Initiation of Bacillus spore germination by hydrostatic pressure: effect of temperature.

Suspensions of Bacillus cereus T, B. subtilis, and B. pumilus spores in water or potassium phosphate buffer were germinated by hydrostatic pressures of between 325 and 975 atm. Kinetics of germination at temperatures within the range of 25 to 44 degrees C were determined, and thermodynamic parameters were calculated. The optimum temperature for germination was dependent on pressure, species, suspending medium, and storage time after heat activation. Germination rates increased significantly with small increments of pressure, as indicated by high negative deltaV values of -230 +/- 5 cm3/mol for buffered B. subtilis (500 to 700 atm) and B. pumilus (500 atm) spores and -254 +/- 18 cm3/mol for aqueous B. subtilis (400 to 550 atm) spores at 40 degrees C and -612 +/- 41 cm3/mol for B. cereus (500 to 700 atm) spores at 25 degrees C. The ranges of thermodynamic constants calculated at 40 degrees C for buffered B. pumilus and B. subtilis spores at 500 and 600 atm and for aqueous B. subtilis spores at 500 atm were: Ea = 181,000 to 267,000 J/mol; deltaH = 178,000 to 264,000 J/mol; deltaG = 94,000 to 98,300 J/mol; deltaS = 264 to 544 J/mol per degree K. These values are consistent with the concept that the transformation of a dormant to a germinating spore induced by hydrostatic pressure involves either hydration or a reduction in the visocosity of the spore core and a conformational change of an enzyme.     

Heat Activation of Phycomyces blakesleeanus Spores: Thermodynamics and Effect of Alcohols, Furfural, and High Pressure

The thermodynamic parameters for the heat activation of the sporangiospores of Phycomyces blakesleeanus were determined. For the apparent activation enthalpy (DeltaH(#)) a value of 1,151 kJ/mol was found, whereas a value of 3,644 J./ degrees K.mol was calculated for the apparent activation entropy (DeltaS(#)). n-Alcohols (from methanol to octanol), phenethyl alcohol, and furfural lowered the activation temperature of P. blakesleeanus spores. The heat resistance of the spores was lowered concomitantly. The effect of the alcohols was a linear function of the concentration in the range that could be applied. When the log of the concentration needed to produce an equal shift of the activation temperature was plotted for each alochol against the log of the octanol/water partition coefficient, a straight line was obtained. The free energy of adsorption of the n-alcohols to their active sites was calculated to be -2,487 J/mol of CH(2) groups. Although still inconclusive, this points toward an involvement of protein in the activation process. The effect of phenethyl alcohol was similar to the effect of n-alcohols, but furfural produced a greater shift than would be expected from the value of its partition coefficient. When the heat activation of the spores was performed under high pressure, the activation temperature was raised by 2 to 4 degrees K/1,000 atm. However, with pressures higher than 1,000 atm (1.013 x 10(5) kPa) the activation temperature was lowered until the pressure became lethal (more than 2,500 atm). It is known that membrane phase transition temperatures are shifted upward by about 20 degrees K/1,000 atm and that protein conformational changes are shifted upward by 2 to 6 degrees K/1,000 atm. Consequently, heat activation of fungal spores seems to be triggered by a protein conformational change and not by a membrane phase transition. Activation volumes of -54.1 cm(3)/mol at 38 degrees C and -79.3 cm(2)/mol at 40 degrees C were found for the lowering effect of high pressure on the heat activation temperature.     

Rupture of the cell envelope by induced intracellular gas phase expansion in gas vacuolate bacteria.

Using a new approach, we estimated the physical strength of the cell envelopes of three species of gram-negative, gas vacuolate bacteria (Microcyclus aquaticus, Prosthecomicrobium pneumaticum, and Meniscus glaucopis). Populations of cells were slowly (0.5 to 2.9 h) saturated with argon, nitrogen, or helium to final pressures up to 100 atm (10, 132 kPa). The gas phases of the vesicles remained intact and, upon rapid (1 to 2 s) decompression to atmospheric pressure, expanded and ruptured the cells; loss of colony-forming units was used as an index of rupture. Because the cell envelope is the cellular component most likely to resist the expanding intracellular gas phase, its strength can be estimated from the minimum gas pressures that produce rupture. The viable counts indicated that these minimum pressures were between 25 and 50 atm; the majority of the cell envelopes were ruptured at pressures between 50 and 100 atm. Cells in which the gas vesicles were collapsed and the gas phases were effectively dissolved by rapid compression tolerated decompression from much higher gas saturations. Cells that do not normally possess gas vesicles (Escherichia coli) or that had been prevented from forming them by addition of L-lysine to the medium (M. aquaticus) were not harmed by decompression from gas saturation pressures up to 300 atm.     

