Osmotic significance of glycerol accumulation in exponentially growing yeasts.

Natural-abundance 13C-nuclear magnetic resonance spectroscopy has shown glycerol to be the major osmotically significant low-molecular-weight solute in exponentially growing, salt-stressed cells of the yeasts Saccharomyces cerevisiae, Zygosaccharomyces rouxii, and Debaromyces hansenii. Measurement of the intracellular nonosmotic volume (i.e., the fraction of the cell that is osmotically unresponsive) by using the Boyle-van't Hoff relationship (for nonturgid cells, the osmotic volume is directly proportional to the reciprocal of the external osmotic pressure) showed that the nonosmotic volume represented up to 53% of the total cell volume; the highest values were recorded in media with maximum added NaCl. Determinations of intracellular glycerol levels with respect to cell osmotic volumes showed that increases in intracellular glycerol may counterbalance up to 95% of the external osmotic pressure due to added NaCl. The lack of other organic osmotica in 13C-nuclear magnetic resonance spectra indicates that inorganic ions may constitute the remaining component of intracellular osmotic pressure.     

Regulation of intracellular osmotic pressure during the initial stages of salt stress in a salt-tolerant yeast, Zygosaccharomyces rouxii.

The accumulation of glycerol and inorganic ions as it related to osmotic pressure, and the regulation of intracellular osmotic pressure in a salt-tolerant yeast, Zygosaccharomyces rouxii, were examined for several hours after salt stress. Intracellular contents of glycerol increased for up to 6 h in media supplemented with 1 M and 2 M NaCl and did not increase in medium containing 3 M NaCl. Intracellular contents of Na+ and Cl- reached a maximum value within 1 and 3 h, respectively, in all NaCl-containing media and increases were proportional to the concentration of NaCl in the medium. As glycerol was accumulated in cells, the intracellular contents of Na+ and Cl- gradually decreased in media containing 1 M and 2 M NaCl. After salt stress, cell volume decreased within 1 h and the original volume was re-established for 3 to 6 h in media with 1 M and 2 M NaCl but not in medium with 3 M NaCl. Intracellular concentrations of solutes, which were calculated from the total contents of glycerol and inorganic ions and the cell volume, became almost equivalent to the external osmotic pressure within 1 h after salt stress. Experiments using various inhibitors showed that a large amount of ATP was required not only for the synthesis and accumulation of glycerol but also for the exclusion of Na+ and Cl- from cells under salt-stressed conditions.     

Physiological responses of Zygosaccharomyces rouxii to osmotic stress

When cell suspensions of Zygosaccharomyces rouxii were subjected to osmotic shock with NaCl, the cell volume decreased sharply and plasmolysis was observed. The cell subsequently recovered and volumes similar to those of cells growing at the respective water activity (a_w) values were found. Cycloheximide prevented cell recovery, indicating the involvement of protein synthesis in the recovery process. The intracellular glycerol concentration of Z. rouxii incubated in the presence of [¹⁴C]glycerol increased from 13 to 96 mmol/l during the initial 20 min after an upshock from 0.998 a_w to 0.96 a_w. All the intracellular glycerol was labelled and therefore derived from the medium. Labelled glycerol was subsequently utilized and replaced by unlabelled glycerol produced by the cell within 90 min. The initial increase in glycerol concentration following the upshock was confirmed by ¹³C-nuclear magnetic resonance (NMR) spectroscopic studies of cell extracts. The combined dihydroxyacetone and dihydroxyacetone phosphate concentrations fluctuated during this period, whereas glycerol-3-phosphate initially increased and then remained constant. This indicates that the production of glycerol is regulated. Decreases in ATP and polyphosphate levels were observed following osmotic upshock and may reflect a greater demand for ATP during the period of adjustment to decreased a_w. The changes in cell volume and in ATP concentration following osmotic upshock may serve as osmoregulatory signals in Z. rouxii, as suggested previously for other microorganisms. Correspondence to: S. G. Kilian     

Osmotic adjustment and the accumulation of organic solutes in whole cells and protoplasts of Saccharomyces cerevisiae

