC 33315 was obtained from the American Type Culture Collection (Manassas, Va.). Cells were grown aerobically without agitation at 30°C. Anaerobic culture conditions were obtained by using the technique described by Bryand (3). Growth was monitored by optical density measurements at 600 nm (OD₆₀₀) of appropriately diluted cultures.

Extraction of intracellular solutes. T. halophila was grown in DM or MRS. Cells were harvested during exponential growth by centrifugation and washed with isotonic medium. The cell pellet was extracted at least twice with 80% (vol/vol) ethanol, under vigorous magnetic stirring, at room temperature, for 30 min. After centrifugation, the supernatants (ethanol-soluble fraction [ESF]) were pooled and evaporated to dryness under reduced pressure at 40°C. The dried residue was finally dissolved in a minimal volume of distilled water and stored in the freezer at 20°C until use for further analysis.

Determination of intracellular potassium and sodium contents. For the determination of potassium content, samples (10 ml) of a mid-log-phase culture were harvested by centrifugation at 10,000 × g for 10 min and washed with 10 ml of potassium-free isotonic DM. Cells were resuspended in 1 ml of perchloric acid (5%) and extracted for 12 h at 4°C. Extracts were diluted 10 times in a 0.01% CsCl solution and centrifuged at 15,000 × g to remove the cellular debris. The K⁺ concentrations were measured using an atomic absorption spectrophotometer at 766.5 nm. The same method was used for the determination of intracellular concentrations of sodium, except that cells were washed three times with an isotonic solution of either maltose or KCl.

Determination of glutamate content. The glutamate content of cell extracts was measured routinely with the corresponding Boehringer (Meylan, France) assay kit, according to the specifications of the supplier.

Chromatographic analysis and NMR spectroscopy. Chromatographic and electrophoretic analyses of the ethanol-soluble cell extracts were performed as described previously (13). The natural-abundance ¹³C-nuclear magnetic resonance (NMR) spectra were recorded in the pulsed-Fourier transform mode at an operational frequency of 75.4 MHz as described previously (32). The ESF was evaporated to dryness, and the residues were dissolved in 1 ml of D₂O.

Transport assays. Cells grown in DM with or without osmoprotectants were centrifuged (5,000 × g for 10 min), washed twice with an isotonic medium, resuspended to an OD₆₀₀ of 5, and maintained at room temperature for 30 min. Osmoprotectant uptake assays were performed as described previously (12), using [methyl-¹⁴C]glycine betaine (2.07 GBq mM¹), [methyl-¹⁴C]choline (2.07 GBq mM¹), DL-[methyl-¹⁴C]carnitine (0.22 GBq mM¹), L-[methyl-¹⁴C]carnitine (1.86 GBq mM¹), and D-[methyl-¹⁴C]carnitine (0.22 GBq mM¹), each at a final concentration of 10 µM in 400 µl of bacterial suspension. [methyl-¹⁴C]glycine betaine was prepared from [methyl-¹⁴C]choline as described by Ikuta et al. (11). D-[methyl-¹⁴C]carnitine was prepared from DL-[methyl-¹⁴C]carnitine as described previously (14).

Determination of the intracellular osmoprotectant levels. Cells were subcultured in DM containing 0 to 2.5 M NaCl, 2 mM [methyl-¹⁴C]glycine betaine, [methyl-¹⁴C]choline, L-[methyl-¹⁴C]carnitine, or D-[methyl-¹⁴C]carnitine. After two to five generations, 2 ml of cell culture was harvested by centrifugation and washed twice with carbon-free DM containing the same NaCl concentration as in the growth media. After extraction with 80% ethanol, the radioactive composition of the ESF was analyzed by paper chromatography and/or electrophoresis (13). The radioactive molecules were visualized using the Packard PhosphorImager. The radioactivity of the ethanol-insoluble fraction (EIF) and CO₂ was also determined.

Chemicals. The radiolabeled compounds [methyl-¹⁴C]choline and DL-[methyl-¹⁴C]carnitine were obtained from NEN-Dupont de Nemours. All other chemicals were of reagent grade and were obtained from Sigma (L'Isle d'Abeau Chesnes, France).

