Characterization and Quantification of Intrinsic Ice Nucleators in Winter Rye (Secale cereale) Leaves

Extracellular ice formation in frost-tolerant organisms is often initiated at specific sites by ice nucleators. In this study, we examined ice nucleation activity (INA) in the frost-tolerant plant winter rye (Secale cereale). Plants were grown at 20[deg]C, at 5[deg]C with a long day, and at 5[deg]C with a short day (5[deg]C-SD). The threshold temperature for INA was -5 to -12[deg]C in winter rye leaves from all three growth treatments. Epiphytic ice nucleation-active bacteria could not account for INA observed in the leaves. Therefore, the INA must have been produced endogenously. Intrinsic rye ice nucleators were quantified and characterized using single mesophyll cell suspensions obtained by pectolytic degradation of the leaves. The most active ice nucleators in mesophyll cell suspensions exhibited a threshold ice nucleation temperature of -7[deg]C and occurred infrequently at the rate of one nucleator per 105 cells. Rye cells were treated with chemicals and enzymes to characterize the ice nucleators, which proved to be complexes of proteins, carbohydrates, and phospholipids, in which both disulfide bonds and free sulfhydryl groups were important for activity. Carbohydrates and phospholipids were important components of ice nucleators derived from 20[deg]C leaves, whereas the protein component was more important in 5[deg]C-SD leaves. This difference in composition or structure of the ice nucleators, combined with a tendency for more frequent INA, suggests that more ice nucleators are produced in 5[deg]C-SD leaves. These additional ice nucleators may be a component of the mechanism for freezing tolerance observed in winter rye.     

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.     

Ultrastructure before freezing,while frozen,and after thawing in assessing cryoinjury of mouse epididymal spermatozoa

Tails of mouse epididymides were treated as follows: control, unfrozen with and without cryoprotective agents (CPA); frozen (to below ?80 °C), slowly (8 °C/min), and rapidly (18 °C/sec), with and without CPA. Intracellular and/or extracellular location of CPA, at least glycerol, was influenced, respectively, by high (22 °C) or low (0 °C) exposure temperature. Standard procedures in electron microscopy were employed and the frozen state preserved by freeze-substitution. Motility before freezing and after thawing was the criterion of cryosurvival.Results showed no evidence of deleterious ultrastructural effects of freezing at rates compared, or of benefits of CPA, regardless of their cellular location. Differences were noted, however, in the appearance of spermatozoa in the frozen state, as a function of the rate of freezing but not as a function of the presence, absence, or location of either glycerol of DMSO. Rapidly frozen cells showed intracellular ice formation in the acrosome, neck, midpiece, and tail regions; there was no intranuclear ice, and extracellular ice artifacts were small. Slowly frozen cells showed large extracellular ice artifacts with evidence of shrinkage distortion due to the dehydration induced by extracellular ice. No spermatozoa survived any of the freezing treatments, showing the lethal effect of both extracellular ice during slow freezing and of intracellular and/or extracellular ice during rapid freezing.     

Low-temperature conditioning of the ice nucleation active bacterium,Erwinia herbicola

Rapid “low-temperature conditioning” and “solute conditioning” of the ice nucleation active bacterium Erwinia herbicola No. 26 are described. Conditioning is the process by which the ability to initiate ice at high temperatures is gained in these bacteria. The cumulative ice nucleator concentration, N[T], was used to measure the number of ice nucleators present in the bacterial systems. N[T] was determined at temperatures from −2 ° to −10 °C and was measured under varying conditioning temperature, time, and solute regimes. Values of N[T] increased rapidly on cooling samples from 30 to 5 °C. The optimum low temperature for conditioning was 5 °C. The conditioning process followed first-order reaction kinetics and time constants (1/rate constant) were between 43 and 62 min at 5 °C. Individual ice nucleators were isolated in droplets and were stable for at least 2 hr. Low-temperature conditioning did not occur when protein synthesis was inhibited by eliminating amino acids in the low-temperature conditioning media or by using the protein synthesis inhibitors chloramphenicol and streptomycin. Analysis of low-temperature conditioning, using heterogeneous ice nucleation theory predicted that ice nucleators are large and have diameters ranging from 80 Å (active at −8 °C) to 300 Å (active at −3 °C). In conclusion, it was predicted that conditioning resulted from growth of the nucleator from about 80 to 300 Å, from a change in the surface properties of 300 Å nucleator making it more similar to ice, or from a combination of these.     

