Pressure built by DNA packing inside virions: enough to drive DNA ejection in vitro, largely insufficient for delivery into the bacterial cytoplasm

Tailed bacteriophage particles carry DNA highly pressurized inside the capsid. Challenge with their receptor promotes release of viral DNA. We show that addition of the osmolyte polyethylene glycol (PEG) has two distinct effects in bacteriophage SPP1 DNA ejection. One effect is to inhibit the trigger for DNA ejection. The other effect is to exert an osmotic pressure that controls the extent of DNA released in phages that initiate ejection. We carried out independent measurements of each effect, which is an essential requirement for their quantitative study. The fraction of phages that do not eject increased linearly with the external osmotic pressure. In the remaining phage particles ejection stopped after a defined amount of DNA was reached inside the capsid. Direct measurement of the size of non-ejected DNA by gel electrophoresis at different PEG concentrations in the latter sub-population allowed determination of the external osmotic pressure that balances the force powering DNA exit (47 atm for SPP1 wild-type). DNA exit stops when the ejection force mainly due to repulsion between DNA strands inside the SPP1 capsid equalizes the force resisting DNA insertion into the PEG solution. Considering the turgor pressure in the Bacillus subtilis cytoplasm the energy stored in the tight phage DNA packing is only sufficient to power entry of the first 17% of the SPP1 chromosome into the cell, the remaining 83% requiring application of additional force for internalization.     

Effects of salt concentrations and bending energy on the extent of ejection of phage genomes

Recent work has shown that pressures inside dsDNA phage capsids can be as high as many tens of atmospheres; it is this pressure that is responsible for initiation of the delivery of phage genomes to host cells. The forces driving ejection of the genome have been shown to decrease monotonically as ejection proceeds, and hence to be strongly dependent on the genome length. Here we investigate the effects of ambient salts on the pressures inside phage-λ, for the cases of mono-, di-, and tetravalent cations, and measure how the extent of ejection against a fixed osmotic pressure (mimicking the bacterial cytoplasm) varies with cation concentration. We find, for example, that the ejection fraction is halved in 30 mM Mg²⁺ and is decreased by a factor of 10 upon addition of 1 mM spermine. These effects are calculated from a simple model of genome packaging, using DNA-DNA repulsion energies as determined independently from x-ray diffraction measurements on bulk DNA solutions. By comparing the measured ejection fractions with values implied from the bulk DNA solution data, we predict that the bending energy makes the d-spacings inside the capsid larger than those for bulk DNA at the same osmotic pressure.     

Polymorphism of DNA conformation inside the bacteriophage capsid

Double-stranded DNA bacteriophage genomes are packaged into their icosahedral capsids at the highest densities known so far (about 50 % w:v). How the molecule is folded at such density and how its conformation changes upon ejection or packaging are fascinating questions still largely open. We review cryo-TEM analyses of DNA conformation inside partially filled capsids as a function of the physico-chemical environment (ions, osmotic pressure, temperature). We show that there exists a wide variety of DNA conformations. Strikingly, the different observed structures can be described by some of the different models proposed over the years for DNA organisation inside bacteriophage capsids: either spool-like structures with axial or concentric symmetries, or liquid crystalline structures characterised by a DNA homogeneous density. The relevance of these conformations for the understanding of DNA folding and unfolding upon ejection and packaging in vivo is discussed.     

Osmotic pressure: resisting or promoting DNA ejection from phage?

Recent in vitro experiments have shown that DNA ejection from bacteriophage can be partially stopped by surrounding osmotic pressure when ejected DNA is digested by DNase I in the course of ejection. In this work, we argue by a combination of experimental techniques (osmotic suppression without DNase I monitored by UV absorbance, pulse-field electrophoresis, and cryo-transmission electron microscopy visualization) and simple scaling modeling that intact genome (i.e., undigested) ejection in a crowded environment is, on the contrary, enhanced or eventually complete with the help of a pulling force resulting from DNA condensation induced by the osmotic stress itself. This demonstrates that in vivo, the osmotically stressed cell cytoplasm will promote phage DNA ejection rather than resist it. The further addition of DNA-binding proteins under crowding conditions is shown to enhance the extent of ejection. We also found some optimal crowding conditions for which DNA content remaining in the capsid upon ejection is maximum, which correlates well with the optimal conditions of maximum DNA packaging efficiency into viral capsids observed almost 20 years ago. Biological consequences of this finding are discussed.     