	RESULTS

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Growth of T. halophila at high salinity. T. halophila was cultured in MRS broth, a complex medium routinely used to cultivate LAB. T. halophila grew in MRS medium containing up to 3.2 M NaCl (Table 1). The growth rate (µ) increased from 0.1 generation h¹ in the absence of sodium chloride to reach a maximal value of 0.16 generation h¹ in medium supplemented with 0.6 M NaCl. Growth was progressively slower as the NaCl concentration increased from 1 to 3.2 M (Table 1). The growth yield was also improved by the addition of NaCl to the culture media, with a maximal OD₆₀₀ of 3.6 obtained at 1 M NaCl. ¹³C-NMR analysis of cells grown in MRS medium without or with NaCl (1.5 M) were performed in order to identify the organic solutes accumulated by T. halophila subjected to high salinity. Glycine betaine and carnitine were identified (Fig. 1). These two well-known osmoprotectants were accumulated by T. halophila at high as well as at low salinities (data not shown). Peaks attributed to lactic acid were also detected at low and high salinities.

View larger version (14K): [in this window] [in a new window]   FIG. 1.   13C-NMR spectra of ethanolic extracts of T. halophila cells grown in MRS medium supplemented with 1.5 M NaCl. Resonances due to glycine betaine (b), carnitine (ca), and lactate (l) are indicated.

Effect of exogenous trimethylammonium compounds on the growth of T. halophila subjected to various NaCl concentrations. Previous attempts to grow T. halophila in DM failed (29). Here, we observed that T. halophila grew in DM containing the nutrients which commonly compose minimal media used to cultivate LAB (Fig. 2). In the absence of osmoprotectant, T. halophila showed optimal growth at 0.4 to 0.8 M NaCl, with a maximum at 0.5 M NaCl (µ = 0.094 generation h¹ and OD₆₀₀ = 0.67; Fig. 2).

View larger version (19K): [in this window] [in a new window]   FIG. 2.   Effect of varied osmolarity on the growth rate (A) and growth yield (B) of T. halophila cells growing in DM in the absence of osmoprotectants () or the presence of 2 mM glycine betaine (), 2 mM DL-carnitine (), or 2 mM choline ().

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View larger version (17K): [in this window] [in a new window]   FIG. 3.   Glycine betaine, DL-carnitine, and choline improve the growth yield of T. halophila at high osmolarity. T. halophila was grown in DM with 1 M NaCl in the presence of various concentrations of DL-carnitine (), glycine betaine (), and choline (). The cells were grown in 5 ml of medium, without shaking, at 30°C, and the growth yield of each culture was monitored by measurements of OD600 after 56 h of incubation.

Transport characteristics and effect of osmolarity on uptake of compatible solutes. Transport experiments were performed to determine whether the uptake of glycine betaine, carnitine, and choline (10 µM) was regulated by the NaCl concentration of the medium. Cells were grown in DM lacking NaCl, washed, and resuspended in the same medium without or with added NaCl (from 0.5 to 2 M). The capacities of T. halophila to transport glycine betaine and choline increased slightly from 3.2 and 0.14 nmol/min/mg (dry weight) in DM without NaCl to 4.3 and 0.33 nmol/min/mg (dry weight), respectively, when the cells were shocked with various increased concentrations of NaCl. The results are the means of three independent experiments, and the standard errors did not exceed 5%. These results suggest that rates of glycine betaine and choline uptake are osmotically modulated. On the other hand, the rates of carnitine uptake were similar for all the salinities tested (2 to 2.5 nmol/min/mg [dry weight]).

Identification of the intracellular solutes of osmotically stressed T. halophila. Natural-abundance ¹³C-NMR analysis was performed to identify the organic osmolytes which might be accumulated in stressed cultures of T. halophila. Cells of T. halophila were grown for 48 h in high-salinity DM in the presence of 2 mM glycine betaine, DL-carnitine, or choline or in the absence of osmoprotectants. Specific signals from glutamate, proline, and aspartate were clearly identified in the spectrum from cells grown in DM with 1 M NaCl (Fig. 4A). Glutamate appeared to be the main organic osmolyte produced in these cells. The ¹³C-NMR tracings obtained from cells grown in DM with 1 M NaCl and 2 mM choline showed major signals attributed to glycine betaine and minor peaks arising from choline, glutamate, and proline (Fig. 4B). These data indicate that T. halophila oxidized choline into betaine. Hence choline serves as a precursor for the production of glycine betaine.

View larger version (13K): [in this window] [in a new window]   FIG. 4.   13C-NMR spectra of ethanolic extracts of T. halophila cells grown in DM supplemented with 1 M NaCl in the absence of osmoprotectants (A) or the presence of 2 mM choline (B), 2 mM glycine betaine (C), or 2 mM DL-carnitine (D). The signals were identified from spectra obtained with authentic compounds and represent glutamate (g), aspartate (a), proline (p), choline (c), glycine betaine (b), and carnitine (ca).