Microbial life beneath a high arctic glacier

The debris-rich basal ice layers of a high Arctic glacier were shown to contain metabolically diverse microbes that could be cultured oligotrophically at low temperatures (0.3 to 4 degrees C). These organisms included aerobic chemoheterotrophs and anaerobic nitrate reducers, sulfate reducers, and methanogens. Colonies purified from subglacial samples at 4 degrees C appeared to be predominantly psychrophilic. Aerobic chemoheterotrophs were metabolically active in unfrozen basal sediments when they were cultured at 0.3 degrees C in the dark (to simulate nearly in situ conditions), producing (14)CO(2) from radiolabeled sodium acetate with minimal organic amendment (> or =38 microM C). In contrast, no activity was observed when samples were cultured at subfreezing temperatures (< or =-1.8 degrees C) for 66 days. Electron microscopy of thawed basal ice samples revealed various cell morphologies, including dividing cells. This suggests that the subglacial environment beneath a polythermal glacier provides a viable habitat for life and that microbes may be widespread where the basal ice is temperate and water is present at the base of the glacier and where organic carbon from glacially overridden soils is present. Our observations raise the possibility that in situ microbial production of CO(2) and CH(4) beneath ice masses (e.g., the Northern Hemisphere ice sheets) is an important factor in carbon cycling during glacial periods. Moreover, this terrestrial environment may provide a model for viable habitats for life on Mars, since similar conditions may exist or may have existed in the basal sediments beneath the Martian north polar ice cap.     

Ultrastructural appearance of freeze-substituted schistosomula of Schistosoma mansoni frozen by a two-step cooling schedule

Schistosomula of the parasitic helminth Schistosoma mansoni were frozen by two-step cooling, then examined for ultrastructural changes by the freeze-substitution method. Samples were cooled at 1 °C min^?1 to ?20, ?25, ?28, and ?38 °C before being cooled at 10,000 °C min^?1 to ?196 °C. The results showed that progressive partial dehydration of the parasites occurred during slow cooling. Numerous cavities, indicating the presence of intracellular ice crystals, were observed in organisms which did not become shrunken. The sizes of the ice cavities varied between organisms and also within the same cell type in individual organisms indicating that intracellular ice nucleation may occur at any time during the slow cooling step. Some organisms cooled first to ?28 or ?38 °C contained no evidence of ice crystal formation. When correlated with previously reported infectivity studies, the results indicated that successful cryopreservation of schistosomula requires slow cooling to approximately ?30 °C to induce cryodehydration, followed by rapid cooling to ?196 °C to prevent ice nucleation or crystal growth.     

Protective effect of intracellular ice during freezing?

Injury results during freezing when cells are exposed to increasing concentrations of solutes or by the formation of intracellular ice. Methods to protect cells from the damaging effects of freezing have focused on the addition of cryoprotective chemicals and the determination of optimal cooling rates. Based on other studies of innocuous intracellular ice formation, this study investigates the potential for this ice to protect cells from injury during subsequent slow cooling. V-79W Chinese hamster fibroblasts and Madin-Darby Canine Kidney (MDCK) cells were cultured as single attached cells or confluent monolayers. The incidence of intracellular ice formation (IIF) in the cultures at the start of cooling was pre-determined using one of two different extracellular ice nucleation temperatures (-5 or -10 degrees C). Samples were then cooled at 1 degrees C/min to the experimental temperature (-5 to -40 degrees C) where samples were warmed rapidly and cell survival assessed using membrane integrity and metabolic activity. For single attached cells, the lower ice nucleation temperature, corresponding to increased incidence of IIF, resulted in decreased post-thaw cell recovery. In contrast, confluent monolayers in which IIF has been shown to be innocuous, show higher survival after cooling to temperatures as low as -40 degrees C, supporting the concept that intracellular ice confers cryoprotection by preventing cell dehydration during subsequent slow cooling.     

