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FEMS MicrobiologyEcology 15 (1994) 99-108 © 1994 Federation of European Microbiological Societies 0168-6496/94/$07.00 Published by Elsevier 99 FEMSEC 00576 MiniReview Phage-host interactions in soil P. M a r s h * a n d E . M . H . W e l l i n g t o n Department of Biological Sciences, University of Warwick, Coventry CF7 4AL, UK (Received 10 March 1994; revision received 18 April 1994; accepted 25 April 1994) Abstract: Phages are abundant and ubiquitous in nature, and are therefore important components of microbial communities. They can impact on host populations in several ways, including predation and alteration of host phenotype by genetic interactions. The dynamic survival of phage populations in soil requires infective interactions with host populations which must be undergoing growth. Hence survivalis limited by the activityof soil bacteria, and phage populations must adopt strategies to overcome periods of inactivity. One of the most effective strategies is the lysogeniccycle of temperate phages. It is argued here that lysogenyin soil has a distinct advantage over virulence for phage and host survival, as opposed to aquatic ecosystemswhere virulence seems a more successful strategy for phage populations. Key words: Phage ecology; Soil streptomycetes; Phage-host interaction; Lysogeny Introduction The ecology of bacteriophages has received comparatively little attention despite their abundance in natural environments. Phages can usually be isolated from all habitats where their hosts exist, and are ubiquitous components of bacterial communities [1]. Ecosystems which allow active bacterial growth have the potential to support multiplication of phage populations which require metabolically active hosts. The presence of phage populations in these ecosystems therefore presents a potential impact on bacterial populations. Our aim is to review the importance of phages in natural environments with particular regard to soil. This will involve consideration of * Corresponding author. SSDI 0168-6496(94)00059-X the abundance of phages in nature, their survival strategies, their impact on host populations, their role in genetic interactions and the importance of lysogeny. Phages are predators or parasites of host bacteria which although they are able to persist in the environment independently of their hosts, they have the absolute requirement to infect host cells in order to multiply and survive as dynamic populations [2]. For multiplication to occur in the environment a phage particle must be able to protect its genome from adverse conditions, gain access to infect a susceptible host and change the host cell into a unit for producing phage progeny which are finally released. Free phage particles have to protect the genome from environmental damage in a protein capsule known as the capsid [3]. The most common phage morphology is that of an isometric protein head classified as A and B 100 types, which have sheathed contractile or unsheathed noncontractile hollow tails respectively [4,5]. Head size is generally between 50 and 100 nm whereas tail length varies greatly between types and can be up to 200 nm [3,6]. A tail plate is usually situated at the end of the tail, and this apparatus is responsible for mediating specific adsorption of phages to host cell surfaces prior to infection. Phages are categorized into two main types depending on the infection cycle they may follow on delivery of the genome into a host cell. Phages which can only lyse the infected host cell to produce daughter progeny follow the lytic cycle of infection and are termed virulent [7]. Those which follow either the lytic cycle or the lysogenic cycle, where the phage genome is retained as a replicable entity within the host without causing lysis, are termed temperate phages [7]. Another type of phage multiplication which cannot be characterized as either the lytic or lysogenic cycle is that of the filamentous phages, which attach to the sex pili of F + Gram-negative bacteria and mediate production of progeny particles from the growing cell without causing lysis [7]. Contact between the host and phage may result in reversible binding of the phage end plate to the host cell surface which often requires the presence of divalent cations such as Ca 2+ and Mg 2+. Pins on the tail plate allow irreversible binding with specific receptors on the cell surface, and enzymes from the tail pin alter this site to enable entry of the phage genome into the cell lumen. Phage-encoded signals then cause shutdown or alteration of the cell's RNA and protein synthesis, and the conversion of the cell into a factory producing copies of the progenitor phage particle. Phage-induced lysozyme causes