Uptake of the fluorescent indicator atebrin into acidic vacuoles in the halotolerant alga Dunaliella satina

The fluorescent indicator atebrin (3-chloro-9-(4-diethylamino-1-methylbutyl)-7-methyoxy-acridine) is taken up by Dunaliella salina cells at alkaline external pH and accumulates in acidic vacuoles. The uptake is unaffected by light, by photosynthetic inhibitors, by protonophores or by ionophores; however, the dye can be released by amines, indicating that it is specifically accumulating in acidic vacuoles. Amines induce a biphasic enhancement of atebrin fluorescence — a fast phase, accompanied by redistribution within the cell, consistent with release of the dye from the vacuoles to the cytoplasm, and a slow phase, correlated with release of atebrin from the cells. These results are interpreted to indicate a slow equilibration of atebrin across the plasma membrane and a fast equilibration across the vacuolar membrane. Part of the dye cannot be released by the amines, and appears to be internally bound. Atebrin uptake is inhibited by cholesteryl hemisuccinate and is stimulated by lysophosphatidylcholine, indicating that modification of the lipid composition of the plasma membrane affects the permeability to atebrin. Analysis of the pH dependence of atebrin uptake indicates that the dye enters the cells by fluid-phase permeation. Different stresses enhance the rate of atebrin uptake and release, indicating that they modify plasma-membrane structure or composition. Atebrin may serve as a specific marker for acidic vacuoles, as an indicator for amine uptake, and as a probe for subtle changes in the permeability of the plasma membrane.Abbreviations Atebrin 3-chloro-9-(4-diethylamino-1-methylbutyl)-7-methoxy-acridine - DCMU 3-(3,4-dichlorophenyl)-1,1-dimethyl-urea - SF-6847 3,5-ditertbutyl-4-hydroxybenzylidenemalonitrile     

Amine Accumulation in Acidic Vacuoles Protects the Halotolerant Alga Dunaliella salina Against Alkaline Stress

Amines at alkaline pH induce in cells of the halotolerant alga Dunaliella a transient stress that is manifested by a drop in ATP and an increase of cytoplasmic pH. As much as 300 millimolar NH₄⁺ are taken up by the cells at pH 9. The uptake is not associated with gross changes in volume and is accompanied by K⁺ efflux. Most of the amine is not metabolized, and can be released by external acidification. Recovery of the cells from the amine-induced stress occurs within 30 to 60 minutes and is accompanied by massive swelling of vacuoles and by release of the fluorescent dye atebrin from these vacuoles, suggesting that amines are compartmentalized into acidic vacuoles. The time course of ammonia uptake into Dunaliella cells is biphasic—a rapid influx, associated with cytoplasmic alkalinization, followed by a temperature-dependent slow uptake phase, which is correlated with recovery of cellular ATP and cytoplasmic pH. The dependence of amine uptake on external pH indicates that it diffuses into the cells in the free amine form. Studies with lysed cell preparations, in which vacuoles become exposed but retain their capacity to accumulate amines, indicate that the permeability of the vacuolar membrane to amines is much higher than that of the plasma membrane. The results can be retionalized by assuming that the initial amine accumulation, which leads to rapid vacuolar alkalinization, activates metabolic reactions that further increase the capacity of the vacuoles to sequester most of the amine from the cytoplasm. The results indicate that acidic vacuoles in Dunaliella serve as a high-capacity buffering system for amines, and as a safeguard against cytoplasmic alkalinization and uncoupling of photosynthesis.     

