Properties of a Novel Extracellular Cell-free Ice Nuclei from Ice-nucleating Pseudomonas antarctica IN-74

Some ice-nucleating bacterial strains, including Pantoea ananatis (Erwinia uredovora), Pseudomonas fluorescens, and Pseudomonas syringae isolates, were examined for the ability to shed ice nuclei into the growth medium. A novel ice-nucleating bacterium, Pseudomonas antarctica IN-74, was isolated from Ross Island, Antarctica. Cell-free ice nuclei from P. antarctica IN-74 were different from the conventional cell-free ice nuclei and showed a unique characterization. Cell-free ice nuclei were purified by centrifugation, filtration (0.45 μm), ultrafiltration, and gel filtration. In an ice-nucleating medium in 1 liter of cell culture, maximum growth was obtained with the production of 1.9 mg of cell-free ice nuclei. Ice nucleation activity in these cell-free ice nuclei preparations was extremely sensitive to pH. It was demonstrated that the components of cell-free ice nuclei were protein (33%), saccharide (12%), and lipid (55%), indicating that cell-free ice nuclei were lipoglycoproteins. Also, carbohydrate and lipid stains showed that cell-free ice nuclei contained both carbohydrate and lipid moieties.     

High-Level Expression of Ice Nuclei in Erwinia herbicola Is Induced by Phosphate Starvation and Low Temperature

In laboratory cultures of ice nucleation-active (Ice⁺) Erwinia herbicola isolates, it has been difficult to achieve high-level expression of ice nuclei, especially nuclei active at temperatures warmer than −5°C (i.e., type 1 ice nuclei). Here we demonstrate that starvation for phosphate and exposure to low temperature triggers expression of ice nuclei in E. herbicola cultures. Starvation for nitrogen, sulfur, or iron was less effective. Under optimal conditions with two different strains, essentially all cells produced ice nuclei active at −10°C or warmer, with an average of 22% containing type 1 ice nuclei within 1 h of a low-temperature shift. These conditions did not greatly enhance the shedding of ice nucleation-active membrane vesicles that are known to be produced by Ice⁺ E. herbicola isolates. These results support the theory that the Ice⁺ phenotype may allow nutrient-limited epiphytes to trigger freezing damage, releasing nutrients from host plants. Received: 2 November 1997 / Accepted: 5 January 1998     

Deletion mutagenesis of the ice nucleation gene from Pseudomonas syringae S203

Summary The ice nucleation gene inaZ, from Pseudomonas syringae S203, was manipulated to produce a series of defined rearrangements in its coding sequence without changing the reading frame. The effects of these mutations on the ice nucleation phenotype were determined in a heterologous host, Escherichia coli K12. Deletions which disrupted the periodicity of 16 codons, in a repetitive region of inaZ, caused the frequencies of ice nuclei in the bacterial population to be significantly depressed; the nuclei with thresholds at warmer temperatures were most affected. In contrast, when the periodicity was left intact, deletions and duplications in the same region had only slight effects on nucleation activity. Deletions removing part or all of one of the nonrepetitive regions (that encoding the amino-terminal domain of the InaZ protein) did not abolish nucleation activity, but caused it to be limited to cooler threshold temperatures. In contrast, the non-repetitive carboxy-terminal domain of the InaZ protein was shown to be essential for ice nucleation at all temperatures. The differential requirements (for periodicity, and for the amino-terminus) in forming nuclei with different thresholds may be significant for understanding what determines the threshold temperature of an ice nucleus.     

Co-production of ice nuclei and xanthan gum by transformed Xanthomonas campestris grown in sugar beet molasses

Two recombinant plasmids, expressing ice nucleation activity, were constructed and named pCPP30inaZ and pCPP38inaZ. They were transferred to the ice-negative, xanthan-producing Xanthomonas campestris pv. campestris by electroporation. The transformants were used for co-production of xanthan gum and ice nuclei from sugar beet molasses. The highest values obtained were 20 g l^–1 and 10¹⁸ ice nuclei ml^–1, respectively. The above values fulfil the criteria for industrial manipulation. This is the first report on co-formation of two products by a transformed X. campestris strain.     