rupture of the cell wall followed by release of the daughter progeny into the environment. At this point, large amounts of lysozyme are also liberated [2,3,7]. The lysogenic cycle of temperate phages is initiated after entry of the genome into the cell cytoplasm, and the choice of this cycle rather than the lytic cycle is dependant upon the expression of host and phage genes as well as environmental conditions which also influence this ex- pression [8-10]. Generally, environmental conditions which are unfavourable for host proliferation will cause increased frequencies of lysogeny. For example, there is evidence [9] that production of cellular cAMP-CAP due to starvation conditions leads to the inhibition of host Hfl (high frequency of lysogenization) protein which in turn allows the establishment of lysogeny by phage ,~. High multiplicities of infection (m.o.i.) lead to excess amounts of phage-encoded protein cIII in cells which also antagonizes Hfl and leads to increased frequencies of lysogeny [9]. These influences lead to the suppression of lytic cycle genes, and allow the expression of lysogenic cycle genes which cause integration of the phage genome into the host chromosome, and subsequent expression of repressor protein(s) which prevent regression into the lytic cycle [11]. The integrated phage genome is known as the prophage, and is replicated with the host genome at cell division without lysing the host. Some temperate phages such as coliphage P1 do not integrate into the host chromosome, but exist in a repressed replicable extra-chromosomal state. The host is now termed lysogenic [12], and is immune to superinfecting phages with genome sites homologous to the binding site of the repressor proteins being produced by the prophage. Reversion to the lytic cycle occurs at a certain frequency in growing lysogenic populations, although prophage induction is usually caused by cellular damage, especially that which affects the host DNA. This causes loss of expression of the repressor protein and therefore a switching on of the lyric cycle. Certain virulent phages can exist inside dormant hosts in an arrested stage of the lytic cycle, which can resume when the host recommences vegetative growth. This state is known as pseudolysogeny [13]. Around 90% of all phages isolated from natural environments have proved to be temperate [2], so it may be postulated that temperate phages have an advantage over virulent phages which require actively growing hosts to multiply. Temperate phages can exist as prophages in hosts through long periods of inactivity when free virions in the environment may become inactivated. When considering phage populations in a particu- 101 lar ecosystem, one question to be addressed concerns mode of cell-to-cell transmission. In virulent populations the only available route is horizontal transmission, where the lytic cycle is a rapid form of multiplication, but entails a high risk in that the infected cell is destroyed leaving the progeny particles with the possibility that new susceptible host cells may not be encountered. Temperate phage populations can follow the lysogenic cycle, during which the prophage is replicated along with the host chromosome. This produces far less copies of the original prophage at a slower rate than the lytic cycle, but has the advantage of greater security in that the host is maintained in a replicable state, protecting the phage [14]. The abundance of phages in natural environments Early studies have shown that phages were present in very low numbers in natural environments, so it was assumed that they were of little ecological importance. This assumption was based on counts made by plating phages on indicator host strains. More recent studies have used transmission electron microscopy (TEM) to make direct counts of viruses in aquatic samples (Table 1). These figures indicate that phages can be present at very high densities. Direct phage counts have so far not been made from soil, due in part Table 2 Abundance of phages in bulk soil Phage type pfu a on indicator Reference host/g soil 4.0 x 1 0 7 3.4 x 103 Actinomycete(temperate) 3.6 x 104 Actinomycete(virulent) 3.6 x 102 Actinomycete 2.0 × 104 Arthrobacter 7.1 × 102 22 23 24 24 25 26 Bacillus Ensifer adhaerans a pfu, plaque forming units. to the difficulty in preparing samples suitable for TEM. Counts of soil phages have been made using indicator strains, and as in aquatic systems the total phage densities may be much higher than shown in Table 2. This abundance in ecosystems makes phage populations important in terms of their influences on host population levels and activity, as well as host population evolution due to the intimacy of phage and host genomes. This last point is emphasised