In the presence of a suitable carbon source, whole cells and protoplasts of Saccharomyces cerevisiae synthesized glycerol as a compatible organic solute in response to increased external osmotic pressure. Boyle-van't Hoff plots showed that protoplasts, and non-turgid cells, exhibited a linear relationship between volume and the external osmotic pressure (i.e. they behaved as near-ideal osmometers), and that both protoplasts and cells have a component which is not osmotically responsive--the non-osmotic volume (NOV). Glycerol levels in whole cells and protoplasts were elevated by increased external osmotic pressure over a similar time-scale to the period of exponential cell growth, reaching a maximum value at 6-12 h and declining thereafter. This suggests that the restoration of turgor pressure in whole cells was not the sole regulator of glycerol accumulation. Stationary phase whole cells had negligible levels of intracellular glycerol after growth in a medium of raised osmotic pressure. However, intracellular trehalose synthesis in these cells began earlier and reached a higher maximum level than in basal medium. Once exponential growth had stopped, cell turgor and internal osmotic pressure decreased somewhat. These new, lower values may be determined by the extent of trehalose accumulation in stationary phase cells.     

Transient breakdown in the selective permeability of the plasma membrane ofChlorella emersonii in response to hyperosmotic shock: Implications for cell water relations and osmotic adjustment

Summary In osmotic experiments involving cells of the euryhaline unicellular green algaChlorella emersonii exposed to hyperosmotic stress by immersion in a range of low molecular weight organic and inorganic solutes, a temporary breakdown in the selective permeability of the plasma membrane was observed during the initial phase of transfer to media of high osmotic strength (up to 2000 mosmol kg^–1). Thus, although the cells appeared to obey the Boyle-van't Hoff relationship in all cases, showing approximately linear changes in volume (at high salinity) as a function of the reciprocal of the external osmotic pressure, the extent of change was least for the triitols, propylene glycol and glycerol, intermediate for glucose, sorbitol, NaCl and KCl, with greatest changes in media containing the disaccharides sucrose and maltose. In NaCl-treated cells, uptake of external solute and loss of internal ions was observed in response to hyperosmotic treatment while sucrose-treated cells showed no significant uptake of external solute, although loss of intracellular K⁺ was observed. These observations suggest that the widely used technique of estimating cellular turgor, and osmotic/nonosmotic volume by means of the changes in volume that occur upon transfer to media containing increasing amounts of either a low molecular weight organic solute or an inorganic salt may be subject to error. The assumption that all algal cells behave as ideal osmometers, with outer membranes that are permeable to water but not to solutes, during the course of such experiments is therefore incorrect, and the data need to be adjusted to take account of hyperosmotically induced external solute penetration and/or loss of intracellular osmotica before meaningful estimates of cell turgor and osmotic volume can be obtained.     

P and C-NMR Studies of the Phosphorus and Carbon Metabolites in the Halotolerant Alga, Dunaliella salina

The intracellular phosphorus and carbon metabolites in the halotolerant alga Dunaliella salina adapted to different salinities were monitored in living cells by ³¹P- and ¹³C-nuclear magnetic resonance (NMR) spectroscopy. The ¹³C-NMR studies showed that the composition of the visible intracellular carbon metabolites other than glycerol is not significantly affected by the salinity of the growth medium. The T₁ relaxation rates of the ¹³C-glycerol signals in intact cells were enhanced with increasing salinity of the growth medium, in parallel to the expected increase in the intracellular viscosity due to the increase in intracellular glycerol. The ³¹P-NMR studies showed that cells adapted to the various salinities contained inorganic phosphate, phosphomonoesters, high energy phosphate compounds, and long chain polyphosphates. In addition, cells grown in media containing up to 1 molar NaCl contained tripolyphosphates. The tripolyphosphate content was also controlled by the availability of inorganic phosphate during cell growth. Phosphate-depleted D. salina contained no detectable tripolyphosphate signal. Excess phosphate, however, did not result in the appearance of tripolyphosphate in ³¹P-NMR spectra of cells adapted to high (>1.5 molar NaCl) salinites.     

Loss of intracellular glycerol from Dunaliella by electroporation at constant osmotic pressure: subsequent restoration of glycerol content and associated volume changes

The effect of electroporation on Dunaliella tertiolecta at constant osmotic pressure (or water activity) was investigated. The following metabolic and physiological parameters were determined: extracellular and intracellular glycerol content, soluble protein content, photosynthetic oxygen evolution, mitochondrial oxygen uptake, cell volume and cell density. Electroporation conditions are described that released about 10% of intracellular glycerol to the external medium with minimal apparent effects on metabolism. Glycerol release originated from most cells rather than by total rupture of a small proportion of cells. Cell volume, measured on motile cells by video microscopy, reduced by 23% immediately after electroporation. Cell density did not increase. The uptake of mannitol, the major solute in the electroporation medium, was less than 20% of glycerol release. Following electroporation, the intracellular glycerol content and the cell volume both returned to pre-electroporation values after about 30min. Because the cells were maintained at constant external osmotic pressure throughout the procedure, it is concluded that the regulatory mechanism responsible for setting the intracellular glycerol content does not sense external osmotic pressure per se. These findings are consistent with a mechanism that senses a parameter linked directly to cell volume to set the intracellular glycerol content.     