冰核真菌胞外冰核产生条件、成冰生物学特性及其分离纯化的研究*

果糖和葡萄糖作碳源、硫酸铵作氮源、培养温度25℃以下、培养液初始pH5～7和少量通气都利于胞外冰核产生,最佳培养时间受培养温度和接种菌龄的制约,而低温处理、光照及添加丝裂霉素C和HNPA对胞外冰核产生无明显影响。胞外冰核耐热(40℃处理后仍保持较高活性),酸碱适应性强(pH2～13);温度50℃以上、蛋白酶K和高浓度脲处理可完全失活或严重破坏其冰核活性,表明蛋白是真菌胞外冰核的必需成分;胞外冰核溶液中盐浓度高于50mmol/L时,活性才受抑制。25%冰乙醇可有效沉淀真菌胞外冰核,同时又保持较高活性;分离纯化的初步研究显示真菌胞外冰核分子量很大,电荷组成和分布上不均一,所带净电荷为负。本研究加深了对真菌胞外冰核的认识,为进一步分离纯化奠定了基础。     

Ice crystallization by Pseudomonas syringae

Several bacterial species can serve as biological ice nuclei. The best characterized of these is Pseudomonas syringae, a widely distributed bacterial epiphyte of plants. These biological ice nuclei find various applications in different fields, but an optimized production method was required in order to obtain the highly active cells which may be exploited as ice nucleators. The results presented here show that P. syringae cells reduce supercooling of liquid or solid media and enhance ice crystal formation at sub-zero temperatures, thus leading to a remarkable control of the crystallization phenomenon and a potential for energy savings. Our discussion focuses on recent and future applications of these ice nucleators in freezing operations, spray-ice technology and biotechnological processes. Received: 21 December 1999 / Received revision: 29 February 2000 / Accepted: 6 March 2000     

Isolation and characterization of hydroxylamine-induced mutations in the Erwinia herbicola ice nucleation gene that selectively reduce warm temperature ice nucleation activity

Cells of ice nucleation active bacterial species catalyse ice formation over the temperature range of -2 to -12°C. Current models of ice nucleus structure associate the size of ice nucleation protein aggregates with the temperature at which they catalyse ice formation. To better define the structural features of ice nucleation proteins responsible for the functional heterogeneity of ice nuclei within a genetically homogeneous collection of cells we used in vitro chemical mutagenesis to isolate mutants with reduced ability to nucleate ice at warm assay temperatures but which retain normal or near normal nucleation activity at cold temperatures (WIND, i.e. w arm i ce n ucleus-d eficient mutants). Nearly half of the mutants obtained after hydroxylamine mutagenesis of the iceE gene from Erwinia herbicola had this phenotype. The phenotypes and location of lesions on the genetic map of iceE were determined for a number of mutants. All WIND mutations were restricted to the portion of iceE encoding the repetitive region of the poty peptide. DNA sequencing of two WIND mutants revealed single nucleotide substitutions changing a conserved serine or glycine residue to phenylalanine and serine, respectively. The implications of these findings in structure/function models for the ice nucleation protein are discussed.     

Cold requirement for maximal activity of the bacterial ice nucleation protein INAZ in transgenic plants

The bacterial ice nucleation gene inaZ confers production of ice nuclei when transferred into transgenic plants. Conditioning of the transformed plant tissue at temperatures near 0°C greatly increased the ice nucleation activity in plants, and maximum ice nucleation activity was achieved only after low-temperature conditioning for about 48 h. Although the transgenic plants contain similar amounts of inaZ mRNA at both normal and low temperatures, low temperatures are required for accumulation of INAZ protein. We propose that the stability of the INAZ protein and thus ice nucleation activity in the transgenic plants is enhanced by low-temperature conditioning.     