by the suggestion that phages, in conditions beneficial to their multiplication, are the most numerous self-perpetuating genetic objects in soil [22]. Phage survival in nature The main requirement for the survival of a parasite or predator population is that the host or Table 1 The abundance of phages in aquatic environments Sample Marine (reefwater) (sediment) Marine Marine Marine Marine Freshwater Freshwater Activated sludge Phage type pill a on indicator host (ml - 1) Direct counts (TEM, ml- 1) Reference mixed b 0.19 8.8 1.5 x 103 3.0 1.2 x 104 5.3 × 10s 3.5 X 10 7 1.3 x 1 0 7 1.5 X 107 2.5 x 10s - 15 15 16 17 18 19 19 20 1.7 × 102/ml - 21 mixed mixed mixed mixed mixed coliphages coliphages a pfu, plaque forming units. b Includes vibrio- and coliphages. - 102 prey population must not be made extinct by predation. This is often ensured by density dependent regulation of interacting phage and host populations, and is manifested as alternating oscillations of phage and host populations where both exist in a state of equilibrium [27,28]. Such oscillations have been observed in the marine environment [18]. The persistence of steady state requires the continual multiplication of host populations and hence requires sustained nutrient input. Phages in aquatic ecosystems are subject to continual movement and therefore have a relatively high probability of encountering susceptible hosts [29]. The fluxing nature of aquatic ecosystems also facilitates the delivery of nutrients via primary production, for example during spring blooms in marine ecosystems. This in turn allows bacterial blooms and consequent peaks in phage populations. These peaks may be responsible for controlling bacterial populations as they are quickly followed by a drop in host numbers [16,18,30]. This type of environment would seem to favour the virulent phages which may move freely in the water and have access to active bacterial populations. The rapid generation times of phage and bacterial populations facilitates the development of new phenotypes. This is well illustrated by mutations to infection immunity in bacteria, and subsequent counter-mutations by phages to overcome host immunity [31]. This leads to polymorphic host and phage populations where there originally existed one clone each of host and phage [32]. In soil, free phages are in close contact with soil components, and physical interactions between such particles and phages greatly influence their survival. This can be beneficial or deleterious to the phage population depending on phage and clay types. For example, the pH optima of actinophages may be expanded or reduced by binding to different types of clays [33]. Clay particles provide a highly active medium on which phage-host interactions may take place. Cations around clays will bind negatively charged phages and bacteria, as well as proteins and other nutrient molecules providing substrates for host -] --'1 ~ 4 o 2 ._/ ~0 -~ 0 i t I I 5 I I I k ~ 10 I I I I ] 15 Time (days) Fig. 1. Growth of indigenous streptomycetes and increase in free phage titre in pre-dried nonsterile amended (2% w / w chitin) soil wetted (to 15% moisture) at day 0. Growth of hosts is shown by increases in total ( n ) and spore (in) counts. Temperate (*) and virulent ( o ) phages were detected 24 h after initial wetting of soil (Marsh and Wellington, 1993. Unpublished data), growth, although there can be competition between phages and proteins for binding sites [34,35]. Phages will often bind strongly to clays [33] and infectivity can be prolonged according to phage and clay type [36]. Infective free phages can persist in soil for long periods of time [1]. It could therefore be argued that virulent phages reside in the free state in soil for prolonged periods of host inactivity, and resume multiplication as the host grows. Virulent actinophages can be readily isolated from soil which has been previously air-dried for several months, and then re-wetted with sterile distilled water (Fig. 1). The exact origin of these phages is unclear as neither virulent nor temperate actinophages were detected at time 0 of incubation. The initial burst in indigenous phage numbers after 24 h incubation could either represent gradual elution of phages tightly bound to clay particles, or the release of daughter progeny from germinating lysogens and pseudolysogens, or both. Phages producing turbid 103 plaques on the indicator strain (temperate) were repeatably more numerous than those producing clear plaques. This, and the fact that free phages are susceptible to unfavourable environmental changes, such as a drop in pH [37], whilst in an unprotected state outside the host, suggest that the lysogenic life-cycle is the more effective mode of survival in soil. Pseudolysogeny certainly ensures the survival of some virulent phages in natural environments, but the occurrence of true lysogeny in temperate phages appears to be a more stable evolutionary progression of this strategy. 