Osmoregulated accumulation of quaternary ammonium compounds in T. halophila. Since ¹³C-NMR can detect the main representative accumulated compounds only qualitatively, the intracellular amounts of D-carnitine, L-carnitine, and glycine betaine accumulated by T. halophila cells cultivated at various salinities were measured. When T. halophila was grown for two to five generations in the presence of 2 mM D-[¹⁴C]carnitine, L-[¹⁴C]carnitine, or [¹⁴C]glycine betaine in DM with different concentrations of NaCl, the radioactive material which disappeared from the medium was recovered in the ESF. No radioactivity was detected in either the EIF or in the CO₂. Chromatographic and electrophoresis analysis of the ESF revealed that the molecule provided accounted for the entire radioactivity of this fraction. Intracellular quantities of glycine betaine, D-carnitine, or L-carnitine increased, but in a nonlinear fashion, when the salt concentration of the medium was raised (Fig. 5). From 0 to 1 M NaCl, the intracellular levels of these betaines increased slightly, by 1.3- to 1.7-fold. Above 1 M NaCl, significant increases in the concentrations of the accumulated solutes were observed. The absolute amounts, however, were quite similar and reached maxima of 3,120, 3,600, and 3,250 nmol/mg (dry weight) for growth in DM with 2.5 M NaCl and glycine betaine, L-carnitine, or D-carnitine respectively. Interestingly, the intracellular concentrations of [¹⁴C]glycine betaine, L-[¹⁴C]carnitine, and D-[¹⁴C]carnitine in stressed cells were 4.7-, 5.3-, and 4.2-fold higher, respectively, than the intracellular concentrations in cells cultivated in DM.

View larger version (19K): [in this window] [in a new window]   FIG. 5.   Effect of the osmotic strength of growth medium on the accumulation of compatible solutes by T. halophila. Cells were grown for two to five generations in DM containing the indicated NaCl concentrations, in the presence of 2 mM [14C]glycine betaine (), L-[14C]carnitine (), or D-[14C]carnitine (). Cells were harvested, and the ethanol-soluble extracts were subjected to paper chromatography and electrophoresis. Radioactivity was recovered only in carnitine or glycine betaine spots and was measured by scintillation counting.

View larger version (22K): [in this window] [in a new window]   FIG. 6.   Conversion of choline to betaine in response to increasing salinity. Paper electrophoresis was used for separation, signals corresponding to choline (hatched bar) and glycine betaine (solid bar) were analyzed by phosphorimager, and the radioactivity corresponding to each spot was determined by scintillation counting. , glycine betaine/choline (GB/Cho) ratio.

Effect of glycine betaine and osmotic stress on intracellular potassium, sodium, and glutamate. (i) Accumulation of potassium is a primary event in the adaptation of many bacteria to hyperosmotic constraints (7). To establish whether the response of T. halophila to increased medium salinity involves the accumulation of potassium, the ion content of cytoplasmic extracts of exponentially growing T. halophila cells was analyzed by atomic absorption spectrophotometry. The steady-state potassium concentration of the cytoplasm increased from 460 to 550 nmol/mg (dry weight) when NaCl concentration was raised from 0 to 1.5 M (Fig. 7A). At 2 M NaCl the potassium content decreased slightly to reach 450 nmol/mg (dry weight), which was equivalent to that obtained in DM. When cells were grown in DM containing 0 to 1.5 M NaCl, the addition of 2 mM glycine betaine lowered the steady-state K⁺ concentrations (300 and 470 nmol/mg [dry weight] at low and high salinity, respectively) (Fig. 7A). In contrast, K⁺ content was increased to 630 nmol/mg (dry weight) in 2 M NaCl medium in the presence of glycine betaine.

View larger version (11K): [in this window] [in a new window]   FIG. 7.   Influence of elevated osmolarity, in the absence (open symbols) or presence (solid symbols) of glycine betaine, on the accumulation of potassium (A), glutamate (B), and sodium (C) by T. halophila.

(ii) In many bacteria, the glutamate level increases after osmotic shock to provide counter-ions for a strong increase in the K⁺ pool. Glutamate is also required to maintain the steady-state K⁺ level content (7, 32). In T. halophila, the level of glutamate increased from 47 nmol/mg (dry weight) at low salinity to reach 133 nmol/mg (dry weight) at high salinity (Fig. 7B). When glycine betaine was present in the growth media, the glutamate amount was maintained below 10 nmol/mg (dry weight) regardless of the NaCl concentration of the medium (Fig. 7B).

