Bacterial nucleation in pseudomonas syringae

Pseudomonas syringae

Species

As a Gram-negative, rod-shaped, obligate aerobic bacterium, Pseudomonas syringae is one of 78 species that has been described in the Pseudomonas genus (1). Characterized as an epiphyte, it grows supported non-parasitically by plants where it derives its nutrients and water from floating dust, rain, etc (9). This species can be found on tomatoes and beans to rice and tobacco, and is responsible for more surface frost damage to plants than any other mineral or organism (4). Its affiliation as a plant pathogen which causes disease in a large variety of plants makes this particular bacterium important in the field of food and biomass production, and is an important focus for the Department of Energy (2). P. syringae is a very stress-tolerant organism, and is the focus of many studies of stress-tolerant gene expression. Kurz et al., (2010) used biochemical approaches to address water stress tolerance in P. syringae (3). They showed that different osmolytes differentially contribute to water stress tolerance and interact at the level of transcription.

Different species of these flagellated, motile bacteria infect leaves and tissues of a wide range of hosts, but can be specific to a particular location of an individual. For example, Pseudomonas syringae pv. aesculi is able to infect vascular tissue to cause cankers in European horse chestnut in northwest Europe, but does not infect leaves, buds, or flowers on the same individual (Picture 2) (5). Some have also identified genes which are only expressed when the bacterium is on plants, which represent a ‘hidden genome’ not very well studied due to the absence in culture (2). Although there is variation with each pathovar, this bacterium grows optimally in cool, wet conditions from 15-25°C. It is proposed by Hirano et al. (1987) that momentum from falling raindrops is responsible for initiation of rapid growth and the forming of massive colonies on host surfaces (6). This has been seen as a method of how these bacterial cells are able to spread infection. This can also however, prevent infection by washing off bacterial cells from yet-infected surfaces.

[Image 1]
Pseudomonas syringae shown using SEM. Source: Gordon Vrdoljak, Electron Microscopy Laboratory, U.C. Berkeley [1]

[Image 2]
Infection of European horse chestnut (Aesculus hippocastanum) with leasions caused by Pseudomonas syringae pv. aesculi. Source: Steele et al. 2010.

Importance

This particular species of Pseudomonas has been the subject of a large array of studies over the past 35 years with its involvement in crop freezing. The majority of frost-sensitive plants usually suffer from damage between -2 and -5°C (10, 11). When water gets this cold, water turns into ice in both inter- and intracellular ways, causing frost damage. P. syringae express a particular type of surface protein, ice-nucleation protein (INP), which increases temperatures to which water is able to freeze. In the absence of sites capable of ice nucleation, the cold water can supercool and freezing will not occur until the temperature is low enough for the most active ice nucleus available is able to catalyze crystallization of supercooled water (freezing)(12). Thus, supercooling instead of ice-nucleation could be a mechanism of frost protection.

P. syringae is a species of bacteria very important to present-day society, particularly with the ever-increasing population of planet earth. Chronic hunger affects 820 million people worldwide, killing 25,000 people every day, one child every eight seconds (13). Large quantities of crops are lost every year are lost due to frost such as in the state of Florida, where 40% of the world’s orange juice supply is grown (14). A large area of interest with Pseudomonas syringae focuses on genetically engineering these bacteria with ice-nucleation-minus proteins. Without these proteins it is thought the temperatures tolerable by plants may be decreased.

Ice Nucleation Active (INA) Proteins

Description

All proteins interact with water, but there are two classes in particular which have a function relating to ice: antifreeze proteins (AFPs) and ice-nucleation proteins (INPs). AFPs have particular structures known to inhibit formation of ice crystals, while INPs do just the opposite. INPs can be seen affiliated with the production of artificial snow (6). Pure water can be supercooled to -40°C in the absence of a heteronucleus (7). INPs are able to promote ice formation by raising the nucleation temperature, and in vitro this temperature can range from -14 to -2°C depending on the number of proteins that cluster together.

Structure

Graether and Jia (2001) attempted to present a model of INP from Pseudomonas syringae based on comparison with two newly determined insect AFP structures. They analyzed the INP sequence of ~60 16-residue repeats similar to a different model organism, and proposed a 16-residue loop for P. syringae (Picture 3). Their result suggested that insect AFPs and bacterial INPs may have a similar B-helical structure, even though they have opposite effects on water molecules.

[Image 3]
Pseudomonas syringae Cross section of modeled INP and a B-helical protein showing a wire frame representation of one loop. Cross section after 100 steps of energy minimization. Source: Graether and Jia, (2001).

Bacterial Effects

Beginning more than 25 years ago, scientists began noticing that concentrations of bacteria residing on leaf surfaces were correlated with the temperatures at which freezing occurred in plant tissues. A study by Lindow et al., (1982) concluded that higher concentrations of P. syringae on leaf surfaces were associated with warmer temperatures of freezing (Figure 1). They also showed that freezing temperatures were much lower without the presence of the bacteria (Figure 2). These results led researchers to conclude that bacteria on the surfaces of leaves play a major role in plant freezing.

[Figure 1]
Proportions of frozen droplets with respect to temperature at Pseudomonas syringae concentrations of 10⁷, 10⁶, 10⁵, 3.5⁴, and 3.5³. Cells were grown on nutrient agar and suspended in sterile water at appropriate concentrations. Source: Lindow et al., 1982.