Roles of N-acetylglutaminylglutamine amide and glycine betaine in adaptation of Pseudomonas aeruginosa to osmotic stress.

The mechanism of osmotic stress adaptation in Pseudomonas aeruginosa PAO1 was investigated. By using natural abundance 13C nuclear magnetic resonance spectroscopy, osmotically stressed cultures were found to accumulate glutamate, trehalose, and N-acetylglutaminylglutamine amide, an unusual dipeptide previously reported only in osmotically stressed Rhizobium meliloti and Pseudomonas fluorescens. The intracellular levels of these osmolytes were dependent on the chemical composition and the osmolality of the growth medium. It was also demonstrated that glycine betaine, a powerful osmotic stress protectant, participates in osmoregulation in this organism. When glycine betaine or its precursors, phosphorylcholine or choline, were added to the growth medium, growth rates of cultures in 0.7 M NaCl were increased more than threefold. Furthermore, enhancement of growth could be observed with as little as 10 microM glycine betaine or precursor added to the medium. Finally, the mechanism of osmotic stress adaptation of two clinical isolates of P. aeruginosa was found to be nearly identical to that of the laboratory strain PAO1 in all aspects studied.     

Determination of intracellular volume and internal solute concentrations of the green alga Chlorococcum submarinum

A method is described for measuring the cell volume of the unicellular green alga Chlorococcum submarinum, which depends on measurements of bromide concentration before and after disruption of the cells by ammonium hydroxide. Simultaneous equations are derived, which along with direct determination of cell water weight, allow the calculation of the intracellular volume in three different ways. The volumes calculated are in agreement indicating the validity of the method. The cell volumes and internal concentrations of glycerol, proline, potassium and sodium were determined for algae adapted to three salinities, 0.1, 0.5 and 1.0 M NaCl. The results showed that glycerol was the major internal solute and that the total measured solutes balanced the external osmotic pressure at all three salinities.Abbreviations DMSO dimethyl sulphoxide - Hepes N-[2-hydroxyethyl]piperazine-N-2-ethane sulfonic acid - TCA trichloroacetic acid - Tris tris[hydroxymethyl]aminoethane     

Osmotic adjustment in the filamentous fungus Aspergillus nidulans.

Aspergillus nidulans was shown to be xerotolerant, with optimal radial growth on basal medium amended with 0.5 M NaCl (osmotic potential [psi s] of medium, -3 MPa), 50% optimal growth on medium amended with 1.6 M NaCl (psi s of medium, -8.7 MPa), and little growth on medium amended with 3.4 M NaCl (psi s of medium, -21 MPa). The intracellular content of soluble carbohydrates and of selected cations was measured after growth on basal medium, on this medium osmotically amended with NaCl, KCl, glucose, or glycerol, and also after hyperosmotic and hypoosmotic transfer. The results implicate glycerol and erythritol as the major osmoregulatory solutes. They both accumulated during growth on osmotically amended media, as well as after hyperosmotic transfer, except on glycerol-amended media, in which erythritol did not accumulate. Furthermore, they both decreased in amount after hypoosmotic transfer. With the exception of glycerol, the extracellular osmotic solute did not accumulate intracellularly when mycelium was grown in osmotically amended media, but it accumulated after hyperosmotic transfer. It was concluded that the extracellular solute usually plays only a transient role in osmotic adaptation. The intracellular content of soluble carbohydrates and cations measured could reasonably account for the intracellular osmotic potential of mycelium growing on osmotically amended media.     

Adaptation of yeasts to salt stress (review)]

Mechanisms underlying adaptation of various yeasts to salt stress were summarized. Stress response involves modulation of enzymatic activities and changes in gene expression. Elevated salinity of the environment can be regarded as a two-factor stress process that includes an osmotic component leading to loss of cellular turgor and a toxic component inhibiting a set of functions due to an increase in the intracellular concentration of Na+. Adaptation of yeast cells to these stress conditions obligatorily involves the accumulation of osmotically active compounds (mainly glycerol) to counterbalance an increased external osmotic pressure and the modification of plasma membrane transport systems to extrude Na+ from the cell.     