Bacteriophage T5 DNA ejection under pressure

The transfer of the bacteriophage genome from the capsid into the host cell is a key step of the infectious process. In bacteriophage T5, DNA ejection can be triggered in vitro by simple binding of the phage to its purified Escherichia coli receptor FhuA. Using electrophoresis and cryo-electron microscopy, we measure the extent of DNA ejection as a function of the external osmotic pressure. In the high pressure range (7-16 atm), the amount of DNA ejected decreases with increasing pressure, as theoretically predicted and observed for λ and SPP1 bacteriophages. In the low and moderate pressure range (2-7 atm), T5 exhibits an unexpected behavior. Instead of a unique ejected length, multiple populations coexist. Some phages eject their complete genome, whereas others stop at some nonrandom states that do not depend on the applied pressure. We show that contrarily to what is observed for the phages SPP1 and λ, T5 ejection cannot be explained as resulting from a simple pressure equilibrium between the inside and outside of the capsid. Kinetics parameters and/or structural characteristics of the ejection machinery could play a determinant role in T5 DNA ejection.     

Uncoating the herpes simplex virus genome

Initiation of infection by herpes simplex virus (HSV-1) involves a step in which the parental virus capsid docks at a nuclear pore and injects its DNA into the nucleus. Once "uncoated" in this way, the virus DNA can be transcribed and replicated. In an effort to clarify the mechanism of DNA injection, we examined DNA release as it occurs in purified capsids incubated in vitro. DNA ejection was observed following two different treatments, trypsin digestion of capsids in solution, and heating of capsids after attachment to a solid surface. In both cases, electron microscopic analysis revealed that DNA was ejected as a single double helix with ejection occurring at one vertex presumed to be the portal. In the case of trypsin-treated capsids, DNA release was found to correlate with cleavage of a small proportion of the portal protein, UL6, suggesting that UL6 cleavage may be involved in making the capsid permissive for DNA ejection. In capsids bound to a solid surface, DNA ejection was observed only when capsids were warmed above 4 degrees C. The proportion of capsids releasing their DNA increased as a function of incubation temperature with nearly all capsids ejecting their DNA when incubation was at 37 degrees C. The results demonstrate heterogeneity among HSV-1 capsids with respect to their sensitivity to heat-induced DNA ejection. Such heterogeneity may indicate a similar heterogeneity in the ease with which capsids are able to deliver DNA to the infected cell nucleus.     

Regulation of intracellular glycine as an organic osmolyte in early preimplantation mouse embryos

GLYT1, a glycine transporter belonging to the neurotransmitter transporter family, has recently been identified as a novel cell volume-regulatory mechanism in the earliest stages of the mouse preimplantation embryo. It apparently acts by regulating the steady-state intracellular concentration of glycine, which functions as an organic osmolyte in embryos, to balance external osmolarity and thus maintain cell volume. GLYT1 in embryos was the first mammalian organic osmolyte transporter identified that appears to function in cell volume control under conditions of normal osmolarity, rather than being a response to the stress of chronic hypertonicity. Its maximal rate of transport was shown to be regulated by osmolarity. However, it was not known whether this osmotic regulation of the rate of glycine transport is sufficient to account for the observed control of steady-state intracellular glycine levels as a function of osmolarity in embryos. Here, we show that the intracellular accumulation of glycine in embryos is a direct function of the rate of glycine uptake via GLYT1. In addition, we have shown that the rate of efflux, likely via the volume-regulated anion and organic osmolyte channel in embryos, is also under osmotic regulation and contributes substantially to the control of steady-state glycine concentrations. Together, control of both the rate of uptake and rate of efflux of glycine underlies the mechanism of osmotic regulation of the steady-state concentration of glycine and hence cell volume in early embryos.     