(iii) All moderately halophilic bacteria require a minimal concentration of Na⁺ for growth (35). In T. halophila optimal growth was obtained in DM with salinity ranging from 0.4 to 0.8 M NaCl. Thus the role of Na⁺ in the moderately halophilic behavior of this organism was studied. In the absence of glycine betaine, the intracellular amount of sodium was relatively high in DM (660 nmol/mg [dry weight]). Then, it decreased three- to fourfold when T. halophila was grown in a salinity range varying from 0.5 to 1 M NaCl. Over 1 M NaCl, the intracellular Na⁺ content increased linearly with increasing medium salinity, to reach a maximal level of 2,065 nmol/mg (dry weight) when the growth medium was amended with 2 M NaCl (Fig. 7C). In the presence of glycine betaine, the intracellular sodium level fluctuated between 150 and 320 nmol/mg (dry weight) in the medium with salinity ranging from 0 to 2 M NaCl. Carnitine and glycine betaine had the same effect on the intracellular Na⁺ concentration, which was estimated at 200 to 300 nmol/mg (dry weight) in a range of salinities varying from 0 to 2 M NaCl. Over a wide range of salinity, glycine betaine, like carnitine, maintained the intracellular Na⁺ concentration close to the level observed in the optimal-growth conditions and in the absence of betaines.

	DISCUSSION

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We analyzed the physiological osmoregulatory responses of the LAB T. halophila in DM. The effect of osmotic stress on growth was investigated in the presence of the osmoprotectants glycine betaine, carnitine, and choline. The present results show that T. halophila can grow in a chemically defined medium and did not require carnitine or glycine betaine for growth; these solutes have been previously described as specific growth factors for T. halophila cultured in DM (28, 29). In MRS medium and DM, T. halophila tolerates up to 3.2 and 1.6 M NaCl, respectively. The difference in bacterial osmotolerance levels in these two media could be due partly to the presence of a large amount of osmoprotectants in MRS broth and partly to the inability of T. halophila to synthesize efficient osmotically active cellular solutes when cultured in DM with elevated salinity. It was demonstrated by ¹³C-NMR that T. halophila accumulated only glycine betaine and carnitine as principal organic solutes when cells were grown in MRS without or with NaCl (1.5 M). It has been shown that the presence of glycine betaine and carnitine in MRS broth confers increased osmolarity tolerance to some LAB (10, 19). The addition of glycine betaine, carnitine, or choline to DM containing various NaCl concentrations allowed T. halophila to grow in a wide range of salinities close to that tolerated in MRS media. It is worth noting that glycine betaine and carnitine improved the growth of T. halophila over the whole range of salinities, even in DM lacking NaCl. The growth rate and the growth yield can be increased by adding osmoprotectant to the growth medium and/or by increasing the NaCl concentration up to 1 M NaCl. These observations are paradoxical since it is assumed that increasing the NaCl concentration generates an osmotic stress situation, of which the osmoprotectants alleviate the harmful effect. This supposes that T. halophila requires osmoprotectants for osmoregulatory purposes and osmoprotectants and sodium simultaneously to develop a moderately halophilic behavior. Similar observations have been made for Halomonas elongata, another moderately halophilic bacterium stimulated by glycine betaine and choline at all salinities, including suboptimal growth conditions (4). In contrast, glycine betaine and other osmoprotectants improve the growth of studied LAB only at high osmolarity, while at low osmolarity glycine betaine had an inhibitory effect on the growth of Lactococcus lactis (9, 20, 22).

Natural-abundance ¹³C-NMR spectroscopy indicated that glutamate was the main organic solute in the cytoplasmic solute pool of T. halophila when cells were grown in DM with 1 M NaCl added. The glutamate level increased two- to threefold when cells were cultured in DM with the NaCl concentration ranging from 0 to 2 M (Fig. 6B). NMR spectra also revealed minor peaks, which were attributed to proline and aspartate. All these amino acids could be accumulated by uptake from the medium and/or by biosynthesis. These solutes have also been found to be the main endogenous osmolytes accumulated by other LAB grown under hyperosmotic conditions (9, 22). Trehalose, which is accumulated by a large number of bacteria under osmotic stress (7, 17), was never detected in T. halophila, either at exponential or at stationary growth phases; this observation has also been reported for other LAB (19, 34). In contrast to most representatives of the moderately halophilic bacteria, for which ¹³C-NMR analysis led to the identification of ectoine and hydroxyectoine as the main endogenous organic compounds (25, 35, 37), T. halophila did not produce these compounds or any other potent compatible solute.

