Bacterial Activity at −2 to −20°C in Arctic Wintertime Sea Ice

Arctic wintertime sea-ice cores, characterized by a temperature gradient of −2 to −20°C, were investigated to better understand constraints on bacterial abundance, activity, and diversity at subzero temperatures. With the fluorescent stains 4′,6′-diamidino-2-phenylindole 2HCl (DAPI) (for DNA) and 5-cyano-2,3-ditoyl tetrazolium chloride (CTC) (for O₂-based respiration), the abundances of total, particle-associated (>3-μm), free-living, and actively respiring bacteria were determined for ice-core samples melted at their in situ temperatures (−2 to −20°C) and at the corresponding salinities of their brine inclusions (38 to 209 ppt). Fluorescence in situ hybridization was applied to determine the proportions of Bacteria, Cytophaga-Flavobacteria-Bacteroides (CFB), and Archaea. Microtome-prepared ice sections also were examined microscopically under in situ conditions to evaluate bacterial abundance (by DAPI staining) and particle associations within the brine-inclusion network of the ice. For both melted and intact ice sections, more than 50% of cells were found to be associated with particles or surfaces (sediment grains, detritus, and ice-crystal boundaries). CTC-active bacteria (0.5 to 4% of the total) and cells detectable by rRNA probes (18 to 86% of the total) were found in all ice samples, including the coldest (−20°C), where virtually all active cells were particle associated. The percentage of active bacteria associated with particles increased with decreasing temperature, as did the percentages of CFB (16 to 82% of Bacteria) and Archaea (0.0 to 3.4% of total cells). These results, combined with correlation analyses between bacterial variables and measures of particulate matter in the ice as well as the increase in CFB at lower temperatures, confirm the importance of particle or surface association to bacterial activity at subzero temperatures. Measuring activity down to −20°C adds to the concept that liquid inclusions in frozen environments provide an adequate habitat for active microbial populations on Earth and possibly elsewhere.     

Phylogenetic Diversity of Numerically Important Arctic Sea-Ice Bacteria Cultured at Subzero Temperature

Heterotrophic bacteria in sea ice play a key role in carbon cycling, but little is known about the predominant players at the phylogenetic level. In a study of both algal bands and clear ice habitats within summertime Arctic pack ice from the Chukchi Sea, we determined the abundance of total bacteria and actively respiring cells in melted ice samples using epifluorescence microscopy and the stains 4', 6'-diamidino-2-phenylindole 2HCl (DAPI) and 5-cyano-2,3-ditolyl tetrazolium chloride (CTC), respectively. Organic-rich and -poor culturing media were used to determine culturable members by plating (at 0 degrees C and 5 degrees C) and most-probable-number (MPN) analyses (at -1 degrees C). Total bacterial counts ranged from 5.44 x 10(4) ml(-1) in clear ice to 2.41 x 10(6) ml(-1) in algal-band ice samples, with 2-27% metabolically active by CTC stain. Plating and MPN results revealed a high degree of culturability in both types of media, but greater success in oligotrophic media (to 62% of total abundance) and from clear ice samples. The bacterial enumeration anomaly, commonly held to mean 相似文献   

16S rRNA sequences and differences in bacteria isolated from the Muztag Ata glacier at increasing depths

Small subunit 16S rRNA sequences, growth temperatures, and phylogenetic relationships have been established for 129 bacterial isolates recovered under aerobic growth conditions from different regions of a 22-m ice core from the Muztag Ata Mountain glacier on the Pamirs Plateau (China). Only 11% were psychrophiles (grew at 2 degrees C or -2 degrees C up to approximately 20 degrees C), although the majority (82%) were psychrotolerant (grew at 2 degrees C or -2 degrees C up to 37 degrees C). The majority of the isolates had 16S rRNA sequences similar to previously determined sequences, ranging from 85% to 100% identical to database sequences. Based on their 16S rRNA sequences, 42.6% of the isolates were high-G+C (HGC) gram-positive bacteria, 23.3% were gamma-Proteobacteria, 14.7% were alpha-Proteobacteria, 14.7% were Flavobacteria, and 4.7% were low-G+C (LGC) gram-positive bacteria. There were clear differences in the depth distribution, with Proteobacteria, HGC/Cytophaga-Flavobacterium-Bacteroides (CFB), Proteobacteria, LGC/CFB/HGC, Cryobacterium psychrophilum, HGC/CFB, Proteobacteria/HGC/CFB, and HGC/CFB being the predominant isolates from ice that originated from 2.7 to 3.8, 6.2, 7.5, 8.3, 9.0, 9.7, 12.5, and 15.3 m below the surface, respectively. This layered distribution of bacterial isolates presumably reflects both differences in bacteria inhabiting the glacier's surface, differences in bacteria deposited serendipitously on the glacier's surface by wind and snowfall, and nutrient availability within the ice.     