Polyphosphate Hydrolysis within Acidic Vacuoles in Response to Amine-Induced Alkaline Stress in the Halotolerant Alga Dunaliella salina

The location and mobilization of polyphosphates in response to an amine-induced alkaline stress were studied in the halotolerant alga Dunaliella salina. The following observations suggest that polyphosphates accumulate in acidic vacuoles: (a) Accumulation of large amounts of polyphosphates is manifested as intravacuolar dense osmiophilic bodies in electron micrographs. (b) Uptake of amines into the vacuoles induces massive hydrolysis of polyphosphates, demonstrated by in vivo ³¹P-nuclear magnetic resonance, and by analysis of hydrolytic products on thin layer chromatograms. The analysis indicates that: (a) Polyphosphate hydrolysis is kinetically correlated with amine accumulation and with the recovery of cytoplasmic pH. (b) The major hydrolytic product is tripolyphosphate. (c) The peak position of the tripolyphosphate terminal phosphate in nuclear magnetic resonance spectra is progressively shifted as the cells recover, indicating that the pH inside the vacuoles increases while the pH in the cytoplasm decreases. (d) In lysed cell preparations, in which vacuoles become exposed to the external pH, mild alkalinization in the absence of amines induces polyphosphate hydrolysis to tripolyphosphates. It is suggested that amine accumulation within vacuoles activates a specific phosphatase, which hydrolyzes long-chain polyphosphates to tripolyphosphates. The hydrolysis increases the capacity of the vacuoles to sequester amines from the cytoplasm probably by releasing protons required to buffer the amine, and leads to recovery of cytoplasmic pH. Thus, polyphosphate hydrolysis provides a high-capacity buffering system that sustains amine compartmentation into vacuoles and protects cytoplasmic pH.     

Regulation of glycerol synthesis in response to osmotic changes in dunaliella

Changes in phosphometabolites, following osmotic shock, were analyzed by two-dimensional thin layer chromatography, in extracts of the halotolerant alga Dunaliella salina in order to clarify the regulation of glycerol synthesis from starch. The experiments were carried out in wild-type and in osmotically defective mutant cells. It is demonstrated that hyperosmotic shock induces a decrease in fructose 6-phosphate and an increase in fructose-1,6-bisphosphate indicating the activation of phosphofructokinase. Two mutants, which are specifically defective in their response to hyperosmotic shock, accumulate glucose 6-phosphate or phosphogluconate following shock, and have remarkably reduced activities of glucose-6-phosphate dehydrogenase and of phosphogluconate dehydrogenase, respectively. These results indicate that the pentose-phosphate oxidative pathway has a major role in glycerol synthesis. Hyperosmotic shock leads to a transient accumulation of phosphorylcholine and to a decrease of inositolbisphosphate in D. salina extracts. Accumulation of phosphorylcholine is not detected in osmotically defective mutants. Hypoosmotic shock induces an increase in inositolbisphosphate but not in phosphorylcholine. These results are consistent with previous indications for differential activations of phospholipases by hyper or hypoosmotic shock in Dunaliella. Based on these results we suggest that (a) phosphofructokinase is an important checkpoint enzyme in the regulation of glycerol production, and (b) that the pentose-phosphate pathway has a major role in keeping oxidation-reduction balance during glycerol synthesis. The possible role of lipid breakdown products as second messengers in regulating glycerol production in Dunaliella is discussed.     

A SALT-INDUCED CHLOROPLAST PROTEIN IN DUNALIELLA SALINA (CHLOROPHYTA)1

The unicellular green alga Dunaliella salina Teod, is halophilic and wall-less. The cell acclimates to osmotic stresses by accumulation or degradation of glycerol. To investigate other mechanisms involved in its physiological recovery following hyperosmotic shocks, protein profiles from cells grown in various salinities were compared. A 13-kDa protein (P13) accumulated when cells were subjected to drastic hyperosmotic shock. Front our results with antibiotic-treated cells and purified chloroplasts, we believe that this component results from de novo translation in chloroplasts. The solubility of P13 was strongly promoted by Triton X-100. Its accumulation was correlated with the recovery of photosynthesis.     