Freeze Concentration of Some Foodstuffs Using Ice Nucleation-active Bacterial Cells Entrapped in Calcium Alginate Gel

Cells of an ice nucleation-active strain of Ermnia ananas were entrapped in calcium alginate to prepare an ice-nucleating gel usable as ice nuclei for freeze concentration. The ice-nucleating gel was also adjusted as to specific gravity. When it was placed at a desired position in a liquid material such as egg white, ice formed at this position as the material was cooled. It was possible to put the ice- nucleating gel in liquid foodstuffs such as egg white and lemon juice before their temperatures reached subzero points. Application of this method produced freeze-concentrated foods whose properties were not significantly deteriorated.     

Development, distribution, and characteristics of intrinsic, nonbacterial ice nuclei in prunus wood

Ice nuclei active at approximately −2°C and intrinsic to woody tissues of Prunus spp. were shown to have properties distinct from bacterial ice nuclei. Soaking 5-centimeter peach stem sections in water for 4 hours lowered the mean ice nucleation temperature to below −4°C, nearly 2°C lower than stems inoculated with ice nucleation-active Pseudomonas syringae strain B301D. Ice nucleation activity in peach was fully restored by air-drying woody stem sections for a few hours. The ice nuclei in woody tissue were inactivated between 40 and 50°C, but unaffected by treatment with bacterial ice nucleation inhibitors (i.e. NaOCl, tartaric acid, Triton XQS-20), sulfhydryl reagents (i.e. p-hydroxymercuribenzoate and iodine) and Pronase. Ice nuclei could not be dislodged from stems by sonication and were shown to be equally distributed in peach bud and internodal stem tissue on a per unit mass basis; outer and inner stem tissues were also indistinguishable in ice nucleation activity. Development of ice nuclei in immature peach and sweet cherry stems did not occur until midsummer and their formation was essentially complete by late August. Once formed the ice nuclei intrinsic to woody stems were stable and unaffected by seasonal changes in growth. The apparent physiological function of the ice nuclei is discussed in relation to supercooling and mechanisms of cold hardiness in Prunus spp.     

Properties of a novel extracellular cell-free ice nuclei from ice-nucleating Pseudomonas antarctica IN-74

Some ice-nucleating bacterial strains, including Pantoea ananatis (Erwinia uredovora), Pseudomonas fluorescens, and Pseudomonas syringae isolates, were examined for the ability to shed ice nuclei into the growth medium. A novel ice-nucleating bacterium, Pseudomonas antarctica IN-74, was isolated from Ross Island, Antarctica. Cell-free ice nuclei from P. antarctica IN-74 were different from the conventional cell-free ice nuclei and showed a unique characterization. Cell-free ice nuclei were purified by centrifugation, filtration (0.45 microm), ultrafiltration, and gel filtration. In an ice-nucleating medium in 1 liter of cell culture, maximum growth was obtained with the production of 1.9 mg of cell-free ice nuclei. Ice nucleation activity in these cell-free ice nuclei preparations was extremely sensitive to pH. It was demonstrated that the components of cell-free ice nuclei were protein (33%), saccharide (12%), and lipid (55%), indicating that cell-free ice nuclei were lipoglycoproteins. Also, carbohydrate and lipid stains showed that cell-free ice nuclei contained both carbohydrate and lipid moieties.     

Ice Nucleation Activity in Fusarium acuminatum and Fusarium avenaceum

Twenty fungal genera, including 14 Fusarium species, were examined for ice nucleation activity at −5.0°C, and this activity was found only in Fusarium acuminatum and Fusarium avenaceum. This characteristic is unique to these two species. Ice nucleation activity of F. avenaceum was compared with ice nucleation activity of a Pseudomonas sp. strain. Cumulative nucleus spectra are similar for both microorganisms, while the maximum temperatures of ice nucleation were −2.5°C for F. avenaceum and −1.0°C for the bacteria. Ice nucleation activity of F. avenaceum was stable at pH levels from 1 to 13 and tolerated temperature treatments up to 60°C, suggesting that these ice nuclei are more similar to lichen ice nuclei than to bacterial ones. Ice nuclei of F. avenaceum, unlike bacterial ice nuclei, pass through a 0.22-μm-pore-size filter. Fusarial nuclei share some characteristics with the so-called leaf-derived nuclei with which they might be identified: they are cell free and stable up to 60°C, and they are found in the same kinds of environment. Highly stable ice nuclei produced by fast-growing microorganisms have potential applications in biotechnology. This is the first report of ice nucleation activity in free-living fungi.     