Modelled and measured dynamics of viruses in Arctic winter sea-ice brines

We describe a model based on diffusion theory and the temperature-dependent mechanism of brine concentration in sea ice to argue that, if viruses partition with bacteria into sea-ice brine inclusions, contact rates between the two can be higher in winter sea ice than in seawater, increasing the probability of infection and possible virus production. To examine this hypothesis, we determined viral and bacterial concentrations in select winter sea-ice horizons using epifluorescence microscopy. Viral concentrations ranged from 1.6 to 82 x 10(6) ml(-1) of brine volume of the ice, with highest values in brines from coldest (-24 to -31 degrees C) ice horizons. Calculated virus-bacteria contact rates in underlying -1 degrees C seawater were similar to those in brines of -11 degrees C ice but up to 600 times lower than those in ice brines at or below -24 degrees C. We then incubated native bacterial and viral assemblages from winter sea ice for 8 days in brine at a temperature (-12 degrees C) and salinity ( approximately 160 psu) near expected in situ values, monitoring their concentrations microscopically. While different cores yielded different results, consistent with known spatial heterogeneity in sea ice, these experiments provided unambiguous evidence for viral persistence and production, as well as for bacterial growth, in -12 degrees C brine.     

Freeze-dried plasma proteins are stable at room temperature for at least 1 year

Thirty human EDTA plasma samples from male and female subjects ranging in age from 24 to 74 years were collected on ice, processed ice cold and stored frozen at ?80 °C, in liquid nitrogen (LN2), or freeze dried and stored at room temperature in a desiccator (FDRT) or freeze dried and stored at ?20 °C for 1 year (FD-20). In a separate experiment, EDTA plasma samples were collected onto ice, processed ice cold and maintained on ice ± protease inhibitors versus incubated at room temperature for up to 96 h. Random and independent sampling by liquid chromatography and tandem mass spectrometry (LC–ESI–MS/MS), as correlated by the MASCOT, OMSSA, X!TANDEM and SEQUEST algorithms, showed that tryptic peptides from complement component 4B (C4B) were rapidly released in plasma at room temperature. Random sampling by LC–ESI–MS/MS showed that peptides from C4B were undetectable on ice, but peptides were cleaved from the mature C4B protein including NGFKSHALQLNNR within as little as 1 h at room temperature. The frequency and intensity of precursors within ± 3 m/z of the C4B peptide NGFKSHALQLNNR was confirmed by automated targeted analysis where the precursors from MS/MS spectra that correlated to the target sequence were analyzed in SQL/R. The C4B preproprotein was processed at the N terminus to release the mature chain that was cleaved on the carboxyl side of the isoprene C2 domain within a polar C terminal sequence of the mature C4B protein, to reveal the thioester reaction site, consistent with LC–ESI–MS/MS and Western blot. Random sampling showed that proteolytic peptides from complement component C4B were rarely observed with long term storage at ? 80 °C in a freezer or in liquid nitrogen (LN2), freeze drying with storage at ? 20 °C (FD-20 °C) or freeze drying and storage at room temperature (FDRT). Plasma samples maintained at room temperature (RT) showed at least 10-fold to 100-fold greater frequency of peptide correlation to C4B and measured peptide intensity compared to samples on ice for up to 72 h or stored at ? 80 °C, LN2, FDRT or FD-20 °C for up to a year.     