Survival of frozen mouse embryos after rapid thawing from -196 degrees C.

The effect of the rate of rewarming on the survival of 8-cell mouse embryos and blastocysts was examined. The samples were slowly cooled (0.3--0.6 degrees C/min) in 1.5 M-DMSO to temperatures between -10 and -80 degrees C before direct transfer to liquid nitrogen (-196 degrees C). Embryos survived rapid thawing (275--500 degrees C/min) only when slow cooling was terminated at relatively high subzero temperatures (-10 to -50 degrees C). The highest levels of survival in vitro of rapidly thawed 8-cell embryos were obtained after transfer to -196 degrees C from -35 and -40 degrees C (72 to 88%) and of rapidly thawed blastocysts after transfer from -25 to -50 degrees C (69 to 74%). By contrast, for embryos to survive slow thawing (8 to 20 degrees C/min) slow cooling to lower subzero temperatures (-60 degrees C and below) was required before transfer to -196 degrees C. The results indicate that embryos transferred to -196 degrees C from high subzero temperatures contain sufficient intracellular ice to damage them during slow warming but to permit survival after rapid warming. Survival of embryos after rapid dilution of DMSO at room temperature was similar to that after slow (stepwise) dilution at 0 degrees C. There was no difference between the viability of rapidly and slowly thawed embryos after transfer to pseudopregnant foster mothers. It is concluded that the behaviour of mammalian embryos subjected to the stresses of freezing and thawing is similar to that of other mammalian cells. A simpler and quicker method for the preservation of mouse embryos is described.     

Stabilization of frozen Lactobacillus delbrueckii subsp. bulgaricus in glycerol suspensions: Freezing kinetics and storage temperature effects

The interactions between freezing kinetics and subsequent storage temperatures and their effects on the biological activity of lactic acid bacteria have not been examined in studies to date. This paper investigates the effects of three freezing protocols and two storage temperatures on the viability and acidification activity of Lactobacillus delbrueckii subsp. bulgaricus CFL1 in the presence of glycerol. Samples were examined at -196 degrees C and -20 degrees C by freeze fracture and freeze substitution electron microscopy. Differential scanning calorimetry was used to measure proportions of ice and glass transition temperatures for each freezing condition tested. Following storage at low temperatures (-196 degrees C and -80 degrees C), the viability and acidification activity of L. delbrueckii subsp. bulgaricus decreased after freezing and were strongly dependent on freezing kinetics. High cooling rates obtained by direct immersion in liquid nitrogen resulted in the minimum loss of acidification activity and viability. The amount of ice formed in the freeze-concentrated matrix was determined by the freezing protocol, but no intracellular ice was observed in cells suspended in glycerol at any cooling rate. For samples stored at -20 degrees C, the maximum loss of viability and acidification activity was observed with rapidly cooled cells. By scanning electron microscopy, these cells were not observed to contain intracellular ice, and they were observed to be plasmolyzed. It is suggested that the cell damage which occurs in rapidly cooled cells during storage at high subzero temperatures is caused by an osmotic imbalance during warming, not the formation of intracellular ice.     

Viability, diversity and composition of the bacterial community in a high Arctic permafrost soil from Spitsbergen, Northern Norway

The viable and non-viable fractions of the bacterial community in a 2347-year-old permafrost soil from Spitsbergen were subjected to a comprehensive investigation using culture-independent and culture-dependent methods. LIVE/DEAD BacLight staining revealed that 26% of the total number of bacterial cells were viable. Quantitatively, aerobic microcolonies, aerobic colony-forming units and culturable anaerobic bacteria comprised a minor fraction of the total number of viable bacteria, which underlines the necessity for alternative cultivation approaches in bacterial cryobiology. Sulfate reduction was detected at temperatures between -2 degrees C and 29 degrees C while methanogenesis was not detected. Bacterial diversity was high with 162 operational taxonomic units observed from 800 16S rDNA clone sequences. The 158 pure cultures isolated from the permafrost soil affiliated with 29 different bacterial genera, the majority of which have not previously been isolated from permafrost habitats. Most of the strains isolated were affiliated to the genera Cellulomonas and Arthrobacter and several of the pure cultures were closely related to bacteria reported from other cryohabitats. Characterization of viable bacterial communities in permafrost soils is important as it will enable identification of functionally important groups together with the as yet undescribed adaptations that bacteria have evolved for surviving subzero temperatures for millennia.     