Toxicity of Smoke to Epiphytic Ice Nucleation-Active Bacteria

Wheat straw smoke aerosols and liquid smoke condensates reduced significantly both the viability and the ice-nucleating activity of Pseudomonas syringae pv. syringae and Erwinia herbicola in vitro and on leaf surfaces in vivo. Highly significant reductions in numbers of bacterial ice nuclei on the surface of both corn and almond were observed after exposure to smoke aerosols. At −5°C, frost injury to corn seedlings colonized by ice nucleation-active bacteria was reduced after exposure to smoke aerosols. Effects on −9°C ice nuclei, although significant, were less than on ice nuclei active at −5°C. These results suggest that smoke from wildfires or smudge pots may reduce plant frost susceptibility and sources of ice nuclei important in other natural processes under some conditions.     

Release of cell-free ice nuclei from Halomonas elongata expressing the ice nucleation gene inaZ of Pseudomonas syringae

Release of ice nuclei in the growth medium of recombinant Halomonas elongata cells expressing the inaZ gene of Pseudomonas syringae was studied in an attempt to produce cell-free active ice nuclei for biotechnological applications. Cell-free ice nuclei were not retained by cellulose acetate filters of 0.2 microm pore size. Highest activity of cell-free ice nuclei was obtained when cells were grown in low salinity (0.5-5% NaCl, w/v). Freezing temperature threshold, estimated to be below -7 degrees C indicating class C nuclei, was not affected by medium salinity. Their density, as estimated by Percoll density centrifugation, was 1.018 +/- 0.002 gml(-1) and they were found to be free of lipids. Ice nuclei are released in the growth medium of recombinant H. elongata cells probably because of inefficient anchoring of the ice-nucleation protein aggregates in the outer membrane. The ice+ recombinant H. elongata cells could be useful for future use as a source of active cell-free ice nucleation protein.     

High-level expression of ice nuclei in a Pseudomonas syringae strain is induced by nutrient limitation and low temperature.

Attempts were made to maximize the expression of ice nuclei in Pseudomonas syringae T1 isolated from a tomato leaf. Nutritional starvation for nitrogen, phosphorous, sulfur, or iron but not carbon at 32 degrees C, coupled to a shift to 14 to 18 degrees C, led to the rapid induction of type 1 ice nuclei (i.e., ice nuclei active at temperatures warmer than -5 degrees C). Induction was most pronounced in stationary-phase cells that were grown with sorbitol as the carbon source and cooled rapidly, and under optimal conditions, the expression of type 1 ice nuclei increased from < 1 per 10(7) cells (i.e., not detectable) to 1 in every cell in 2 to 3 h. The induction was blocked by protein and RNA synthesis inhibitors, indicative of new gene expression. Pulse-labeling of nongrowing cultures with [35S]methionine after a shift to a low temperature demonstrated that the synthesis of a new set of "low-temperature" proteins was induced. Induced ice nuclei were stable at a low temperature, with no loss in activity at 4 degrees C after 8 days, but after a shift back to 32 degrees C, type 1 ice nuclei completely disappeared, with a half-life of approximately 1 h. Repeated cycles of low-temperature induction and high-temperature turnover of these ice nuclei could be demonstrated with the same nongrowing cells. Not all P. syringae strains from tomato or other plants were fully induced under the same culture conditions as strain T1, but all showed increased expression of type 1 ice nuclei after the shift to the low temperature. In support of this view, analysis of the published DNA sequence preceding the translational start site of the inaZ gene (R. L. Green and G. Warren, Nature [London] 317:645-648, 1985) suggests the presence of a gearbox-type promoter (M. Vincente, S. R. Kushner, T. Garrido, and M. Aldea, Mol. Microbiol. 5:2085-2091, 1991).     

