Stress Responses of Bacillus Subtilis to High Osmolarity Environments: Uptake and Synthesis of Osmoprotectants

Stress Responses of Bacillus Subtilis to High Osmolarity Environments: Uptake and Synthesis of Osmoprotectants

Stress responses of Bacillus subtilis to high osmolarity environments: Uptake and synthesis of osmoprotectants BETTINA KEMPF and ERHARD BREMER* Department of Biology, Laboratory for Microbiology, Philipps University Marburg, Kart-von-Frisch Str, D-35032 Marburg, Germany *Corresponding author (Fax, 49-6421-288979; Email, [email protected]). A decrease in the water content of the soil imposes a considerable stress on the soil-living bacterium Bacillus subtifis: water exits from the cetts, resulting in decreased turgor and cessation of growth. Under these adverse circumstances, B. subtilis actively modulates the osmolarity of its cytoplasm to maintain turgor within acceptable boundaries. A rapid uptake of potassium ions via turgor-responsive transport systems is the primary stress response to a sudden increase in the external osmolarity. This is followed by the massive accumulation of the so-called compatible solutes, i.e., organic osmolytes that are highly congruous with cellular functions and hence can be accumulated by bacterial cells up to molar concentrations. Initially, the compatible solute proline is accumulated via de novo synthesis, but B. subtilis can also acquire proline from the environment by an osmoregulated transport system, OpuE. The preferred compatible solute of B. subtitis is the potent osmoprotectant gIycine betaine. This trimethylammonium compound can be taken up by the ceil through three high-affinity transport systems: the multicomponent ABC transporters OpuA and OpuC, and the single-component transporter OpuD. The OpuC systems also mediates the accumulation of a variety of naturally occurring betaines, each of which can confer a considerable degree of osmotic tolerance. In addition to the uptake of glycine betaine from the environment, B. subtilis can also synthesize this osmoprotectant but it requires exogenously provided choline as its precursor. Two evolutionarily closely related ABC transport systems, OpuB and OpuC, mediate the uptake of choline which is then converted by the GbsA and GbsB enzymes in a two-step oxidation process into glycine betaine. Our data show that the intracellular accumulation of osmoprotectants is of central importance for the cellular defence of B. subtitis against high osmolarity stress. 1. Introduction envelope of microorganisms is permeable to water, fluc- tuations in the environmental osmoIarity trigger the flux The osmotic strength of the environment is an important of water across the cytoplasmic membrane along the physical parameter that influences the ability of micro- osmotic gradient. To avoid lysis under low-osmolarity organisms to proliferate and successfully compete for a or dehydration under high-osmolarity growth conditions, given habitat. Bacteria maintain an osmotic pressure in bacteria must possess active mechanisms to efficiently the cytoplasm that is higher than that in the surrounding adjust the osmolarity of their cytoplasm. environment, resulting in an outward directed tension, AnaIyses of the cellular responses of bacteria to osmotic the turgot (figure 1). In Gram-negative bacteria, turgor stress have been focused primarily on high-osmolarity has been estimated at 0.3-0.5MPa (Csonka 1989), environments (Csonka 1989; Csonka and Hanson 1991; whereas Gram-positive bacteria, such as Bacillus subtilis, Galinski and Trtiper 1994; Lucht and Bremer 1994; maintain a much higher turgot, estimated at approximately Csonka and Epstein I996; Miller and Wood 1996). Two 1.9MPa (Whatmore and Reed 1990). Since the cell basic schemes of adaptation to these environments have Keywords. Stress responses; osmoprotection; compatible solutes; osmoregulation; transporters J. Biosci., 23, No. 4, October 1998, pp 447--455. Indian Academy of Sciences 447 448 Bettina Kempf and Erhard BPemer glycosylglycerot), quaternary amines and their sulphonium analogues (e.g., glycine betaine, proline betaine, dimethyl- sulphoniopropionate), sulphate esters (e.g., choline-O- sulphate), N-acetylated diamino acids (e.g., N6-acetyl- H2o ornithine, Ne-acetyllysine), and small peptides (e.g., N-acetylglutaminylglutamine amide) (Csonka 1989; Galinski and Trfiper 1994). In general, compatible solutes are highly Soluble molecules and do not carry a net charge at physiologicat pH. In contrast to inorganic salts, they can reach high intracellular concentrations without disturbing vital functions such as DNA-replication, DNA- protein interactions, and cellulhr metabolism. high Compatible solutes serve a cluaI function in osmo- H20 = osmolarity regulating cel[s. Because they can accumulate up to molar concentrations, they make a major contribution to the osmotic balance of the cytoplasm (Galinski and