When glycine betaine or carnitine was present, it was preferentially accumulated and inhibited the accumulation of proline, aspartate, and glutamate. Carnitine or glycine betaine was accumulated in unmodified form by T. halophila at low and high salinities. Their intracellular levels were significantly stimulated (four- to fivefold) only when the salinity of the medium was raised from 1 to 2.5 M NaCl. These results suggest that cells are osmotically stressed at these salinities. On the other hand, the conspicious increase in the accumulated osmoprotectant at salt concentrations >1 M NaCl is probably linked to an activation of the transport of these betaines. Uptake and cross-competition experiments suggested that at least two transport systems operate in T. halophila: the first system transports glycine betaine, and the second transports all the betaines assayed. These uptake systems are not induced and are not activated, or slightly activated, by elevated salinity. The gram-positive model bacterium B. subtilis transports glycine betaine by three separate systems: OpuA, OpuC, and OpuD. Only the OpuC system displays a broad substrate specificity (17). Thus, the T. halophila glycine betaine transport systems are somewhat close to those characterized in B. subtilis but differ from the E. coli ProP and ProU systems, which can recognize all osmoprotectants assayed. Several nonhalophilic bacteria, including Pseudomonas, Agrobacterium, and Rhizobium species (21, 33) and certain halophilic bacteria such as H. elongata (4, 35), have the ability to use L-carnitine and glycine betaine as sole sources of carbon and nitrogen. Brevibacterium linens is able to convert L-carnitine into glycine betaine, which functions as an osmoprotectant in this bacterium, while B. subtilis and E. coli accumulated carnitine under hyperosmotic and aerobic conditions if supplied in the growth medium (14, 16, 21). T. halophila, like other LAB, cannot catabolize any of these compounds under aerobic growth conditions and hence accumulates them only for osmoregulatory purposes (9, 10, 19, 20, 22).

Among the assayed quaternary ammonium compounds, choline appears to be the least efficient for improving both growth yield and growth rate of T. halophila subjected to hyperosmotic constraint. The osmoprotective effect of choline in both gram-positive and gram-negative bacteria has been described (1, 2, 4, 6, 13, 27). In LAB that have been studied, data concerning osmoprotective properties of choline are contradictory. For example, depending on which L. plantarum strain was used, choline has been reported to have osmoprotective effects (9, 20). This solute was accumulated in unmodified form in osmotically stressed L. plantarum cells (9, 20). In Lactococcus lactis, choline did not improve the growth at high osmolarity but was accumulated when provided in the culture medium (34). To our knowledge, T. halophila is the first LAB which can convert choline into glycine betaine under aerobic growth conditions and accumulate glycine betaine during salt stress. Thus, the osmoprotective effect of choline appears to depend on its enzymatic conversion to glycine betaine. The glycine betaine/choline ratio increases from 3 at low salinity (0 to 0.5 M NaCl) to 5 at high salinity (1 to 2 M) which suggests that the choline-glycine betaine pathway is activated and/or induced by elevated salinity. T. halophila thus shares the ability to oxidize choline to glycine betaine for osmoprotective purposes with a number of nonhalophilic and halophilic bacteria (1, 2, 4, 6, 13, 27, 35).

Organic osmolytes are not the only efficient compounds for the adaptation of bacteria to hyperosmotic conditions. Potassium is also known to be a key ion for osmotic adaptation in many bacteria. In T. halophila, the steady-state intracellular concentration of K⁺ increases from 460 to 550 nmol/mg (dry weight) in DM with added NaCl from 0 to 1.5 M. Under these conditions, glycine betaine inhibits potassium accumulation by 10 to 35%. At >1.5 M NaCl, growth is highly affected and potassium content decreases to reach 450 nmol/mg (dry weight) at 2 M NaCl. Glycine betaine, which greatly improved growth under hyperosmotic conditions (2 M NaCl), allowed the cells to maintain the intracellular K⁺ concentration at 630 nmol/mg (dry weight). These results suggest that K⁺ is necessary for growth in media of varied salinities. Nevertheless, it does not seem to be essential in the response to osmotic changes in T. halophila, since (i) the apparent intracellular K⁺ concentration did not increase in correlation with increasing external NaCl concentration and (ii) the accumulation of glycine betaine does not significantly affect the steady-state intracellular concentration of potassium. The relatively small role of potassium in the achievement of osmotic balance has also been observed in other LAB and most moderately halophilic bacteria (9, 20, 35).