The Role of Glycerol in the Osmotic Regulation of the Halophilic Alga Dunaliella parva

Dunaliella parva, a green halophilic alga, was found to accumulate very large amounts of intracellular glycerol. Through measurements of the intracellular volume the internal concentration of glycerol was calculated and found to be around 2.1 m in cells cultured in 1.5 m NaCl. When the extracellular salt concentration of an algal suspension was increased or decreased, the intracellular glycerol varied accordingly, reaching its new osmotic equilibrium after about 90 minutes. Since no leakage of intracellular glycerol was observed above 0.6 m NaCl, these alterations in glycerol content are interpreted as due to metabolic formation and degradation of intracellular glycerol. The above results indicate the existence of a new type of algal osmoregulation, in which the osmotic balance depends on the synthesis or degradation of intracellular glycerol in response to the external salt concentration.     

Osmotic adjustment in cyanobacteria from hypersaline environments

The intracellular concentrations of the monovalent inorganic cations K⁺ and Na⁺, low molecular weight carbohydrates and quaternary ammonium compounds have been determined for 4 strains of cyanobacteria (Aphanothece halophytica, Coccochloris elabens, Dactylococcopsis salina and Synechocystis DUN52) originally isolated from hypersaline habitats (i.e. habitats with a salinity greater than that of seawater) over a range of external salt concentration (from 50% to 400% seawater). Intracellular cation levels (Na⁺ and K⁺) were determined to be within the range 80–320 mmol · dm^-3 (cell volume), showing only minor changes in response to salinity. Intracellular carbohydrates were found to comprise a negligible component of the intracellular osmotic potential [at 2–19 mmol · dm^-3 (cell volume)], throughout the salinity range. Quaternary ammonium compounds, however, were recorded in osmotically significant quantities [up to 1,640 mmol · dm^-3 (cell volume)] in these strains, showing major variation in response to salinity. Thus Synechocystis DUN 52 showed an increase in quaternary ammonium compounds in the oder of 1,200 mmol · dm^-3 between 50% and 400% seawater medium, accounting for a significant proportion of the change in external osmotic potential.Examination of intact cells and cell extracts using ¹³C and ¹H nuclear magnetic resonance (NMR) spectroscopy confirmed the presence of the quaternary ammonium compound glycine betaine as the major osmoticum in the 4 strains; no other compounds were detected during NMR assays. These results suggest a common mechanism of osmotic adjustment, involving quaternary ammonium compounds, in cyanobacteria from hypersaline environments.     

Determinants of epithelial cell volume

Epithelial cell volume is determined by the concentration of intracellular, osmotically active solutes. The high water permeability of the cell membrane of most epithelia prevents the establishment of large osmotic gradients between the cell and the bathing solutions. Steady-state cell volume is determined by the relative rates of solute entry and exit across the cell membranes. Inhibition of solute exit leads to cell swelling because solute entry continues; inhibition of solute entry leads to cell shrinkage because solute exit continues. Cell volume is then a measure of the rate and direction of net solute movements. Epithelial cells are also capable of regulation of the rate of solute entry and exit to maintain intracellular composition. Feedback control of NaCl entry into Necturus gallbladder epithelial cells is demonstrable after inhibition of the Na,K-ATPase or reduction in the NaCl concentration of the serosal bath. Necturus gallbladder cells respond to a change in the osmolality of the perfusion solution by rapidly regulating their volume to control values. This regulatory behavior depends on the transient activation of quiescent transport systems. These transport systems are responsible for the rapid readjustments of cell volume that follow osmotic perturbation. These powerful transporters may also play a role in steady-state volume regulation as well as in the control of cell pH.     

Osmoregulation of the salt-tolerant yeast Debaryomyces hansenii grown in a chemostat at different salinities.

The intracellular solute composition of the salt-tolerant yeast Debaryomyces hansenii was studied in glucose-limited chemostat cultures at different concentrations of NaCl (4 mM, 0.68 M, and 1.35 M). A strong positive correlation between the total intracellular polyol concentration (glycerol and arabinitol) and medium salinity was demonstrated. The intracellular polyol concentration was sufficient to balance about 75% of the osmotic pressure of the medium in cultures with 0.68 and 1.35 M NaCl. The intracellular concentration of K+ and Na+, which at low external salinity gave a considerable contribution to the intracellular water potential, was only slightly enhanced with raised medium salinity. However, the ratio of intracellular K+ to Na+ decreased; but this decrease was less drastic in the cells than in the surrounding medium, i.e., the cells were able to select for K+ in favor of Na+. The turgor pressure, which was estimated on the basis of intracellular solute concentrations, was 2,200 kPa in cultures with 4 mM NaCl and decreased when the external salinity was raised, resulting in a value of about 500 kPa in cultures with 1.35 M NaCl. The maintenance of a positive turgor pressure at high salinity was mainly due to an increased production and accumulation of glycerol.     