Extracellular ice and cell shape in frost-stressed cereal leaves: A low-temperature scanning-electron-microscopy study

Low-temperature scanning electron microscopy was used to examine transverse fracture faces through cereal leaf pieces subjected to frost. Specimens were studied before and after sublimation of the ice. The position of extracellular ice in the leaf was inferred from the difference between the specimen before and after sublimation and from ridges and points which occurred in the extracellular ice during sublimation. Steps in the fracture surface indicated that the fracture plane passed through the extracellular ice crystals as well as through cells and also helped identify extracellular ice. The cells in controls were turgid and extracellular ice was absent. Leaf pieces from hardened rye were excised and frost-stressed to-3.3°,-21° and-72°C, cooling at 2–12°·h^-1. Cell collapse and extracellular ice were evident at-3.3°C and increased considerably by-21° C. At-21° and-72°C the leaf pieces were mainly filled with extracellular ice and there were few remaining gas spaces. The epidermal and mesophyll cells were laterally flattened, perpendicular to their attachment to adjacent cells, and phloem and vascular sheath cells were more irregularly deformed. Leaf pieces from tender barley were cooled at 2°C·min^-1 to-20° C; they were then mainly filled with extracellular ice, and the cells were highly collapsed as in the rye. In rye leaves frozen to-3.6° C before excision, ice crystals occurred in peri-vascular, sub-epidermal and intervening mesophyll spaces. In rye leaf pieces frozen to-3.3° C after excision or to-3.6° C before excision, mesophyll cells were partly collapsed even when not covered by ice, indicating that collapse of the cell wall, as well as the enclosed protoplast, was driven by dehydration. No gas or ice-filled spaces were found between wall and the enclosed protoplast. It is suggested that this can be explained without invoking chemical bonding between cell wall and plasma membrane: when the wall pores are filled by water, the pore size would reduce vapour pressure so making penetration of the wall by ice or gas less likely.Abbreviations SEM scanning electron microscopy     

Calorimetric studies of freeze-induced dehydration of phospholipids.

Differential scanning calorimetry (DSC) was used to determine the amount of water that freezes in an aqueous suspension of multilamellar dipalmitoylphosphatidylcholine (DPPC) liposomes. The studies were performed with dehydrated suspensions (12-20 wt% water) and suspensions containing an excess of water (30-70 wt% water). For suspensions that contained > or = 18 wt% water, two ice-formation events were observed during cooling. The first was attributed to heterogeneous nucleation of extraliposomal ice; the second was attributed to homogeneous nucleation of ice within the liposomes. In suspensions with an initial water concentration between 13 and 16 wt%, ice formation occurred only after homogeneous nucleation at temperatures below -40 degrees C. In suspensions containing < 13 wt% water, ice formation during cooling was undetectable by DSC, however, an endotherm resulting from ice melting during warming was observed in suspensions containing > or = 12 wt% water. In suspensions containing < 12 wt% water, an endotherm corresponding to the melting of ice was not observed during warming. The amount of ice that formed in the suspensions was determined by using an improved procedure to calculate the partial area of the endotherm resulting from the melting of ice during warming. The results show that a substantial proportion of water associated with the polar headgroup of phosphatidylcholine can be removed by freeze-induced dehydration, but the amount of ice depends on the thermal history of the samples. For example, after cooling to -100 degrees C at rates > or = 10 degrees C/min, a portion of water in the suspension remains supercooled because of a decrease in the diffusion rate of water with decreasing temperature. A portion of this supercooled water can be frozen during subsequent freeze-induced dehydration of the liposomes under isothermal conditions at subfreezing storage temperature Ts. During isothermal storage at Ts > or = -40 degrees C, the amount of unfrozen water decreased with decreasing Ts and increasing time of storage. After 30 min of storage at Ts = -40 degrees C and subsequent cooling to -100 degrees C, the amount of water associated with the polar headgroups was < 0.1 g/g of DPPC. At temperatures > -50 degrees C, the amount of unfrozen water associated with the polar headgroups of DPPC decreased with decreasing temperature in a manner predicted from the desorption isotherm of DPPC. However, at lower temperatures, the amount of unfrozen water remained constant, in large part, because the unfrozen water underwent a liquid-to-glass transformation at a temperature between -50 degrees and -140 degrees C.     