The common denominator for all moderately halophilic bacteria is their requirement for salt and their ability to tolerate high salt concentrations (35). In most cases, a minimum of Na⁺ is essential for growth. Thus, it was of interest to examine also the change in intracellular sodium concentration in T. halophila subjected to various salinities. In this bacterium, Na⁺ content was high in DM (660 nmol/mg [dry weight]) and decreased to about 200 nmol/mg (dry weight) in the optimal concentrations of NaCl (0.5 to 1 M). Over these salinities, the Na⁺ content increased 4- to 10-fold at high osmolarities. At 2 M NaCl, the intracellular concentration of the most prevalent organic anion (glutamate) did not exceed 10% of that of Na⁺, and ¹³C-NMR shows that T. halophila does not accumulate other negatively charged osmolytes to balance high levels of cytosolic Na⁺. In fact, the charge balance in T. halophila cells could be maintained by the accumulation of large amounts of Cl, as observed in Bacillus haloalkaliphilus and other moderately halophilic bacteria (35). Also, studies based on ²³Na-NMR have shown that about 40% of the intracellular Na⁺ is free and 60% of Na⁺ is bound to cell components in several moderately halophilic bacteria (35). Thus, T. halophila may not need a large amount of counter-ions equivalent to Na⁺ if most of these ions are associated with negative charge present on macromolecules. Most microorganisms keep their intracellular Na⁺ concentration much lower than the external Na⁺ concentrations (23, 35). However, T. halophila is not the only organism that does not attempt to keep Na⁺ out of its cytoplasm. For example, Haloanaerobium acetoethylicum, another fermentative halophilic bacterium, also accumulates high levels of Na⁺ (23). The nonavailability of organic osmoprotectants in the environment may force T. halophila to accumulate high Na⁺ concentrations. Moreover, the accumulation of salt probably represents an energetically cheaper option than the accumulation of organic osmolytes synthesized de novo. In some anaerobic halophilic bacteria, it was reported that the cells may maintain high intracellular salt (KCl in most cases) concentrations that are at least osmotically equivalent to the external salt (NaCl in most cases) concentrations (23). These bacteria require large amounts of substrates, which supply little energy; thus, the strategy of accumulating salt appears to require much less of the expensive substrate than does the production of organic osmotic solutes (23).

The inability to control the intracellular Na⁺ level on both sides of the optimal growth salinities may be involved in inhibiting the growth of T. halophila. The presence of betaine or carnitine allows this bacterium to maintain the Na⁺ concentration at a low level (200 to 300 nmol/mg [dry weight]) at all salinities. This suggests that T. halophila, in the presence of betaines, excludes Na⁺ to maintain a low concentration, even in an environment containing large amounts of sodium. In many moderately halophilic bacteria, the low intracellular sodium content is achieved by two possible mechanisms of Na⁺ extrusion: activity of an Na⁺/H⁺ antiporter and presence of a primary respiration-driven Na⁺ pump (35). An effect of betaine on the respiration-driven Na⁺ pump has previously been described for the moderately halophilic bacterium Halomonas israelensis (24, 31), where glycine betaine induced the stimulation of respiration at high salinities. A respiratory chain is lacking in LAB, but in streptococci and enterococci, two separate Na⁺ extrusion systems have been described (15), an Na⁺ ATPase and an Na⁺/H⁺ antiporter. These systems function as proton pumps in the membranes of these bacteria, which are unable to generate a large proton potential (15). Although no one doubts the ubiquitous distribution of these Na⁺ extrusion systems in LAB, if T. halophila possesses these systems, they are probably inhibited under high-salinity conditions, which could explain the high level of Na⁺ accumulated by the cells under high-salt treatment. In T. halophila, the accumulation of betaines allows physiological conditions that maintain the Na⁺ concentration inside the cells lower than that outside. The mechanisms by which betaines allow the cells to regulate the intracellular Na⁺ concentration are still unknown in T. halophila. Finally, as in most bacteria facing adverse hypersaline stress conditions, T. halophila cells have adopted the strategy of accumulating organic osmolytes through a process involving active transport of exogenous osmoprotectants (carnitine and glycine betaine) or through conversion of choline into glycine betaine. In T. halophila, these organic solutes are required not as growth factors but as osmotic and salt stabilizers. Thus, T. halophila has a moderately halophilic behavior provided that osmoprotectants are available in its environment.