Trtiper 1994; Miller and Wood 1996). They also serve as stabilizers of enzymes and cell components against 11 the denaturing effects of high ionic strength and hence can be described as chemical chaperones. This protective t property of compatible solutes appears to stem from their preferential exclusion from the hydration shell of H20 " " Turgor--~ Adaptation macromolecules (Potts 1994; Yancey 1994). In this over- 9 9 9 +.,, view, we focus on the physiological and molecular stress responses of B. subtilis to high osmolarity environments i and report on the characteristics of the systems for the Figure 1. Initial adaptation of B. st+btitis to high osmolarity. synthesis and uptake of osmoprotectants and compatible solutes in this soil bacterium. been identified: (i) The accumulation of very high 3. B+ subtilis as a model system for studies on intracelluIar concentrations of ions. This s:rategy is osmoregtflafion followed by many halophiIic and halotolerant micro- B. svbtitis frequently occupies the upper layers of the organisms whose entire physiology has been adapted to soil, where desiccation often causes high salinity and a permanent life in a high-saline environment. (it) The intracellular accumulation of compatible solutes, i.e., high osmolarity (Miller and Wood 1996; Potts 1994). organic osmolytes that are highly congruous with the To survive and grow in this ecological niche, B. subti/is must be able to adapt to high osmolarity stress. It structure and function of the ceil. This approach is of exhibits a behavioural response to brief increases in general importance; not only is it widely employed in osmolarity, whereby it swims away from the area of the prokaryotic world by (bacteria and archaea), but it high osmolarity (Wong et al 1995). It aIso responds is also used as a stress reaction in yeast, plant, animal, genetically with the induction of a large general stress and even human cells (Rhodes and Hanson i993; Biota- regulon (Antetmann et al 1997; Hocker et al 1996). The berg 1997; Burg et al 1997). members of this stress regulon are induced not only by salt but also by a number of growth-limiting conditions 2. Characteristics of compatible solutes and stationary phase signals; these stress proteins provide Osmoprotectants are defined as exogenous organic solutes cross-protection for a variety of environmental challenges that enhance bacterial growth in media of high osmolarity. and are thought to prepare non-growing ceils for a These substances may themselves be compatible solutes diverse range of stress conditions (Hocker et al 1996). or they may be precursor molecules that can be enzy- Expression of many members of the general stress regulon mafically converted to these compounds (Galinski and is under the control of the alternative transcription factor Traper t994; Miller and Wood 1996). The spectrum of sigma B (oz), whose activity is determined by a complex compatible solutes used by microorganisms comprise a network of regulatory proteins (Hocker et al t996; Yang limited number of compounds: amino acids and amino et at 1996). Although the addition of salt transiently acid derivatives (e.g., proline, glutamate, fl-alanine, triggers the enhanced transcription of many genes of the ectoine), sugars and polyols (e.g., trehalose, glycerol, a B regulon, sigB mutants are not at a survival disadvantage Osmoregulation in B. subtilis 449 compared with the wild type when exposed to osmotic transport systems, hut the molecular details of these shock or extreme desiccation under laboratory conditions transporters have not yet been elucidated. The influx of (Boylan et al 1993). Hence, o~ is elearIy not the master K § is essential for the recovery of turgor after upshock regulator for the osmostress response in proliferating (figure 1) and the subsequent resumption of growth B. subtilis cells. Under high osmolarity growth condi- (Whatmore et al 1990). Hence K § serves a crucial role tions, B. subtilis incites specific and highly co-ordinated in the initial cellular stress response of B. subtilis to genetic and physiological adaptation reactions to limit sudden increases in the environmental osmolarity. the loss of water from the cell and thus maintain turgot at a level suitable for growth (figure 1). At the core of this stress response is the intracellular accumulation of 4.2 Synthesis of the compatible solute proline osmoprotectants and compatible solutes (figure 2) through synthesis and uptake from the environment. Because high intracellular concentrations of K § are dele- terious for the bacterial cell, the massive accumulation of K* is an inadequate strategy for coping with proionged 4, The initial stress response to high osmolarity high osmolarity. In E. coli and S. typhimurium (Csonka and Epstein I996), the initial rapid accumulation of K § 4.1 Uptake of K + is followed by a long-term

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