Isolation and characterization of phage–host systems from the Baltic Sea ice

In search for sea ice bacteria and their phages from the Baltic Sea ice, two ice samples were collected from land-fast ice in a south-west Finland coastal site in February and March 2011. Bacteria were isolated from the melted sea ice samples and phages were screened from the same samples for 43 purified isolates. Plaque-producing phages were found for 15 bacterial isolates at 3 °C. Ten phage isolates were successfully plaque purified and eight of them were chosen for particle purification to analyze their morphology and structural proteins. Phage 1/32 infecting an isolate affiliated to phylum Bacteroidetes (Flavobacterium sp.) is a siphovirus and six phages infecting isolates affiliated to γ-Proteobacteria (Shewanella sp.) hosts were myoviruses. Cross titrations between the hosts showed that all studied phages are host specific. Phage solutions, host growth and phage infection were tested in different temperatures revealing phage temperature tolerance up to 45 °C, whereas phage infection was in most of the cases retarded above 15 °C. This study is the first to report isolation and cultivation of ice bacteria and cold-active phages from the Baltic Sea ice.     

东天山地区庙儿沟雪坑中微生物多样性、群落结构与环境关系研究

通过荧光计数、恢复培养和变形梯度凝胶电泳(DGGE),分析了东天山地区庙儿沟不同深度积雪中的可培养细菌数量、多样性及其群落结构。结果表明,东天山地区冰雪微生物数量和多样性指数与气候环境替代指标钙离子、镁离子、氯离子等具有相关性。该地区雪坑中细菌隶属于4个不同系统发育群:proteobacteria(α-,β-,γ-),CFB,HGC和LGC,其中CFB类和proteobacteria类为主要类群。与青藏高原、南北极冰雪中微生物的比较分析发现Paracoccu和Aquasalina属是该地区的特殊微生物类群。直接培养和DGGE分析发现不同深度雪坑中微生物数量和群落结构都有明显的变化。结果表明,由于东天山地区的特殊地理位置,该地区冰雪微生物具有其特殊性。     

Differential enumeration and in situ localization of microorganisms in the hindgut of the lower termite Mastotermes darwiniensis by hybridization with rRNA-targeted probes

We examined the abundance and spatial distribution of major phylogenetic groups of the domain Bacteria in hindguts of the Australian lower termite Mastotermes darwiniensis by using in situ hybridization with group-specific, fluorescently labeled, rRNA-targeted oligonucleotide probes. Between 32.0 ± 7.2% and 52.3 ± 8.2% of the DAPI-stained cells in different hindgut fractions were detected with probe EUB338, specific for members of the domain Bacteria. About 85% of the prokaryotic cells were associated with the flagellates of the thin-walled anterior region (P3a) and the thick wall of the posterior region (P3b/P4) of the hindgut, as shown by DAPI staining. At most, half of the EUB338-detected cells hybridized with one of the other probes that targeted a smaller assemblage within the bacterial domain. In most fractions, cells were found in varying numbers with probe ALF1b, which targeted members of the α-Proteobacteria, whereas substantial amounts of sulfate-reducing bacteria, gram-positive bacteria with a high DNA G+C content and members of the Cytophaga-Flavobacterium cluster of the Cytophaga-Flavobacterium-Bacteroides (CFB) phylum could be detected only in the wall fraction of P3b/P4. This clearly indicates that the hindgut microhabitats differ in the composition of their microbial community. In situ hybridization of cryosections through the hindgut showed only low numbers of bacteria attached to the P3a wall. In contrast, the wall of P3b was densely colonized by rod- and coccus-shaped bacteria, which could be assigned to the Cytophaga-Flavobacterium cluster of the CFB phylum and to the group of gram-positive bacteria with a high DNA G+C content, respectively. Oxygen concentration profiles determined with microelectrodes revealed steep oxygen gradients both in P3a and P3b. Oxygen was consumed within 100 μm below the gut surface, and anoxic conditions prevailed in the central portions of both gut regions, indicating that oxygen consumption in the hindgut does not depend on the presence of a biofilm on the hindgut wall. Received: 17 May 1999 / Accepted: 16 September 1999     