MEMBRANE CHARACTERISTICS AND OSMOTIC BEHAVIOR OF ISOLATED ROD OUTER SEGMENTS

Freshly isolated frog rod outer segments are sensitive osmometers which retain their photosensitivity; their osmotic behavior reveals essentially the same light-sensitive Na⁺ influx observed electrophysiologically in the intact receptor cell. Using appropriate osmotic conditions we have examined freeze-etch replicas of freshly isolated outer segments to identify the membrane which regulates the flow of water and ions. Under isosmotic conditions we find that the disc to disc repeat distance is almost exactly twice the thickness of a disc. This ratio appears to be the same in a variety of vertebrate rod outer segments and can be reliably measured in freeze-etch images. Under all our osmotic conditions the discs appear nearly collapsed. However, when the length of the outer segment is reduced by hyperosmotic shocks the discs move closer together. This markedly reduces the ratio of repeat distance to disc thickness since disc thickness remains essentially constant. Thus, the length reduction of isolated outer segments after hyperosmotic shocks primarily results from reduction of the extradisc volume. Since the discs are free floating and since they undergo negligibly small changes in volume, the plasma membrane alone must be primarily responsible for regulating the water flux and the light-sensitive Na⁺ influx in freshly isolated outer segments. On this basis we calculate, from the osmotic behavior, that the plasma membrane of frog rod outer segment has a Na⁺ permeability constant of about 2.8 x 10^-6 cm/s and an osmotic permeability coefficient of greater than 2 x 10^-3 cm/s.     

Selection and Characterization of Dunaliella salina Mutants Defective in Haloadaptation

A technique for selection of Dunaliella mutants defective in their capacity to recover from osmotic shocks has been developed. The selection is based on physical separation of mutants on density gradients. This technique takes advantage of the fact that Dunaliella cells, when exposed to osmotic shocks, initially change volume and density due to water gain or loss and subsequently recover their volume and density by readjusting their intracellular glycerol. Eight mutants that do not recover their original density following hyperosmotic shocks have been isolated. The mutants grow similar to wild type cells in 1 molar NaCl, and recover like the wild type from hypotonic shocks but are defective in recovering from hypertonic shocks. A partial characterization of one of the mutants is described.     

Hyperosmotic Stress Reduces Melanin Production by Altering Melanosome Formation

Many tissues of the human body encounter hyperosmotic stress. The effect of extracellular osmotic changes on melanin production has not yet been elucidated. In this study, we determined that hyperosmotic stress induced by organic osmolytes results in reduced melanin production in human melanoma MNT-1 cells. Under hyperosmotic stress, few pigmented mature melanosomes were detected, but there was an increase in swollen vacuoles. These vacuoles were stained with an anti-M6PR antibody that recognizes late endosomal components and with anti-TA99 and anti-HMB45 antibodies, implying that melanosome formation was affected by hyperosmotic stress. Electron microscopic analysis revealed that the M6PR-positive swollen vacuoles were multi-layered and contained melanized granules, and they produced melanin when L-DOPA was applied, indicating that these vacuoles were still capable of producing melanin, but the inner conditions were not compatible with melanin production. The vacuolation phenomenon induced by hyperosmotic conditions disappeared with treatment with the PI3K activator 740 Y-P, indicating that the PI3K pathway is affected by hyperosmotic conditions and is responsible for the proper formation and maturation of melanosomes. The microarray analysis showed alterations of the vesicle organization and transport under hyperosmotic stress. Our findings suggest that melanogenesis could be regulated by physiological conditions, such as osmotic pressure.     