Changes in cell size during the cooling, warming and post-thawing periods of the freeze-thaw cycle.

Chinese Hamster Ovary (CHO) cells were cooled at 1 and 200 °C/min and subsequently thawed, while being studied with a cryomicroscope. Post-thaw size changes were measured with a Quantimet 720 Image Analysing Computer. It was found that the behavior of individuals in a population varied and depended on cooling rate. Cooling at 1 °C/min resulted in cells showing no intracellular ice, whereas cooling at 200 °C/min caused intracellular ice formation in some cells but not in others. In addition, at the slow rate, during cooling, the cells shrank significantly but swelled on thawing to become larger than non-frozen controls. Following swelling, as their temperature rose, the cells shrank to the size of non-frozen controls. At the fast rate, cells showed variation in their amount of intracellular ice and in their degree of shrinkage. Cells containing most ice shrank least. On warming, cells with intracellular ice began to swell at a lower temperature than did those cells without intracellular ice, while after thawing they swelled to a greater extent partly due to widespread blebbing. Corresponding recovery indices were measured, and correlation of these with the above effects suggests that: (i) cells completely filled with intracellular ice are non-viable; (ii) cells partially filled with intracellular ice respond to, or can be rescued by, first warming; (iii) cells without intracellular ice are viable; (iv) viable cells are those which regain their original size following thawing; (v) non-viable cells are those which remain swollen above their original size.     

High subzero cryofixation: A technique for observing ice within tissues

While various fixation techniques for observing ice within tissues stored at high sub-zero temperatures currently exist, these techniques require either different fixative solution compositions when assessing different storage temperatures or alteration of the sample temperature to enable alcohol-water substitution. Therefore, high-subzero cryofixation (HSC), was developed to facilitate fixation at any temperature above −80 °C without sample temperature alteration. Rat liver sections (1 cm²) were frozen at a rate of −1 °C/min to −20 °C, stored for 1 h at −20 °C, and processed using classical freeze-substitution (FS) or HSC. FS samples were plunged in liquid nitrogen and held for 1 h before transfer to −80 °C methanol. After 1, 3, or 5 days of −80 °C storage, samples were placed in 3% glutaraldehyde on dry ice and allowed to sublimate. HSC samples were stored in HSC fixative at −20 °C for 1, 3, or 5 days prior to transfer to 4 °C. Tissue sections were paraffin embedded, sliced, and stained prior to quantification of ice size. HSC fixative permeation was linear with time and could be mathematically modelled to determine duration of fixation required for a given tissue depth. Ice grain size within the inner regions of 5 d samples was consistent between HSC and FS processing (p = 0.76); however, FS processing resulted in greater ice grains in the outer region of tissue. This differed significantly from HSC outer regions (p = 0.016) and FS inner regions (p = 0.038). No difference in ice size was observed between HSC inner and outer regions (p = 0.42). This work demonstrates that HSC can be utilized to observe ice formed within liver tissue stored at −20 °C. Unlike isothermal freeze fixation and freeze substitution alternatives, the low melting point of the HSC fixative enables its use at a variety of temperatures without alteration of sample temperature or fixative composition.     

VISUALIZATION OF FREEZING DAMAGE

Freeze-cleaving can be used as a direct probe to examine the ultrastructural alterations of biological material due to freezing. We examined the thesis that at least two factors, which are oppositely dependent upon cooling velocity, determine the survival of cells subjected to freezing. According to this thesis, when cells are cooled at rates exceeding a critical velocity, a decrease in viability is caused by the presence of intracellular ice; but cells cooled at rates less than this critical velocity do not contain appreciable amounts of intracellular ice and are killed by prolonged exposure to a solution that is altered by the presence of ice. As a test of this hypothesis, we examined freeze-fractured replicas of the yeast Saccharomyces cerevisiae after suspensions had been cooled at rates ranging from 1.8 to 75,000°C/min. Some of the frozen samples were cleaved and replicated immediately in order to minimize artifacts due to sample handling. Other samples were deeply etched or were rewarmed to -20°C and recooled before replication. Yeast cells cooled at or above the rate necessary to preserve maximal viability (~7°C/min) contained intracellular ice, whereas cells cooled below this rate showed no evidence of intracellular ice.     