Prolonged exposure of mice to He-O2 at high pressure: effects on seizure and anesthesia liability

Multiday exposures of CD-1 mice to He-O2 atmospheres at pressures from 30 to 100 atm result in marked increases of threshold pressures for type I high-pressure neurological syndrome seizures. The effect develops with a half time (t1/2) of 12 h and is reversible (t1/2 = 7 h). The maximum enhancement of Pc is attained at a conditioning pressure of 80 ATA. Pressure conditioning also results in suppression of the compression rate effect on Pc. Furthermore, reserpine blocks the increase in Pc during prolonged pressure exposure. The entire effect thus appears to be an extension in time of the monoaminergic compression rate effect on Pc. Pressure conditioning does not modify anesthesia tolerance, unlike N2 habituation which affects anesthesia threshold pressure as well as Pc. The results are compared with the effects of habituation to inert-gas narcotics and the implications of the data for an understanding of inert-gas high-pressure antagonism in intact animals are discussed.     

The Influence of High Concentrations of Carbon Dioxide on the Germination of Bacterial Spores

The influence of carbon dioxide at 1–55 atm on the germination of Clostridium sporogenes, Clostridium perfringens and Bacillus cereus spores in a complex medium was studied. The germination studies at atmospheric pressure were done in the pH range 5.2–6.7. Controls at the same pH were done in 100% nitrogen. Carbon dioxide at atmospheric pressure (1 atm) inhibited the spore germination of B. cereus spores but strongly enhanced the germination rate of those of the clostridia. Spore germination of Cl. sporogenes and Cl. perfringens was inhibited completely at 10 atm and at 25 atm, respectively. The germination rate in carbon dioxide or nitrogen was generally higher at pH 6.7 than at 5.2–6.0.     

Effects of Hyperbaric Pressure on a Deep-Sea Archaebacterium in Stainless Steel and Glass-Lined Vessels

The effects of hyperbaric helium pressures on the growth and metabolism of the deep-sea isolate ES4 were investigated. In a stainless steel reactor, cell growth was completely inhibited but metabolic gas production was observed. From 85 to 100°C, CO₂ production proceeded two to three times faster at 500 atm (1 atm = 101.29 kPa) than at 8 atm. At 105°C, no CO₂ was produced until the pressure was increased to 500 atm. Hydrogen and H₂S were also produced biotically but were not quantifiable at pressures above 8 atm because of the high concentration of helium. In a glass-lined vessel, growth occurred but the growth rate was not accelerated by pressure. In most cases at temperatures below 100°C, the growth rate was lower at elevated pressures; at 100°C, the growth rates at 8, 250, and 500 atm were nearly identical. Unlike in the stainless steel vessel, CO₂ production was exponential during growth and continued for only a short time after growth. In addition, relatively little H₂ was produced in the glass-lined vessel, and there was no growth or gas production at 105°C at any pressure. The behavior of ES4 as a function of temperature and pressure was thus very sensitive to the experimental conditions.     

Study of the Formation Time of a Self-Sustained Subnanosecond Discharge at High and Ultrahigh Gas Pressures