Membrane fluidity of halophilic ectoine-secreting bacteria related to osmotic and thermal treatment

In response to sudden decrease in osmotic pressure, halophilic microorganisms secrete their accumulated osmolytes. This specific stress response, combined with physiochemical responses to the altered environment, influence the membrane properties and integrity of cells, with consequent effects on growth and yields in bioprocesses, such as bacterial milking. The aim of this study was to investigate changes in membrane fluidity and integrity induced by environmental stress in ectoine-secreting organisms. The halophilic ectoine-producing strains Alkalibacillus haloalkaliphilus and Chromohalobacter salexigens were treated hypo- and hyper-osmotically at several temperatures. The steady-state anisotropy of fluorescently labeled cells was measured, and membrane integrity assessed by flow cytometry and ectoine distribution. Strong osmotic downshocks slightly increased the fluidity of the bacterial membranes. As the temperature increased, the increasing membrane fluidity encouraged more ectoine release under the same osmotic shock conditions. On the other hand, combined shock treatments increased the number of disintegrated cells. From the ectoine release and membrane integrity measurements under coupled thermal and osmotic shock conditions, we could optimize the secretion conditions for both bacteria.     

Osmotic responses of unicellular blue-green algae (cyanobacteria): changes in cell volume and intracellular solute levels in response to hyperosmotic treatment

Abstract Changes in cell volume and solute content upon hyperosmotic shock have been studied for six unicellular blue-green algae (cyanobacteria): Synechococcus PCC 6301, PCC 6311; Synechocystis PCC 6702, PCC 6714, PCC 6803 and PCC 7008. The extent of change in volume was shown to be dependent upon the solute used to establish the osmotic gradient, with cells in NaCl showing a reduced shrinkage when compared to cells in media containing added sorbitol and sucrose. Uptake of extracellular solutes during hyperosmotic shock was observed in Synechocystis PCC 6714, with maximum accumulation of external solutes in NaCl and minimum solute uptake in sucrose solutions. Conversely, solute loss from the cells (K⁺ and amino acids) was greatest in sucrose-containing media and least in NaCl. The results show that these blue-green algae do not behave as ‘ideal osmometers’ in media of high osmotic strength. It is proposed that short-term changes in plasmalemma permeability in these organisms may be due to transient membrane instability resulting from osmotic imbalance between the cell and its surrounding fluid at the onset of hyperosmotic shock.     

A 150 Kilodalton Cell Surface Protein Is Induced by Salt in the Halotolerant Green Alga Dunaliella salina

Dunaliella salina is an extremely halotolerant, unicellular, green alga lacking a rigid cell wall. Osmotic adaptation to high salinities is based on the accumulation of glycerol. To uncover other functions responsible for halotolerance, protein profiles of algae continuously grown in different salinities were compared. A 150 kilodalton protein (p 150) increased in amount with salt concentration. Furthermore, when the cells were subjected to drastic hyperosmotic shocks, p150 started to rise long after completion of the osmotic response but coincident with reinitiation of cell proliferation. Cells with an initially higher level of p150 resumed growth faster than cells with a lower level of the protein. Addition of cycloheximide early after hyperosmotic shock prevented the rise in p150, indicating this rise was due to de novo synthesis of the protein. These observations suggest that p150 is a saltinduced protein required for proliferation of the cells in saline media. p150 was purified to homogeneity and found to be a detergent-soluble glycoprotein. Polyclonal antibodies against p150 recognized a single protein component in D. salina crude extracts. A high M_r cross-reacting protein was also observed in another Dunaliella strain, D. bardawil. Immunoelectron microscopy localized p150 to the cell surface.     

Growth,cell volume,and fine structure of Porphyra umbilicalis in relation to osmotic tolerance

Porphyra umbilicalis, a marine red alga occurring in the intertidal zone of the cold North Sea, tolerates a wide range of osmotic conditions from 0.2 x to 6 x artificial seawater medium ASP₁₂. In cells osmotically adapted for two weeks, photosynthesis and respiration are progressively inhibited in media more concentrated than 2 x. In both hypo- and hyperosmotic stress ranges, the most striking fine structural change is the development of vacuoles. In comparison to 1 x medium, where vacuoles are virtually lacking, the vacuolar part of the protoplasm increases 6-fold in 0.2 x and 10-fold in 3.5 x medium, respectively. However, at extreme hyperosmotic stress (6 x medium) the vacuolar part is extremely small. The largest cell volumes are found in 0.2 x and 3.5 x media, the smallest one in 6 x medium. In the osmotically regulated range (0.2–3.5 x medium), the regulated parameter is the volume of the protoplasm without the vacuolar system. It is suggested that at hyperosmotic stress the vacuoles may serve as osmotically active compartment, probably by accumulation of inorganic ions. The intracellular content of Floridean starch granules decreases with increasing osmotic pressure, possibly indicating the significance of soluble organic constituents as osmotically active solutes.Member of the Arbeitsgemeinschaft für Elektronenmikroskople un der Ticrärztlichen Hochschule Hannover     