10 M.S.D. (P<0.05): -E-I [] z 0 "0 o _J i The impact of phages on host populations 0 The most obvious impact phages can have on host populations is that of reducing population density by direct lysis. One-step growth experiments in flasks readily demonstrate the crash of a host population by lysis [3]. This destruction of a host population is rarely seen in natural environments, and probably only occurs in restricted areas of host growth such as inside soil aggregates. Observations of the epidemiology of Drosophila C virus (DCV) showed that susceptible fly populations were completely infected when one infected fly was added to laboratory vials [38]. Similar epidemics have never been reported for DCV in natural environments, and indeed no viral epidemic has been known to wipe out its host population on a global scale. This is probably a result of the combined effects of density dependent regulation and high mutational rate of virus and phage populations. Peaks in marine bacterial numbers during a spring bloom of diatoms in a Norwegian fjord were closely followed by peaks in virus numbers [18]. The peak in viral numbers was closely followed by a drop in bacterial numbers, and was subsequently followed by a drop in viral numbers, illustrating the predator-prey pattern of alternating, oscillating peaks of host and predator population numbers. It may be concluded that the marine bacteria in this ecosystem were regulated in part by the presence of viral populations, although other factors such as temperature and h I 0 I I I I I 5 I I I I I I I 10 I t 15 Time (days) Fig. 2. Survival of S. lividans TK24 in sterile soil in the presence of actinophage KC301 (2.0×105 p f u / g dry soil). Vegetative host growth (total viable count) between days 1 and 2 was retarded when the efficiency of infection was 1.4x 10 -5 (11), whereas no effect was seen at an efficiency of infection of 1.1 x 10 -6 (ID). Following sporulation, host populations reached a density of 5.0 x 107 cfu/g dry soil regardless of efficiency of infection (Marsh and Wellington, 1993. Unpublished data). nutrient status would also play a part in host population regulation. Little information is available concerning the effects of in situ lysis by phages in soil. The results of Pantastico-Caldas et al. [39] suggested that the presence of the virulent Bacillus subtilis phage, SP10C, in soil resulted in a decrease in the host population level by one order of magnitude. The lytic action of the temperate actinophage KC301 appeared to have no numerical impact on streptomycete populations in sterile and nonsterile soil [40-42]. Where the infection efficiency of KC301 was sufficiently high to retard vegetative growth of Streptomyces lividans in sterile soil, sporulation compensated for the reduction in propagule numbers (Fig. 2). Other impacts on host populations can be both adverse and beneficial. Many effects relate to the 104 states of lysogeny and transduction where the expression of phage-borne genes and maintenance of lysogeny burden the host cells. tions, whereby released lysozyme would attack bacteria sensitive to both the phage and lysozyme in a particular niche and provide additional resources to the lysogens in the form of liberated nutrients. The importance of lysogeny in nature Lysogenic infections can result in lysogenic conversion of the host where the expression of genes on the phage genome alter the host phenotype [43]. Superinfection immunity is the most common form of lysogenic conversion, whereby the expression of the phage-encoded repressor protein(s) inhibits further infections by the same phage type or different phages with specific binding sites for the repressor protein. Superinfection immunity in addition to changes in phage specificity can also be caused by prophage-encoded alterations to attachment sites on the cell surface, a feature seen in some lysogenic strains of E. coli and Salmonella species [7]. Lysogenic conversion can also confer pathogenicity, for example the prophage of lysogenic Corynebacterium diptheriae strains encodes the toxins enabling establishment of bacterial infection in hosts [7]. Engineered phages containing antibiotic and heavy metal resistance determinants [40,41,44-46] may be advantageous to lysogenic hosts in selective environments [42]. Conversely, the need to synthesise extra foreign DNA and express prophage genes exerts a burden on the host cell by utilising extra resources, and results in a metabolic burden on the host [32]. Therefore the lysogenic relationship between