The formation times of self-sustained subnanosecond discharges in nitrogen at pressures of 1?40 atm and in hydrogen at pressures of 1–60 atm are analyzed in terms of the avalanche model. In experiments, a subnanosecond voltage pulse with an amplitude of 102 ± 2 kV was applied to a 0.5-mm-long discharge gap with a uniformly distributed electric field (the curvature radii of both the cathode and anode ends were 1 cm). The rise time of the voltage pulse from 0.1 to 0.9 of its amplitude value was about 250 ps. Breakdown occurred at the leading edge of the pulse. The discharge formation time was measured at different gas pressures with a step of 5–10 atm. Analysis of the experimental results shows that, in nitrogen at pressures of 10–40 atm and in hydrogen at pressures of 20–50 atm, breakdown occurs earlier than the electron avalanche reaches its critical length and that the critical avalanche length lies in the range of (2–8) × 10^–2 mm, which is one order of magnitude shorter than the discharge gap length. This means that the avalanche–streamer model is inapplicable in this case. The fast formation of a conducting channel under these conditions can be explained by ionization of gas by runaway electrons. In this case, the conducting column develops as a result of simultaneous development of a large number of electron avalanches in the gas volume. An increase in the hydrogen pressure from 50 to 60 atm leads to an abrupt increase in the discharge formation time by about 50%. As a result, the growth time of the electron avalanche to its critical length becomes shorter than the discharge formation time. In this case, the electrons cease to pass into the runaway regime and the discharge is initiated from the cathode due to field emission from microinhomogeneities on its surface. Under these conditions, the discharge formation time is well described by the avalanche–streamer model.     

Effect of hydrostatic pressure on the solvent in crystals of hen egg-white lysozyme

The mass density of protein crystals can be measured in Ficoll gradients as a function of hydrostatic pressure. Carbon tetrachloride-toluene mixtures provide convenient density markers, and the compressibility of these standards is reported. Measurements on tetragonal crystals of hen egg-white lysozyme yielded densities at room temperature of 1.2367(+/- 0.0010) g cm-3 at 1 atm and 1.2586(+/- 0.0017) g cm-3 at 1000 atm (1 atm = 101,325 Pa). When combined with the unit cell dimensions at these two pressures these values lead to an estimated compression (fractional change in volume) of the crystal solvent at 1000 atm of 0.0369(+/- 0.0054). This value is comparable to that of a 0.7 M solution of NaCl. From an approximate estimate of the Donnan effect for the crystal in the 1.4 M-NaCl mother liquor, the crystal solvent contains 0.8 M-Na+ and 2.5 M-Cl-. It is concluded that the compressibility of solvent in lysozyme crystals is, within experimental error, the same as bulk solvent and does not exhibit the dramatically altered compressibility expected of an ice or glass-like solid. The crystallographically observable water sites, 151 at 1 atm and 163 at 1000 atm, showed a tendency to increase the number of hydrogen bonds made to other water sites at the expense of hydrogen bonds made to protein. The explanation for this phenomenon is presently unknown. Water sites that occur in both structures tend to have comparable temperature factors and show some tendency to follow the pressure-induced changes in protein atom positions. The compression expected for the water molecules themselves is too small to be observable at the resolution of the X-ray data collected in this study.     

Tissue ammonia and amino acids in rats at various oxygen pressures

The amino acid and ammonia profiles in various tissues of the rat exposed to different pressures of pure oxygen have been studied. Well-defined changes in behavioral activity accompanied a profile of increasing pressure, culminating in convulsive activity in each group of exposed animals. After an initial depression of ammonia, in all tissues studied at 0.68 atm oxygen ammonia increased significantly at higher oxygen pressures. A rise in tissue ammonia took place in the absence of undue muscular activity on the part of the exposed animals. A significant increase in ammonia occurred first in brain and liver at 3.40 atm. Ammonia concentration was high in all tissues after convulsions occurred at 4.08 atm. Between 0.68 and 2.72 atm oxygen, tissue ammonia concentration was generally low and brain glutamate and gamma-aminobutyric acid were high. At pressures higher than 2.72 atm oxygen, tissue glutamate declined and glutamine increased. Alanine became significantly elevated in serum and muscle at high oxygen pressure, and aspartate was depressed in heart, liver, and muscle. These pressure-course experiments on ammonia accumulation in tissue confirm previous serial time course observations that ammonia accumulates in the brain and several tissues of the rat even in the absence of undue muscular activity during high-pressure oxygen exposure and is a significant factor in inducing convulsions.     