Biophysical and Ultrastructural Characterization of Adeno-Associated Virus Capsid Uncoating and Genome Release

We describe biophysical and ultrastructural differences in genome release from adeno-associated virus (AAV) capsids packaging wild-type DNA, recombinant single-stranded DNA (ssDNA), or dimeric, self-complementary DNA (scDNA) genomes. Atomic force microscopy and electron microscopy (EM) revealed that AAV particles release packaged genomes and undergo marked changes in capsid morphology upon heating in physiological buffer (pH 7.2). When different AAV capsids packaging ss/scDNA varying in length from 72 to 123% of wild-type DNA (3.4 to 5.8 kb) were incrementally heated, the proportion of uncoated AAV capsids decreased with genome length as observed by EM. Genome release was further characterized by a fluorimetric assay, which demonstrated that acidic pH and high osmotic pressure suppress genome release from AAV particles. In addition, fluorimetric analysis corroborated an inverse correlation between packaged genome length and the temperature needed to induce uncoating. Surprisingly, scAAV vectors required significantly higher temperatures to uncoat than their ssDNA-packaging counterparts. However, externalization of VP1 N termini appears to be unaffected by packaged genome length or self-complementarity. Further analysis by tungsten-shadowing EM revealed striking differences in the morphologies of ssDNA and scDNA genomes upon release from intact capsids. Computational modeling and molecular dynamics simulations suggest that the unusual thermal stability of scAAV vectors might arise from partial base pairing and optimal organization of packaged scDNA. Our work further defines the biophysical mechanisms underlying adeno-associated virus uncoating and genome release.     

Dynamics of bacteriophage genome ejection in vitro and in vivo

Bacteriophages, phages for short, are viruses of bacteria. The majority of phages contain a double-stranded DNA genome packaged in a capsid at a density of ～500 mg ml(-1). This high density requires substantial compression of the normal B-form helix, leading to the conjecture that DNA in mature phage virions is under significant pressure, and that pressure is used to eject the DNA during infection. A large number of theoretical, computer simulation and in vitro experimental studies surrounding this conjecture have revealed many--though often isolated and/or contradictory--aspects of packaged DNA. This prompts us to present a unified view of the statistical physics and thermodynamics of DNA packaged in phage capsids. We argue that the DNA in a mature phage is in a (meta)stable state, wherein electrostatic self-repulsion is balanced by curvature stress due to confinement in the capsid. We show that in addition to the osmotic pressure associated with the packaged DNA and its counterions, there are four different pressures within the capsid: pressure on the DNA, hydrostatic pressure, the pressure experienced by the capsid and the pressure associated with the chemical potential of DNA ejection. Significantly, we analyze the mechanism of force transmission in the packaged DNA and demonstrate that the pressure on DNA is not important for ejection. We derive equations showing a strong hydrostatic pressure difference across the capsid shell. We propose that when a phage is triggered to eject by interaction with its receptor in vitro, the (thermodynamic) incentive of water molecules to enter the phage capsid flushes the DNA out of the capsid. In vivo, the difference between the osmotic pressures in the bacterial cell cytoplasm and the culture medium similarly results in a water flow that drags the DNA out of the capsid and into the bacterial cell.     

Effect of salt concentration on membrane lysis pressure

Cell membranes are capable of withstanding significant osmotic stress, the exact amount of which varies with the lipid composition. In this paper, we examine the effect that salt concentration has on the lysis pressure of membranes containing anionic lipids. Vesicles containing varying amounts of phosphatidylcholine and phosphatidylglycerol were osmotically stressed using NaCl as the osmolyte. The lysis pressure was observed to vary linearly with the Debye screening length and the extent of the variation was linear with anionic lipid content. The implications these results have for cells that frequently encounter low solute environments are discussed.     