Bacterial incorporation of leucine into protein down to -20 degrees C with evidence for potential activity in sub-eutectic saline ice formations

Direct evidence for metabolism in a variety of frozen environments has pushed temperature limits for bacterial activity to increasingly lower temperatures, so far to -20 degrees C. To date, the metabolic activities of marine psychrophilic bacteria, important components of sea-ice communities, have not been studied in laboratory culture, not in ice and not below -12 degrees C. We measured [3H]-leucine incorporation into macromolecules (further fractionated biochemically) by the marine psychrophilic bacterium Colwellia psychrerythraea strain 34H over a range of anticipated activity-permissive temperatures, from +13 to -20 degrees C, including expected negative controls at -80 and -196 degrees C. For incubation temperatures below -1 degrees C, the cell suspensions [all in artificial seawater (ASW)] were first quick-frozen in liquid nitrogen. We also examined the effect of added extracellular polymeric substances (EPS) on [3H]-leucine incorporation. Results showed that live cells of strain 34H incorporated substantial amounts of [3H]-leucine into TCA-precipitable material (primarily protein) down to -20 degrees C. At temperatures from -1 to -20 degrees C, rates were enhanced by EPS. No activity was detected in the killed controls for strain 34H (or in Escherichia coli controls), which included TCA-killed, heat-killed, and sodium azide- and chloramphenicol-treated samples. Surprisingly, evidence for low but significant rates of intracellular incorporation of [3H]-leucine into protein was observed for both ASW-only and EPS-amended (and live only) samples incubated at -80 and -196 degrees C. Mechanisms that could explain the latter results require further study, but the process of vitrification promoted by rapid freezing and the presence of salts and organic polymers may be relevant. Overall, distinguishing between intracellular and extracellular aspects of bacterial activity appears important to understanding behavior at sub-freezing temperatures.     

Bacterial activity in South Pole snow

Large populations (200 to 5,000 cells ml(-1) in snowmelt) of bacteria were present in surface snow and firn from the south pole sampled in January 1999 and 2000. DNA isolated from this snow yielded ribosomal DNA sequences similar to those of several psychrophilic bacteria and a bacterium which aligns closely with members of the genus Deinococcus, an ionizing-radiation- and desiccation-resistant genus. We also obtained evidence of low rates of bacterial DNA and protein synthesis which indicates that the organisms were metabolizing at ambient subzero temperatures (-12 to -17 degrees C).     

16S rRNA Sequences and Differences in Bacteria Isolated from the Muztag Ata Glacier at Increasing Depths

Small subunit 16S rRNA sequences, growth temperatures, and phylogenetic relationships have been established for 129 bacterial isolates recovered under aerobic growth conditions from different regions of a 22-m ice core from the Muztag Ata Mountain glacier on the Pamirs Plateau (China). Only 11% were psychrophiles (grew at 2°C or −2°C up to ~20°C), although the majority (82%) were psychrotolerant (grew at 2°C or −2°C up to 37°C). The majority of the isolates had 16S rRNA sequences similar to previously determined sequences, ranging from 85% to 100% identical to database sequences. Based on their 16S rRNA sequences, 42.6% of the isolates were high-G+C (HGC) gram-positive bacteria, 23.3% were γ-Proteobacteria, 14.7% were α-Proteobacteria, 14.7% were Flavobacteria, and 4.7% were low-G+C (LGC) gram-positive bacteria. There were clear differences in the depth distribution, with Proteobacteria, HGC/Cytophaga-Flavobacterium-Bacteroides (CFB), Proteobacteria, LGC/CFB/HGC, Cryobacterium psychrophilum, HGC/CFB, Proteobacteria/HGC/CFB, and HGC/CFB being the predominant isolates from ice that originated from 2.7 to 3.8, 6.2, 7.5, 8.3, 9.0, 9.7, 12.5, and 15.3 m below the surface, respectively. This layered distribution of bacterial isolates presumably reflects both differences in bacteria inhabiting the glacier's surface, differences in bacteria deposited serendipitously on the glacier's surface by wind and snowfall, and nutrient availability within the ice.     