Bubble formation in crabs induced by limb motions after decompression

In vivo bubble formation was studied in the megalopal stage of the crab Pachygrapsus crassipes. The animals were equilibrated with elevated argon, nitrogen, or helium pressures then rapidly decompressed to atmospheric pressure. Voluntary motions induced bubble nucleation in leg joints after exposures to as low as 2 atm nitrogen (gauge pressure). Delays of several minutes sometimes passed between decompression and bubble formation. Mechanically stimulating the animals to move their legs increased this bubble formation, whereas immobilizing the legs before gas equilibration prevented it, even in animals decompressed from 150 atm nitrogen. We conclude that preformed nuclei are not responsible for bubbles developing in the legs of this animal. Instead, tribonucleation of bubbles apparently occurs as a result of limb motions at relatively low gas supersaturations.     

Variability of pressure adaptation in deep sea bacteria

Isolations of pressure-adapted deep sea bacteria from depths of 1,400 to 5,100 m resulted in a variety of psychrophilic barotolerant and barophilic strains. Growth rates determined at different pressures indicated a gradual transition between the two types of pressure-adapted isolates. The presence of barotolerant bacteria in deep water, sustained by sinking particulate matter, causes the nonbarophilic response of natural populations, i.e., increased growth after decompression. With increasing pressure-adaptation in barophilic isolates the maximum growth rates at optimum pressures decrease. Thus, the observed general slow-down of microbial activity in the deep sea takes effect regardless of the common occurrence of psychrophilic and barophilic bacteria. The highest degree of barophilism was observed in isolates from nutrient-rich habitats such as intestinal tracts of deep sea animals or decaying carcasses. Detailed studies with an isolate, growing barophilically on a complex as well as a single-carbon-source medium, showed that (1) culturing at pressures lower than optimal for growth resulted in the formation of cell filaments, (2) growth was unaffected by repeated compression/decompression cycles and (3) no perceptible differences in the distribution of radiolabeled carbon from an amino acid mixture occurred in cells grown at, below and above the pressure optimal for growth.Dedicated to Professor Dr. Hans G. Schlegel on the occasion of his 60th birthday in recognition of his broad microbiological interests and in special appreciation of his lasting support for the Marine Microbiology Course at the Stazione Zoologica (Naples, Italy) now for almost 25 years Non-standard abbreviations. The traditional use of atm as a unit of pressure (=10 m of water column, =1.013 bar, =101.3 kN/m²) is retained here in view of the important relation between water depth and hydrostatic pressure in the present study. Due to the compression of seawater and the geographic variability of gravity, there is a progressive deviation of the actual pressure with depth amounting to +4.9 atm at 5,000 m and a latitude of 30°. EPC, cell counts obtained by epifluorescence microscopy. PY, peptone yeast extract medium     

Kinetics of Initiation of Germination of Bacillus pumilus Spores by Hydrostatic Pressure

The kinetics of initiation of germination and inactivation by hydrostatic pressure of phosphate-buffered Bacillus pumilus spores is shown to be a consecutive first-order process at 25 C. The effect of increasing pressure at constant temperature was studied, and rate constants were derived by using the criteria of heat resistance, refractility, and stainability. The calculated volume change of activation (DeltaVdouble dagger) was -139 +/- 6 cm(3)/mole for loss of heat resistance, -158 +/- 8 cm(3)/mole for the loss of refractility, and -153 +/- 4 cm(3)/mole for the change in permeability to dilute stains for the pressure range 800 to 1,010 atm at 25 C. It is suggested that the spore exists as a Donnan phase and that pressure triggers germination by influencing the equilibrium.     

New information on the mechanism of forcible ascospore discharge from Ascobolus immersus

Many ascomycete fungi spurt their spores from asci pressurized by osmosis. This paper explores the details of this process in the coprophilous species Ascobolus immersus, through a combination of biomechanical and biochemical experiments, and mathematical modeling. A. immersus forms large asci that expel 8 spores as a single, mucilage-embedded projectile. Measurements of ascus turgor using a microprobe attached to a strain gauge showed a pressure of 0.3 MPa or 3 atm. Analysis of ascus sap using GC/MS identified glycerol as a major osmolyte, accounting for 0.1 MPa of the osmotic pressure within the ascus sap. A mathematical model indicated that a pressure of 0.2 MPa would be sufficient to propel the cluster of ascospores over the distance measured in previous studies. The difference between the measured and predicted pressures is ascribed to loss of pressure as the spores are forced through the tip of the open ascus.     