Isolation and characterization of polyphosphates from the yeast cell surface

When cells of Saccharomyces fragilis are subjected to osmotic shock, they release a limited amount of inorganic polyphosphate into the medium, which represents about 10% of the total cellular content. The osmotic shock procedure causes no substantial membrane damage, as judged from the unimpaired cell viability, limited K⁺ leakage and low percentage of stained cells. It is therefore suggested that this polyphosphate fraction is localized outside the plasma membrane. The released polyphosphate fraction differs from the remaining cellular polyphosphates in two respects: the mean chain length of the shock-sensitive fraction is significantly higher than that of the total cellular polyphosphates and its metabolic turnover rate, subsequent to pulsing with [³²P]orthophosphate is much lower compared to the rest of the cellular polyphosphate. Incubation of intact cells with the anion exchange resin Dowex AG 1-X4 results in the release of high molecular weight polyphosphates. These results suggest that the osmotic shock-sensitive polyphosphate fraction has specific characteristics in both its cellular localization and metabolism.     

[14C]Carbon-dioxide fixation by isolated leaf epidermes with stomata closed or open

Following small hypo-osmotic shocks, ion concentrations (Na⁺, K⁺, Cl^-) in Platymonas subcordiformis decreased; this was due mainly to an increase of cell volume. With larger hypo-osmotic stresses, the decrease of ion concentration continued and, additionally, extrusion of mannitol was observed. The ion and mannitol concentrations were not regained after 240 min. In contrast, following hyperosmotic shocks, the ion concentrations increased transitorily during the first 20–40 min. The same was true for K⁺ following small hyperosmotic stresses and for Na⁺ and — partially — Cl^- with larger shocks. Large hyperosmotic stresses caused permanent accumulation of mannitol, which levelled off after 60–80 min. Thus the transient increase of ions bridged the concentration gap until mannitol was accumulated to a high enough concentration to account for the osmotic adaptation of Platymonas, together with a basal level of the ions K⁺, Na⁺, Cl^-.Abbreviations PS photosynthesis - Resp respiration     

The Contractile Vacuole as a Key Regulator of Cellular Water Flow in Chlamydomonas reinhardtii

Most freshwater flagellates use contractile vacuoles (CVs) to expel excess water. We have used Chlamydomonas reinhardtii as a green model system to investigate CV function during adaptation to osmotic changes in culture medium. We show that the contractile vacuole in Chlamydomonas is regulated in two different ways. The size of the contractile vacuoles increases during cell growth, with the contraction interval strongly depending on the osmotic strength of the medium. In contrast, there are only small fluctuations in cytosolic osmolarity and plasma membrane permeability. Modeling of the CV membrane permeability indicates that only a small osmotic gradient is necessary for water flux into the CV, which most likely is facilitated by the aquaporin major intrinsic protein 1 (MIP1). We show that MIP1 is localized to the contractile vacuole, and that the expression rate and protein level of MIP1 exhibit only minor fluctuations under different osmotic conditions. In contrast, SEC6, a protein of the exocyst complex that is required for the water expulsion step, and a dynamin-like protein are upregulated under strong hypotonic conditions. The overexpression of a CreMIP1-GFP construct did not change the physiology of the CV. The functional implications of these results are discussed.     