Halotolerance of Methanobacterium thermoautotrophicum delta H and Marburg.

Methanobacterium thermoautotrophicum delta H and Marburg were adapted to grow in medium containing up to 0.65 M NaCl. From 0.01 to 0.5 M NaCl, there was a lag before cell growth which increased with increasing external NaCl. The effect of NaCl on methane production was not significant once the cells began to grow. Intracellular solutes were monitored by nuclear magnetic resonance (NMR) spectroscopy as a function of osmotic stress. In the delta H strain, the major intracellular small organic solutes, cyclic-2,3-diphosphoglycerate and glutamate, increased at most twofold between 0.01 and 0.4 M NaCl and decreased when the external NaCl was 0.5 M. M. thermoautotrophicum Marburg similarly showed a decrease in solute (cyclic-2,3-diphosphoglycerate, 1,3,4,6-tetracarboxyhexane, and L-alpha-glutamate) concentrations for cells grown in medium containing > 0.5 M NaCl. At 0.65 M NaCl, a new organic solute, which was visible in only trace amounts at the lower NaCl concentrations, became the dominant solute. Intracellular potassium in the delta H strain, detected by atomic absorption and 39K NMR, was roughly constant between 0.01 and 0.4 M and then decreased as the external NaCl increased further. The high intracellular K+ was balanced by the negative charges of the organic osmolytes. At the higher external salt concentrations, it is suggested that Na+ and possibly Cl- ions are internalized to provide osmotic balance. A striking difference of strain Marburg from strain delta H was that yeast extract facilitated growth in high-NaCl-containing medium. The yeast extract supplied only trace NMR-detectable solutes (e.g., betaine) but had a large effect on endogenous glutamate levels, which were significantly decreased. Exogenous choline and glycine, instead of yeast extract, also aided growth in NaCl-containing media. Both solutes were internalized with the choline converted to betaine; the contribution to osmotic balance of these species was 20 to 25% of the total small-molecule pool. These results indicate that M. thermoautotrophicum shows little changes in its internal solutes over a wide range of external NaCl. Furthermore, they illustrate the considerable differences in physiology in the delta H and Marburg strains of this organism.     

On the mechanism of salt tolerance. Production of glycerol and heat during growth of Debaryomyces hansenii.

As glycerol was suggested as an osmotic agent in the salt tolerant Debaryomyces hansenii the concentrations of total, intracellular, and extracellular glycerol produced by this yeast was followed during growth in 4 mM, 0.68 M, and 2.7 M NaCl media. The total amount of glycerol was not directly proportional to biomass production but to the cultural salinity with maximum concentrations just prior to or at the beginning of the stationary phase. In all cultures the cells lost some glycerol to the media, at 2.7 M NaCl the extracellular glycerol even amounted maximally to 80% of the total. A distinct maximum of intracellular glycerol, related to dry weight or cell number, appeared during the log phase at all NaCl concentrations. As the intracellular calculated glycerol concentrations amounted to 0.2 M, 0.8 M, and 2.6 M in late log phase cells at 4mM, 0.68 M, and 2.7 M NaCl, respectively, whereas the corresponding analysed values for the glycerol concentrations of the media were 0.7 mM, 2.5 mM, and 3.0 mM, glycerol contributes to the osmotic balance of the cells. During the course of growth all cultures showed a decreasing heat production related to cell substance produced, most pronounced at 2.7 M NaCl. At 2.7 M NaCl the total heat production amounted to--1690 kJ per mole glucose consumed in contrast to--1200 and--1130 kJ at 4 mM and 0.68 M NaCl, respectively. The Ym-values were of an inverse order, being 129, 120, and 93 at 4 mM, 0.68 M, and 2.7 M NaCl respectively.     