High hydrostatic pressure effects in vivo: changes in cell morphology, microtubule assembly, and actin organization

We present the first study of the changes in the assembly and organization of actin filaments and microtubules that occur in epithelial cells subjected to the hydrostatic pressures of the deep sea. Interphase BSC-1 epithelial cells were pressurized at physiological temperature and fixed while under pressure. Changes in cell morphology and cytoskeletal organization were followed over a range of pressures from 1 to 610 atm. At atmospheric pressure, cells were flat and well attached. Exposure of cells to pressures of 290 atm or greater caused cell rounding and retraction from the substrate. This response became more pronounced with increased pressure, but the degree of response varied within the cell population in the pressure range of 290-400 atm. Microtubule assembly was not noticeably affected by pressures up to 290 atm, but by 320 atm, few microtubules remained. Most actin stress fibers completely disappeared by 290 atm. High pressure did not simply induce the overall depolymerization of actin filaments for, concurrent with cell rounding, the number of visible microvilli present on the cell surface increased dramatically. These effects of high pressure were reversible. Cells re-established their typical morphology, microtubule arrays appeared normal, and stress fibers reformed after approximately 1 hour at atmospheric pressure. High pressure may disrupt the normal assembly of microtubules and actin filaments by affecting the cellular regulatory mechanisms that control cytological changes during the transition from interphase into mitosis.     

Bubble formation in crustaceans following decompression from hyperbaric gas exposures

In vivo bubble formation was studied in various crustaceans equilibrated with high gas pressures and rapidly decompressed to atmospheric pressure. The species varied widely in susceptibility to bubble formation, and adults were generally more susceptible than larval stages. Bubbles did not form in early brine shrimp larvae unless equilibration pressures of at least 175 atm argon or 350 atm helium were used; for adult brine shrimp, copepods, and the larvae of crabs and shrimps, 100-125 atm argon or 175-225 atm helium were required. In contrast, bubbles formed in the leg joints of megalopa and adult crabs following decompression from only 3-10 atm argon; stimulation of limb movements increased this bubble formation, whereas inhibition of movements decreased it. High hydrostatic compressions applied before gas equilibration or slow compressions did not affect bubble formation. We concluded that circulatory systems, musculature, and storage lipids do not necessarily render organisms susceptible to bubble formation and that bubbles do not generally originate as preformed nuclei. In some cases, tribonucleation appears to be the cause of the bubbles.     

Pressure-adaptive differences in proteolytic inactivation of M4-lactate dehydrogenase homologues from marine fishes

The inactivation by hydrostatic pressure of muscle-type lactate dehydrogenase (M4-LDH, EC 1.1.1.27; L-lactate: NAD+ oxidoreductase) homologues from five shallow-living and six deep-living marine teleost fishes was compared. The pressures which inactivate these enzymes are much higher than the pressures experienced by any of the species. To determine whether hydrostatic pressure effects on protein aggregation state and conformation might influence proteolysis, the inactivation of LDH by the proteases, trypsin (EC 3.4.21.4) and subtilisin (EC 3.4.4.16) was determined at atmospheric pressure and 1,000 atm pressure. At 10 degrees C and atmospheric pressure, the enzymes of the shallow-living fishes are inactivated four times faster by trypsin and three times faster by subtilisin than are the homologues of the deep-living species. At 1,000 atm pressure, the homologues of shallow-occurring fishes were inactivated 28 to 64% more than predicted from the summed effects of denaturation by 1,000 atm pressure and tryptic inactivation at atmospheric pressure. In contrast, the homologues of the deep-sea species were inactivated by trypsin 0 to 21% more than expected. At 1,000 atm, inactivation by subtilisin increased to a similar degree for enzymes from both deep- and shallow-living species. However, at 1,000 atm, the M4-LDH homologues of the deep-sea species lost less activity (55.3%) than did the homologues of the shallow species (86.4%). In comparisons made at 200 atm, a pressure typical of the habitat of the deep-occurring species, tryptic inactivation of the LDH of the shallow-living Sebastes melanops was increased 14%. No pressure inactivation of the enzyme is evident at 200 atm.(ABSTRACT TRUNCATED AT 250 WORDS)     

Effect of oxygen on batch and continuous cultures of a nitrogen-fixing Arthrobacter sp.