temperate phage and host can be seen as a situation of compromise on both parts. The host population is burdened by the presence of extra DNA and induction, whilst the rate of phage multiplication is restricted by the low level of prophage induction and the particular rate of host multiplication at a given time. In natural environments, the rates of prophage induction are usually very low [42,47] probably resulting in a negligible impact on host populations. This and the large amounts of lysozyme released at prophage induction [47] means that reversion to the lytic cycle by prophages constitutes a potential 'weapon' for lysogenic popula- The role of phages in genetic interactions Phage-mediated transfer of genetic elements (transduction) between bacterial cells [43] has been well documented, particularly with regard to the use of phages in molecular biology [2]. Transduction in natural environments may be a rare event, as generalised transduction has only been demonstrated once in freshwater ecosystems [48]. The potential for transduction in soil was assessed by adding coliphage transducing lysates to soil containing recipients which were subsequently transduced [44]. The general inactivity of soil microbial populations suggests that transduction in soil occurs at a low frequency, although this frequency may be comparable to those of conjugation and transformation in soil which also require recipients to be present in an active state. Lysogenic conversion as shown by lysogenic infections of inoculated hosts in soil by temperate phages containing genetic markers [40-42,45,46] is likely to be a far more frequent occurrence in soil in comparison to transduction. This is because all of the daughter progeny of a lysing cell will contain the genetic information to be expressed by the prophages of subsequent lysogenic infections. Hence genes on temperate phages which can be expressed by lysogenic hosts may be spread through soil by the movement of phage particles through soil water via channels in and between aggregates [49]. These genes will have a higher likelihood of surviving than genes on transducing particles. The potential for an engineered actinophage to establish itself in indigenous host populations in soil was assessed by Marsh and Wellington [41]. Lysates of KC301 (a derivative of ~bC31) carrying the thiostrepton resistance gene tsr were added to nonsterile soil. Thiostrepton resistant streptomycete spores were extracted from this soil and were found to contain KC301 DNA by 105 123456 5.7kb ..... 2.5kb Fig. 3. Southern blot of DNA from putative streptomycete lysogens isolated from soil inoculated with actinophage KC301. The KC301 junction fragment of S. lividans TK24 (KC301) and the indigenous lysogens can be seen at 5.7 kb (lane 3) and 2.5 kb (lanes 4, 5 and 6) resepectively. Lanes: 1, KC301; 2, S. lividans TK24; 3, S. lividans TK24 (KC301); 4, 5 and 6, indigenous lysogens (Marsh and Wellington, 1993. Unpublished data). colony blot analysis with radiolabelled KC301 DNA. Most of the putative lysogens were stable, and a sample of the stable lysogens proved to contain the KC301 prophage integrated into the indigenous host's chromosomes, as shown by Southern analysis of ClaI digested host DNA using nonradioactive DIG-labelled KC301 DNA (Fig. 3). Thus the release of an engineered phage such as KC301 into the environment where susceptible hosts were present could lead to the phage's persistence in natural habitats, particularly when the host concerned survives well in the soil. Conclusions Phages are abundant and widely distributed components of natural habitats, with several ef- fective survival strategies which ensure the persistence of phage DNA both inside and outside host cells. However, the lysogenic lifestyle is a distinct advantage in soil where long periods of host inactivity can be survived by residence within host populations. Phages may regulate host populations by lysis, but this regulation is probably extremely limited in discontinuously active ecosystems such as soil when host populations have periods of inactivity. Differentially growing hosts such as streptomycetes may escape the long-term deleterious effects of lytic attack by phages by only growing vegetatively for short periods of time, and existing as resistant spores for long periods of time. Lysogeny represents a compromise between hosts and phage where both parties are granted advantages in terms of improved survival capabilities in return for reduced abundance or multiplication potential. Phages are obviously active participants in genetic interactions between bacteria in nature, and therefore must contribute to evolutionary development of host populations. 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