Cold-active chemoorganotrophic bacteria from permanently ice-covered Lake Hoare, McMurdo Dry Valleys, Antarctica

Eight strains of chemoorganotrophic bacteria were isolated from the water column of Lake Hoare, McMurdo Dry Valleys, Antarctica, using cold enrichment temperatures. The isolates were Alpha-, Beta-, and Gammaproteobacteria and Actinobacteria spp. All isolates grew at 0 degrees C, and all but one grew at subzero temperatures characteristic of the water column of Lake Hoare. Growth temperature optima varied among isolates, but the majority showed optima near 15 degrees C, indicative of cold-active phenotypes. One isolate was truly psychrophilic, growing optimally around 10 degrees C and not above 20 degrees C. Half of the isolates grew at 2% salt while the other half did not, and all but one isolate grew at 2 atm of O(2). Our isolates are the first prokaryotes from the water column of Lake Hoare to be characterized phylogenetically and physiologically and show that cold-active species of at least two major phyla of Bacteria inhabit Lake Hoare.     

Reproduction and metabolism at - 10 degrees C of bacteria isolated from Siberian permafrost

We report the isolation and properties of several species of bacteria from Siberian permafrost. Half of the isolates were spore-forming bacteria unable to grow or metabolize at subzero temperatures. Other Gram-positive isolates metabolized, but never exhibited any growth at - 10 degrees C. One Gram-negative isolate metabolized and grew at - 10 degrees C, with a measured doubling time of 39 days. Metabolic studies of several isolates suggested that as temperature decreased below + 4 degrees C, the partitioning of energy changes with much more energy being used for cell maintenance as the temperature decreases. In addition, cells grown at - 10 degrees C exhibited major morphological changes at the ultrastructural level.     

Freezing and cryoprotective dehydration in an Antarctic nematode (Panagrolaimus davidi) visualised using a freeze substitution technique

The pattern of ice formation during the freezing of Panagrolaimus davidi, an Antarctic nematode that can survive intracellular ice formation, was visualised using a freeze substitution technique and transmission electron microscopy. Nematodes plunged directly into liquid nitrogen had small ice crystals throughout their tissues, including nuclei and organelles, but did not survive. Those frozen at high subzero temperatures showed three patterns of ice formation: no ice, extracellular ice, and intracellular ice. Nematodes subjected to a slow-freezing regime (at -1 degrees C) had mainly extracellular ice (70.4%), with the bulk of the ice in the pseudocoel. Some (24.8%) had no ice within their bodies, due to cryoprotective dehydration. Nematodes subjected to a fast-freezing regime (at -4 degrees C) had intracellular (54%) and extracellular (42%) ice. Intracellular ice was confined to the cytoplasm of cells, with organelles in the spaces in between ice crystals. The survival of nematodes subjected to the fast-freezing regime (53%) was less than those subjected to the slow-freezing regime (92%).     

Cryomicroscopic observations of cattle embryos during freezing and thawing

A cryomicroscope was used to observe changes in the appearance of day 6 1 2 to 7 1 2 cattle embryos during cooling and warming in 1.4M glycerol/PBS. Embryos were cooled at various rates between 0.2 and 25 degrees C/min to temperatures between -25 and -60 degrees C and then cooled rapidly ( approximately 250 degrees C/min) to temperatures below -140 degrees C. The volume of the embryos calculated from the cross-sectional area during slow cooling decreased at -25 degrees C to about 50% of the isotonic volume. Fracture planes could be observed in the extracellular ice matrix surrounding the embryos after rapid cooling to approximately -140 degrees C. The fracture planes often touched the zona pellucida and sometimes caused cracks in the zona. Cracks in the zona pellucida were observed more often after rapid cooling from temperatures between -20 to -35 degrees C (9 13 ) than from temperatures between -36 to -60 degrees C (2 7 ). When embryos were warmed rapidly ( approximately 250 degrees C/min) from temperatures below -140 degrees C, no change was observed in the appearance of either the embryo or its surroundings except the melting of the extracellular ice. However, when embryos were warmed slowly (2 or 5 degrees C/min), a series of events was observed; first, at approximately -70 degrees C the cytoplasm and the extracellular space gradually darkened and reached maximum darkness at approximately -55 degrees C. Then, on continued slow warming, the dark material gradually disappeared and finally the large extracellular ice crystals melted.     