Carbohydrate metabolism during osmoregulation in Chasmagnathus granulata dana, 1851 (crustacea,decapoda)

• 1.1. Since glucose is one of the main energetic substrates for general metabolic processes in crustaceans, analysis of carbohydrate levels can furnish information on the energy metabolism of intact animals during osmoregulation.
• 2.2. Different groups of Chasmagnathus granulata were transferred to different salinities (0 and 40%), and the glucose and glycogen concentrations in blood, gills, muscle and hepatopancreas were determined at the beginning of the experiment and 24, 72, 168 and 360 hr after the salinity changes.
• 3.3. Differences in tissues carbohydrate levels were observed between summer and winter, that reflected differences in reserve mobilization.
• 4.4. In the summer, hypo- and hyperosmotic shocks induced an increase in carbohydrate levels in almost all tissues studied, indicating gluconeogenesis.
• 5.5. In the winter, a carbohydrate mobilization occurred only in the gills and hepatopancreas after both osmotic shocks.
• 6.6. Thus, the substrate reserve used for energy production required for osmoregulation seems to be dependent on the season and tissues.

     

Neutral lipid production in <Emphasis Type="Italic">Dunaliella salina</Emphasis> during osmotic stress and adaptation

The salt-tolerant green microalga Dunaliella salina can survive both hyper- and hypo-osmotic shock. Upon osmotic shock, the cells transiently and rapidly decreased or increased in size within minutes and slowly over hours acquired their original cell size and volume. Cell size distribution differs significantly in the cultures grown in the salinity range from 1.5 to 15 % NaCl. By using Nile Red fluorescence to detect neutral lipids, it became clear that only hyper-osmotic shock on cells induced transient neutral lipid appearance in D. salina, while those transferred from 9 to 15 % NaCl stimulated the most neutral lipid accumulation. These cells grew well in 9 % NaCl, but they cannot recover a shift to 15 % NaCl and cell division is accordingly slowed down. The transient appearance of neutral lipid could be dependent on the inhibition of cell division experiencing the NaCl shift. Moreover, the effect of nutrient limitation slows down cell division and photosynthesis as a secondary result, which triggers the cells to accumulate neutral storage lipids when they entered the stationary phase, which is seen in all the batch cultures of D. salina grown in the salinity range of 3–15 %. The changes in salt concentration did not significantly influence the overall fatty acid composition in D. salina cells. Although there shows both increased amounts of total lipids and neutral lipids in the cells grown in salinity higher than 9 % NaCl, lipid productivity is however compromised by the slower cell growth rate and lower cell density under this condition.     

Physiological response of the unicellular green alga Chlorococcum submarinum to rapid changes in salinity

Cell volumes and intracellular concentrations of major solutes of Chlorococcum submarinum were determined before and after salinity shocks. Cells were found to shrink in size by about 30% following changes from 0.1 to 0.5 M NaCl, there was a transitory increase in sodium concentration and more permanent increases in concentrations of potassium, proline and glycerol (the major osmolyte). Conversely, cells doubled in size after the reciprocal downshock, there was rapid loss of about 70% of the cells' glycerol to the medium, a much smaller loss of cellular potassium and a steady disappearance of proline from the cells. The respiratory and photosynthetic responses to salinity fluctuations were also studied. Salinity downshocks stimulated respiration by 30% and inhibited photosynthesis by 16% within 5 min, but within 2 h these rates were identical to control rates. Upshocks caused a slight inhibition of respiration, but decreased photosynthesis by 40% within 5 min and recovery took 2 h. Downshocks had little effect on chlorophyll fluorescence, however, Fo strongly increased and both Fm and Fv/Fm declined within 5 min of salinity increases. This is consistent with a decrease in efficiency of PS2. Ecological and metabolic implications of the results are discussed.Abbreviations DMSO dimethyl sulphoxide - Hepes N-[2-hydroxyethyl]piperazine-N-2-ethane sulphonic acid - TCA trichloroacetic acid - Tris tris[hydroxymethyl]aminoethane