Ice-nucleation on kiwifruit

Ice-nucleating capability of the kiwifruit vine, Actinidia deliciosa, was examined. Pseudomonas viridiflava, present as an epiphyte on the vine, was an effective icenucleating agent. The presence of other sources of ice nuclei on the surface of the vines, leaves and fruit, which could not be inhibited by anti-bacterial agents, was also demonstrated.     

Characterization of biological ice nuclei from a lichen.

Biological ice nuclei (active at approximately -4 degrees C) were extracted from cells of the lichen Rhizoplaca chrysoleuca by sonication. Sensitivity to proteases, guanidine hydrochloride, and urea showed these nuclei to be proteinaceous. The nuclei were relatively heat stable, active from pH 1.5 to 12, and active without lipids, thereby demonstrating significant differences from bacterial ice nuclei.     

Rates of assembly and degradation of bacterial ice nuclei

The kinetics of ice-nucleus assembly from newly synthesized nucleation protein were observed following induction of nucleation gene expression in the heterologous host Escherichia coli. Assembly was significantly slower for the small proportion of ice nuclei active above -4.4 degrees C; this was consistent with the belief that these nuclei comprise the largest aggregates of nucleation protein. The kinetics of nucleus degradation were followed after inhibiting protein synthesis. Nucleation activity and protein showed a concerted decay, indicating that most of the functional ice nuclei are in equilibrium with a single cellular pool of nucleation protein. A minority of the ice nuclei decayed much more slowly than the majority; presumably their nucleation protein was distinct either by virtue of different structure or different subcellular compartmentalization, or because of its presence in a metabolically distinct subpopulation of cells.     

Release of cell-free ice nuclei by Erwinia herbicola.

Several ice-nucleating bacterial strains, including Erwinia herbicola, Pseudomonas fluorescens, and Pseudomonas syringae isolates, were examined for their ability to shed ice nuclei into the growth medium. Only E. herbicola isolates shed cell-free ice nuclei active at -2 to -10 degrees C. These cell-free nuclei exhibited a freezing spectrum similar to that of ice nuclei found on whole cells, both above and below -5 degrees C. Partially purified cell-free nuclei were examined by density gradient centrifugation, chemical and enzymatic probes, and electron microscopy. Ice-nucleating activity in these cell-free preparations was associated with outer membrane vesicles shed by cells and was sensitive to protein-modifying reagents.     

Use of two-step cooling procedures to examine factors influencing cell survival following freezing and thawing

The two-step cooling procedure has been used to investigate factors involved in cell injury. Chinese hamster fibroblasts frozen in dimethylsulphoxide (5%, $\text{v}\text{v}$) were studied. Survival was measured using a cell colony assay and simultaneous observations of cellular shrinkage and the localization of intracellular ice were done by an ultrastructural examination of freeze-substituted samples.Correlations were obtained between survival and shrinkage at the holding temperature. However, cells shrunken at ?25 °C for 10 min (the optimal conditions for survival on rapid thawing from ?196 °C) contain intracellular ice nuclei at ?196 °C detectable by recrystallization. These ice nuclei only form below ?80 °C and prevent recovery on slow or interrupted thawing but not on rapid thawing. Cells shrunken at ?35 °C for 10 min (just above the temperature at which intracellular ice forms in the majority of rapidly cooled cells) can tolerate even slow thawing from ?196 °C, suggesting that they contain very few or no ice nuclei even in liquid nitrogen. Damage may correlate with the total amount of ice formed per cell rather than the size of individual crystals, and we suggest that injury occurs during rewarming and is osmotic in nature.