Effects of osmotic stress on Methanococcus thermolithotrophicus: 13C-edited 1H-NMR studies of osmolyte turnover

In vivo NMR studies of the thermophilic archaeon Methanococcus thermolithotrophicus, with sodium formate as the substrate for methanogenesis, were used to monitor formate utilization, methane production, and osmolyte pool synthesis and turnover under different conditions. The rate of formate conversion to CO2 and H2 decreased for cells adapted to higher external NaCl, consistent with the slower doubling times for cells adapted to high external NaCl. However, when cells grown at one NaCl concentration were resuspended at a different NaCl, formate utilization rates increased. Production of methane from 13C pools varied little with external NaCl in nonstressed culture, but showed larger changes when cells were osmotically shocked. In the absence of osmotic stress, all three solutes used for osmotic balance in these cells, l-alpha-glutamate, beta-glutamate, and Nepsilon-acetyl-beta-lysine, had 13C turnover rates that increased with external NaCl concentration. Upon hyperosmotic stress, there was a net synthesis of alpha-glutamate (over a 30-min time-scale) with smaller amounts of beta-glutamate and little if any of the zwitterion Nepsilon-acetyl-beta-lysine. This is a marked contrast to adapted growth in high NaCl where Nepsilon-acetyl-beta-lysine is the dominant osmolyte. Hypoosmotic shock selectively enhanced beta-glutamate and Nepsilon-acetyl-beta-lysine turnover. These results are discussed in terms of the osmoadaptation strategies of M. thermolithotrophicus.     

A METHOD FOR THE CRYOCONSERVATION OF DUNALIELLA SALINA (CHLOROPHYCEAE): EFFECT OF GLYCEROL AND COLD ADAPTATION1

The unicellular green alga Dunaliella salina Teod. was frozen according to the following procedure: 3 days cold adaptation at 4°C, addition of 3.5 M glycerol as a cryoprotectant, slow cooling to –40°C, immersion in liquid nitrogen, and rapid thawing. The survival rate was higher when cells were grown, before freezing, in the presence of 2 M NaCl instead of 1 M NaCl (78 and 48% survival, respectively). This difference is probably due to the intracellular amount of glycerol, which increases with external NaCl concentration and, therefore, may enhance cell protection. Although cells grown in 4 M NaCl accumulated a large amount of glycerol in response to osmotic stress, they did not withstand freezing. The use of cryoprotectant was absolutely necessary for the cells to recover from storage at –196°C. Glycerol was used because it is naturally produced by Dunaliella salina and therefore is not toxic. Provided it was added slowly to avoid osmotic shock, 3.5 M glycerol gave better results than 1M glycerol (48 and 18% survival, respectively). Cold adaptation in the dark increased postthaw viability. Cells grown in 1 M or 2 M NaCl had a survival rate of 48 and 78%, respectively, when cold-adapted, against 10 and 42% when not cold-adapted. This adaptation could be due to the synthesis, at low temperature, of specific proteins because two bands (28–29 kDa) appeared when electrophoretically separated proteins from cold-adapted cells and control cells were compared. Also, it could be due to the degradation of starch that occurs in the dark and leads to glycerol accumulation. Our procedure has never been used to cryopreserve microalgae and could enhance reported survival rates.     

THE GLYCEROL PERMEABILITY OF THE PLASMALEMMA OF THE HALOTOLERANT GREEN ALGA DUNALIELLA PARVA (VOLVOCALES)1

The glycerol permeability of the plasmalemma of the green alga Dunaliella parva Lerche was investigated by efflux studies with labelled glycerol, by enzymatic determination of glycerol leakage, and the determination of the reflection coefficient from osmotically induced volume changes (zero flow method). All results indicate that the plasmalemma of D. parva does not exhibit a special low permeability towards glycerol as would be expected from a glycerol accumulating alga. Rather, significant amounts of glycerol diffuse continuously into the medium following the glycerol concentration gradient between the cells and the medium. Efflux rates vary between 0.1 and 2 μmoles glycerol·mg^?1 chlorophyll·h^?1 depending on the external NaCl concentration. After one day up to 25% of the total glycerol of the algal suspension was found in the medium. Within 10 days this value can increase to 60%, depending on the growth constant of the culture. The reflection coefficient σ was determined to be 0.87, the permeability coefficient 2800 × 10^?11 m·sec^?1. To maintain a proper endogenous glycerol level corresponding to the external osmotic pressure, glycerol efflux in D. parva has to be balanced by a continuous synthesis of glycerol. D. parva follows the strategy of “glycerol efflux tolerance” instead of “glycerol efflux avoidance”. The alga has to pay the energetic costs of this strategy of tolerance.