DNA Ejection from an Archaeal Virus—A Single-Molecule Approach

The translocation of genetic material from the viral capsid to the cell is an essential part of the viral infection process. Whether the energetics of this process is driven by the energy stored within the confined nucleic acid or cellular processes pull the genome into the cell has been the subject of discussion. However, in vitro studies of genome ejection have been limited to a few head-tailed bacteriophages with a double-stranded DNA genome. Here we describe a DNA release system that operates in an archaeal virus. This virus infects an archaeon Haloarcula hispanica that was isolated from a hypersaline environment. The DNA-ejection velocity of His1, determined by single-molecule experiments, is comparable to that of bacterial viruses. We found that the ejection process is modulated by the external osmotic pressure (polyethylene glycol (PEG)) and by increased ion (Mg²⁺ and Na⁺) concentration. The observed ejection was unidirectional, randomly paused, and incomplete, which suggests that cellular processes are required to complete the DNA transfer.     

Effect of salt concentration on membrane lysis pressure

Cell membranes are capable of withstanding significant osmotic stress, the exact amount of which varies with the lipid composition. In this paper, we examine the effect that salt concentration has on the lysis pressure of membranes containing anionic lipids. Vesicles containing varying amounts of phosphatidylcholine and phosphatidylglycerol were osmotically stressed using NaCl as the osmolyte. The lysis pressure was observed to vary linearly with the Debye screening length and the extent of the variation was linear with anionic lipid content. The implications these results have for cells that frequently encounter low solute environments are discussed.     

Osmotic shock and the strength of viral capsids

Osmotic shock is a familiar means for rupturing viral capsids and exposing their genomes intact. The necessary conditions for providing this shock involve incubation in high-concentration salt solutions, and lower permeability of the capsids to salt ions than to water molecules. We discuss here how values of the capsid strength can be inferred from calculations of the osmotic pressure differences associated with measured values of the critical concentration of incubation solution.     

DNA Heats Up: Energetics of Genome Ejection from Phage Revealed by Isothermal Titration Calorimetry

Most bacteriophages are known to inject their double-stranded DNA into bacteria upon receptor binding in an essentially spontaneous way. This downhill thermodynamic process from the intact virion to the empty viral capsid plus released DNA is made possible by the energy stored during active packaging of the genome into the capsid. Only indirect measurements of this energy have been available until now, using either single-molecule or osmotic suppression techniques. In this work, we describe for the first time the use of isothermal titration calorimetry to directly measure the heat released (or, equivalently, the enthalpy) during DNA ejection from phage λ, triggered in solution by a solubilized receptor. Quantitative analyses of the results lead to the identification of thermodynamic determinants associated with DNA ejection. The values obtained were found to be consistent with those previously predicted by analytical models and numerical simulations. Moreover, the results confirm the role of DNA hydration in the energetics of genome confinement in viral capsids.     

Forces controlling the rate of DNA ejection from phage lambda

The goal of this work was to investigate how internal and external forces acting on DNA affect the rate of genome ejection from bacteriophage lambda after the ejection is triggered in vitro by a lambda receptor. The rate of ejection was measured with time-resolved static and dynamic light scattering, while varying such parameters as temperature and packaged DNA length, as well as adding DNA-binding proteins to the host solution. We found that temperature has a strong effect on the ejection rate, with an exponential increase of the initial ejection rate as a function of temperature. This can possibly be explained by the temperature-induced conformational changes in the tail pore-forming proteins where the "open" conformation dominates over "closed", at elevated temperatures. The DNA length also had an effect on initial ejection rate, with a nearly linear dependence comparing the three different genomes (37.7, 45.7 and 48.5 kb DNA), with faster ejection rate for longer genomes. Since the initial rate of ejection increases in an almost direct relationship with the length of the genome, the total time needed to eject DNA completely appeared to be nearly constant for all three DNA length phage mutants. The increased initial rate of ejection with increasing DNA length is due to the increased DNA bending and inter-strand repulsion forces for the longer DNA chains. Finally, we also show that addition of non-specific DNA-binding proteins (HU and DNase I) increases the rate of ejection by exerting additional "pulling" forces on the DNA that is being ejected.     

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.     