Intracellular ice formation and growth in MCF-7 cancer cells

Direct cell injury in cryosurgery is highly related to intracellular ice formation (IIF) during tissue freezing and thawing. Mechanistic understanding of IIF in tumor cells is critical to the development of tumor cryo-ablation protocol. In aid of a high speed CMOS camera system, the events of IIF in MCF-7 cells have been studied using cryomicroscopy. Images of ‘darkening’ type IIF and recrystallization are compared between cells frozen with and without ice seeding. It is found that ice seeding has significant impact on the occurrence and growth of intracellular ice. Without ice seeding, IIF is observed to occur over a very small range of temperature (∼1 °C). The crystal dendrites are indistinguishable, which is independent of the cooling rate. Ice crystal grows much faster and covers the whole intracellular space in comparison to that with ice seeding, which ice stops growing near the cellular nucleus. Recrystallization is observed at the temperature from −13 °C to −9 °C during thawing. On the contrary, IIF occurs from −7 °C to −20 °C with ice seeding at a high subzero temperature (i.e., −2.5 °C). The morphology of intracellular ice frozen is greatly affected by the cooling rate, and no ‘darkening’ type ice formed inside cells during thawing. In addition, the intracellular ice formation is directional, which starts from the plasma membrane and grows toward the cellular nucleus with or without ice seeding. These results can be used to explain some findings of tumor cryosurgery in vivo, especially the causes of insufficient killing of tumor cells in the peripheral area near vessels.     

Diversity and association of psychrophilic bacteria in Antarctic sea ice.

The bacterial populations associated with sea ice sampled from Antarctic coastal areas were investigated by use of a phenotypic approach and a phylogenetic approach based on genes encoding 16S rRNA (16S rDNA). The diversity of bacteria associated with sea ice was also compared with the bacterial diversity of seawater underlying sea ice. Psychrophilic (optimal growth temperature, < or = 15 degrees C; no growth occurring at 20 degrees C) bacterial diversity was found to be significantly enriched in sea ice samples possessing platelet and bottom ice diatom assemblages, with 2 to 9 distinct (average, 5.6 +/- 1.8) psychrophilic taxa isolated per sample. Substantially fewer psychrophilic isolates were recovered from ice cores with a low or negligible population of ice diatoms or from under-ice seawater samples (less than one distinct taxon isolated per sample). In addition, psychrophilic taxa that were isolated from under-ice seawater samples were in general phylogenetically distinct from psychrophilic taxa isolated from sea ice cores. The taxonomic distributions of psychrotrophic bacterial isolates (optimal growth temperature, > 20 degrees C; growth can occur at approximately 4 degrees C) isolated from sea ice cores and under-ice seawater were quite similar. Overall, bacterial isolates from Antarctic sea ice were found to belong to four phylogenetic groups, the alpha and gamma subdivisions of the Proteobacteria, the gram-positive branch, and the Flexibacter-Bacteroides-Cytophaga phylum. Most of the sea ice strains examined appeared to be novel taxa based on phylogenetic comparisons, with 45% of the strains being psychrophilic. 16S rDNA sequence analysis revealed that psychrophilic strains belonged to the genera Colwellia, Shewanella, Marinobacter, Planococcus, and novel phylogenetic lineages adjacent to Colwellia and Alteromonas and within the Flexibacter-Bacteroides-Cytophaga phylum. Psychrotrophic strains were found to be members of the genera Pseudoalteromonas, Psychrobacter, Halomonas, Pseudomonas, Hyphomonas, Sphingomonas, Arthrobacter, Planococcus, and Halobacillus. From this survey, it is proposed that ice diatom assemblages provide niches conducive to the proliferation of a diverse array of psychrophilic bacterial species.     