[Figure 2]
Ice nucleation activity of corn leaf disks from plants with and without leaf surface populations of Pseudomonas syringae. Plants were sprayed with suspensions of 2 x 10⁸ cells/ml. Source: Lindow et al., 1982.

Current Research

Clouds

The use of ice-nucleating bacteria has already been seen in uses for creating fake snow to protection of crops from frost during growing seasons. On a larger scale, IN bacteria has begun to be studied in the atmosphere. Mohler, et al. (2008) conducted a study investigating five different bacterial species in the range of -5 to -15^oC and their correlations to condensation. Pseudomonas syringae resides on plant surfaces, where it is emitted into the atmosphere (17). Ice nucleation active strains have been detected in rain and snow, as well as in the atmosphere (18, 19), and suggests that they may be disseminated through the water cycle. Bacterial ice nucleation is an important area of study in the initiation of precipitation, and with particular species nucleation can occur at a range of temperatures. In this study, bacterial cells were suspended in the aerosol phase using the Aerosol Interaction and Dynamics in the Atmosphere facility in Germany. Growing water droplets and ice particles were sensitively detected using in situ light scattering and depolarization setup SIMONE, which measures the depolarization of polarized light at a particular wavelength scattered from particles in the center of the large, cold cloud chamber. Infrared extinction spectrometers were also used to characterize droplet and ice clouds. As a result, the IN active cell fraction was calculated from the ratio of ice particle number concentration to number of total cells. The bacteria investigated are mainly IN active between -7 and -11^oC with an IN active fraction of the order of 10^-4. This means that in similar conditions to what is present in the atmosphere, IN active bacteria are able to form ice crystals. From this data, future studies should test at what concentrations of IN active bacterial cells the initiation of precipitation occurs through the ice phase. More studies are needed to measure distribution, sources, and bacterial cell concentration in the troposphere, as well as characterization of IN active cells extracted from cloud and rain water.

Foods

There have also been studies using ice-nucleating bacteria commercially. In some uses, bacterial ice nucleation at higher temperatures may be useful in keeping foods frozen. For example, it was found that the nucleation temperature of salmon muscle with the use of ice-nucleation active (INA) Pseudomonas syringae was raised from -4.9 to -1.5^oC (21). This means that the difference between the freezing-point temperature and the nucleation temperature of the sample was reduced by 3.4^oC (Table XXXX). Li et al. (1997) tests freezing effects in multiple foods in response to concentrations of bacterial ice nucleators. The addition of P. syringae cells to egg white solutions resulted in a significant increase in their nucleation temperatures at -6^oC (Table XXXXXX). In solution containing 9% egg white solution freezing occurred at -5.1^oC without INA bacteria, but was raised to -0.6^oC in the presence of INA Pseudomonas syringae cells. At 20% egg white solution, the control did not freeze at -6^oC, but the INA samples had frozen easily. This means that the behavior of the egg white solution was determined by the presence or absence of INA bacteria. It may be impractical to supplement large quantities of bacteria into everyday foods, but their effects on the freezing model of food systems may provide information for future studies of microbes in the food industry.

[Figure 2]
Hypothetical freezing curve of water. Degree of supercooling is defined as the temperature difference between freezing point (A) and nucleation point (B). The total freezing time is the time difference between when the temperature of water passes the freezing point (a), and when it reaches the freezer temperature (b). Source: Li et al., 1997.

[Figure 2]
Nucleation temperatures (^oC) of egg white solutions in the absence and presence of INA cells ^a. Source: Li et al., 1997.

Conclusion

Although most go unnoticed, the presence of ice-nucleating bacteria is important for everyday life from agriculture to making snow. In particular, Pseudomonas syringae have been an epiphyte of great interest for nearly three decades. Its ice nucleating proteins protruding from the membrane are important to structural properties of molecule organization. The process of nucleation can be catalyzed by these specific IN proteins, or inhibited by a mutation in these proteins. The addition of ice-nucleating bacteria to agriculture has potential benefits of protecting crops from frosts dropping below freezing, which might contribute to a solution of the world-wide problem of starvation and chronic hunger. These bacterial mechanisms might also someday be used to keep food frozen leading to conservation of energy or other benefits. The role of INA bacteria is also predicted to influence cloud formation. Future studies could uncover even more answers for most people who don’t realize how dependent they really are on these bacteria.  

References

[1] http://genome.jgi-psf.org/psesy/psesy.home.html [2]

[2] Steele, H., B.E. Laue, G.A. MacAskill, A.J. Hendry, and S. Green. “Analysis of the natural infection of European horse chestnut (Aesculus hippocastanum) by Pseudomonas syringae pv. Aesculi.” Plant Pathology 59: 1005-1013.

[3] Graether, S.P., and Z. Jia. 2001. Modeling Pseudomonas syringae ice-nucleation protein as a B-helical protein. Biophysical Journal 80: 1169-1173.

[4] Lindow, S.E., D.C. Arny, and C.D. Upper. 1982. Bacterial ice nucleation: a factor in frost injury to plants. Plant Physiology 70: 1084-1089.

Edited by Ryan O'Connor,student of Joan Slonczewski for BIOL 238 Microbiology, 2011, Kenyon College.