Forces during bacteriophage DNA packaging and ejection

The conjunction of insights from structural biology, solution biochemistry, genetics, and single-molecule biophysics has provided a renewed impetus for the construction of quantitative models of biological processes. One area that has been a beneficiary of these experimental techniques is the study of viruses. In this article we describe how the insights obtained from such experiments can be utilized to construct physical models of processes in the viral life cycle. We focus on dsDNA bacteriophages and show that the bending elasticity of DNA and its electrostatics in solution can be combined to determine the forces experienced during packaging and ejection of the viral genome. Furthermore, we quantitatively analyze the effect of fluid viscosity and capsid expansion on the forces experienced during packaging. Finally, we present a model for DNA ejection from bacteriophages based on the hypothesis that the energy stored in the tightly packed genome within the capsid leads to its forceful ejection. The predictions of our model can be tested through experiments in vitro where DNA ejection is inhibited by the application of external osmotic pressure.     

Is phage DNA 'injected' into cells--biologists and physicists can agree

The double-stranded DNA inside bacteriophages is packaged at a density of approximately 500 mg/ml and exerts an osmotic pressure of tens of atmospheres. This pressure is commonly assumed to cause genome ejection during infection. Indeed, by the addition of their natural receptors, some phages can be induced in vitro to completely expel their genome from the virion. However, the osmotic pressure of the bacterial cytoplasm exerts an opposing force, making it impossible for the pressure of packaged DNA to cause complete genome ejection in vivo. Various processes for complete genome ejection are discussed, but we focus on a novel proposal suggesting that the osmotic gradient between the extracellular environment and the cytoplasm results in fluid flow through the phage virion at the initiation of infection. The phage genome is thereby sucked into the cell by hydrodynamic drag.     

Concentration dependence of the subunit association of oligomers and viruses and the modification of the latter by urea binding.

A theoretical model is presented that accounts for the facilitation of the pressure dissociation of R17 phage, and for the partial restoration of the concentration dependence of the dissociation, by the presence of subdenaturing concentrations of urea. As an indifferent osmolyte urea should promote the stability of the protein aggregates under pressure, and the decrease in pressure stability with urea concentration demonstrates that such indirect solvent effects are not significant for this case, and that the progressive destabilization is the result of direct protein-urea interactions. By acting as a "homogenizer" of the properties of the phage particles, urea addition converts the pressure-induced deterministic dissociation of the phage into a limited stochastic equilibrium. The model establishes the origin of the uniform progression from the stochastic equilibrium of dimers, to the temperature-dependent and partially concentration-dependent association of tetramers, to the fully deterministic equilibrium observed in many multimers and in the virus capsids.     

Bacteriophage P22 in vitro DNA packaging monitored by agarose gel electrophoresis: rate of DNA entry into capsids.

Bacteriophage P22, like other double-stranded DNA bacteriophages, packages DNA in a preassembled, DNA-free procapsid. The P22 procapsid and P22 bacteriophage have been electrophoretically characterized; the procapsid has a negative average electrical surface charge density (sigma) higher in magnitude than the negative sigma of the mature bacteriophage. Dextrans, sucrose, and maltose were shown to have a dramatic stimulatory effect on the in vitro packaging of DNA by the P22 procapsid. However, sedoheptulose, smaller sugars, and smaller polyols did not stimulate in vitro P22 DNA packaging. These and other data suggest that an osmotic pressure difference across some particle, probably a capsid, stimulates P22 DNA packaging. After in vitro packaging was optimized by including dextran 40 in extracts, the entry kinetics of DNA into P22 capsids were measured. Packaged DNA was detected by: (i) DNA-specific staining of intact capsids after fractionation by agarose gel electrophoresis and (ii) agarose gel electrophoresis of DNase-resistant DNA after release of DNase-resistant DNA from capsids. It was found that the first DNA was packaged by 1.5 min after the start of incubation. The data further suggest that either P22 capsids with DNA partially packaged in vitro are too unstable to be detected by the above procedures or entry of DNA into the capsid occurs in less than 0.25 min.