Growth, acetylene reduction, and respiration rate were studied in batch and continuous cultures of Arthrobacter fluorescents at different oxygen partial pressures. The optimum pO2 values for growth and acetylene reduction were 0.05 and 0.025 atm, respectively, but microorganisms can tolerate higher pO2 values. The growth of cultures provided with combined nitrogen was dependent on oxygen availability, and strict anaerobic conditions did not support growth. Acetylene reduction of a population grown in continuous culture and adapted to low pO2 (0.02 atm) was much more sensitive to oxygenation than that of a population adapted to high pO2 (0.4 atm). Their maximum nitrogenase activity, at their optimal pO2 values, were quite different. The respiratory activity of nitrogen-fixing cultures increased with increasing oxygen tensions until a pO2 of 0.2 atm. At higher pO2 values, the respiration rate began to decrease.     

A Study of the Effects of Hydrostatic Pressure on Macromolecular Synthesis in Escherichia coli

In cultures of Escherichia coli 15 (thymine^-, leucine^-) which were incubated at high hydrostatic pressures, cell division occurred only at pressures below 430 atm but in a somewhat synchronous fashion at around 250 atm. The rate of leucine-¹⁴C incorporation into a macromolecular fraction of the cells diminished to a zero value at about 580 atm and that of uracil-¹⁴C incorporation to a zero value at about 770 atm. The rate of thymine-¹⁴C incorporation at pressures around 330 atm was that to be expected with a culture in which DNA synthesis is somewhat synchronous. At pressures above 500 atm, thymine-¹⁴C was incorporated only over the initial part of the pressure incubation and further incorporation under pressure was not observed no matter how long the duration of the incubation. We present evidence along several lines that the thymine incorporation kinetics reflect an effect of pressure on a locus at the origin (or termination) of a replication of the bacterial chromosome. The recovery of cell division and of the incorporation rates upon release of pressure were found to depend on the magnitude of the pressure and the duration of the pressure incubation.     

Pressure and Temperature Effects on Growth and Methane Production of the Extreme Thermophile Methanococcus jannaschii

The marine archaebacterium Methanococcus jannaschii was studied at high temperatures and hyperbaric pressures of helium to investigate the effect of pressure on the behavior of a deep-sea thermophile. Methanogenesis and growth (as measured by protein production) at both 86 and 90°C were accelerated by pressure up to 750 atm (1 atm = 101.29kPa), but growth was not observed above 90°C at either 7.8 or 250 atm. However, growth and methanogenesis were uncoupled above 90°C, and the high-temperature limit for methanogenesis was increased by pressure. Substantial methane formation was evident at 98°C and 250 atm, whereas no methane formation was observed at 94°C and 7.8 atm. In contrast, when argon was substituted for helium as the pressurizing gas at 250 atm, no methane was produced at 86°C. Methanogenesis was also suppressed at 86°C and 250 atm when the culture was pressurized with a 4:1 mix of H₂ and CO₂, although limited methanogenesis did occur when the culture was pressurized with H₂.     

Effects of hyperoxia on composition and rate of synthesis of fatty acids in Escherichia coli

Growth of and fatty acid synthesis in Escherichia coli were inhibited by oxygen at partial pressures above 1 atm and were prevented by exposure to oxygen at 4.2 atm on membranes incubated on a minimal medium. Growth and fatty acid synthesis returned to control rates when cells were removed from hyperoxia to air. The spectrum of fatty acids produced was unchanged by oxygen at pressures which reduced the rate of synthesis. In situ fatty acids were stable to oxygen at pressures which prevented growth and synthesis. Reinitiation of synthesis after complete inhibition in hyperoxia occurred without production of aberrant fatty acids. Fatty acid synthetase specific activity was virtually unchanged, compared with air controls, in cells exposed either to 3.2 or to 15.2 atm of oxygen. The spectrum of fatty acids synthesized by cell-free extracts during incubation in 4.2 atm of oxygen was not different from air-incubated controls. Synthetase assays included added NADPH, acyl carrier protein, mercaptoethanol, and malonyl coenzyme A; hence, damage, other than reversible sulfhydryl oxidation, to the apoenzymes of synthetase was ruled out.