Effects of river ice on riparian vegetation

1. Many rivers and streams experience pronounced ice dynamics caused by the formation of anchor and frazil ice, leading to flooding and disturbance of riparian and aquatic communities. However, the effects of dynamic ice conditions on riverine biota are little known. 2. We studied the formation of anchor ice in natural streams over 2 years and assessed the effects of anchor ice on riparian vegetation by comparing sites with frequent or abundant and little or no anchor ice formation. We also studied the direct impact of ice on riparian plants by experimentally creating ice in the riparian zone over three winters and by exposing plants of different life forms to ?18 °C cold ice in the laboratory. 3. Riparian species richness per 1‐m² plot was higher at sites affected by anchor ice than at sites where anchor ice was absent or rare, whereas dominance was lower, suggesting that disturbance by ice enhances species richness. Species composition was more homogenous among plots at anchor ice sites. By experimentally creating riparian ice, we corroborated the comparative results, with species richness increasing in ice‐treated plots compared to controls, irrespective of whether the sites showed natural anchor ice. 4. Because of human alterations of running waters, the natural effects of river ice on stream hydrology, geomorphology and ecology are little known. Global warming in northern streams is expected to lead to more dynamic ice conditions, offering new challenges for aquatic organisms and river management. Our results should stimulate new research, contributing to a better understanding of ecosystem function during winter.     

Rapidly cooled horse spermatozoa: loss of viability is due to osmotic imbalance during thawing, not intracellular ice formation

The cellular damage that spermatozoa encounter at rapid rates of cooling has often been attributed to the formation of intracellular ice. However, no direct evidence of intracellular ice has been presented. An alternative mechanism has been proposed by Morris (2006) that cell damage is a result of an osmotic imbalance encountered during thawing. This paper examines whether intracellular ice forms during rapid cooling or if an alternative mechanism is present. Horse spermatozoa were cooled at a range of cooling rates from 0.3 to 3,000 degrees C/min in the presence of a cryoprotectant. The ultrastructure of the samples was examined by Cryo Scanning Electron Microscopy (CryoSEM) and freeze substitution, to determine whether intracellular ice formed and to examine alternative mechanisms of cell injury during rapid cooling. No intracellular ice formation was detected at any cooling rate. Differential scanning Calorimetry (DSC) was employed to examine the amount of ice formed at different rate of cooling. It is concluded that cell damage to horse spermatozoa, at cooling rates of up to 3,000 degrees C/min, is not caused by intracellular ice formation. Spermatozoa that have been cooled at high rates are subjected to an osmotic shock when they are thawed.     

<Emphasis Type="Italic">Polytrichum commune</Emphasis> spores nucleate ice and associated microorganisms increase the temperature of ice nucleation activity onset

Moss spores disperse via wind and have been found previously in precipitation and air samples. Their presence in the atmosphere led to this study’s examining the potential of moss spores to contribute to ice nucleation, a process necessary for ice formation in clouds prior to precipitation. Ice nucleation assays were conducted using Polytrichum commune spores that were either associated with natural assemblages of microbes or extracted aseptically from capsules and subsequently confirmed to be free of culturable microbes. Liquid suspensions of capsule spores and non-sterile spores nucleated ice at temperatures as high as ?12 and ?7 °C, respectively. When capsule and non-sterile spores were heated at 95 °C for 10 min, which killed all culturable microbes on non-sterile spores, both nucleated ice from ?10 to ?13 °C. An additional non-sterile spore sample collected from partially opened capsules in a forested ecosystem (ID, USA) nucleated ice at temperatures as high as ?7 °C, similar to non-sterile P. commune spores. This is the first set of results to indicate that P. commune spores themselves are capable of nucleating ice at temperatures higher than many abiological particles such as mineral dust (≤?15 °C) and that natural assemblages of microbes can increase their ice nucleation efficiency. Future studies aimed at determining the abundance of moss spores in the atmosphere and the identity of ice-nucleating microbes associated with them will provide further insights into the ability of moss spores to impact precipitation patterns.     

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).