Community analysis of the bacterial assemblages in the winter cover and pelagic layers of a high mountain lake by in situ hybridization

The bacterial community structure in the winter cover and pelagic zone of a high mountain lake was analyzed by in situ hybridization with fluorescently labeled rRNA-targeted oligonucleotide probes. Cells fixed on membrane filters were hybridized with a probe specific for the domain Bacteria as well as with probes for the alpha, beta, and gamma subclasses of the class Proteobacteria and the Cytophaga-Flavobacterium group. The fraction of bacteria detectable after hybridization with the bacterial probe EUB ranged from 40 to 81% of 4(prm1),6-diamidino-2-phenylindole (DAPI) counts. The bacterial assemblage varied considerably between and within different habitats (snow, slush, and lake water) but was in most cases dominated by members of the beta subclass (6.5 to 116% of bacteria detectable with probe EUB). The sum of bacteria hybridizing with group-specific probes was usually lower than the fraction detectable with probe EUB. Image analysis was used to characterize morphology and the size-specific biomass distribution of bacterial assemblages, which clearly separated the three habitats. Although the measured secondary production parameters and the fraction of 2-(p-iodophenyl)-3-(p-nitrophenyl)-5-phenyltetrazolium chloride-reducing bacteria varied by more than an order of magnitude in the different slush and pelagic layers, detectability with the fluorescent probe EUB was constantly high. Physiological strategies of bacteria under nutrient limitation and at low temperatures are discussed in the context of the ribosome content of single cells. This study confirms the suitability of fluorescently labeled rRNA-targeted probes for the characterization of bacterial population structures even in oligotrophic habitats.     

Variations in antifreeze activity and serum inorganic ions in the eelpout Zoarces viviparus: antifreeze activity in the embryonic state.

The eelpout Zoarces viviparus is a common inhabitant in the shallow waters along the Danish coastline. Specimens were caught in the brackish (12-16 per thousand) Roskilde fjord where water temperatures range from >20 degrees C during summer to subzero in winter. The serum melting points found in Z. viviparus varied between -0.76 (September) to -0.94 degrees C (January). Eighty to 97% of the serum melting points could be attributed to sodium, chloride and potassium. Hysteresis freezing points showed seasonal variation varying from -0.83 (September) to -2.08 degrees C (February). Serum antifreeze activity showed a seasonal variation with high levels (>1.2 degrees C) in winter and low levels (<0.1 degrees C) during summer and autumn. Antifreeze proteins are responsible for this antifreeze activity. Antifreeze activity was also found in Z. viviparus during their embryological development in the female ovary. Embryo thermal hysteresis reached the maximum level (approx. 0.6 degrees C) during December and maintained this level until parturition in January. Antifreeze activity seems unaffected by diminishing ice crystal fractions at ice fractions below 0.1 whereas ice fractions above 0.1 caused a decline in antifreeze activity.     

Cryopreservation of isolated hepatocytes: intracellular ice formation under various chemical and physical conditions.

Kinetics of intracellular ice formation (IIF) for isolated rat hepatocytes was studied using a cryomicroscopy system. The effect of the cooling rate on IIF was investigated between 20 and 400 degrees C/min in isotonic solution. At 50 degrees C/min and below, none of the hepatocytes underwent IIF; whereas at 150 degrees C/min and above, IIF was observed throughout the entire hepatocyte population. The temperature at which 50% of hepatocytes showed IIF (50TIIF) was almost constant with an average value of -7.7 degrees C. Different behavior was seen in isothermal subzero holding temperatures in the presence of extracellular ice. 50TIIF from isothermal temperature experiments was approximately -5 degrees C as opposed to -7.7 degrees C for constant cooling rate experiments. These experiments clearly demonstrated both the time and temperature dependence of IIF. On the other hand, in cooling experiments in the absence of extracellular ice, IIF was not observed until approximately -20 degrees C (at which temperature the whole suspension was frozen spontaneously) suggesting the involvement of the external ice in the initiation of IIF. The effect of dimethyl sulfoxide (Me2SO) on IIF was also quantified. 50TIIF decreased from -7.7 degrees C in the absence of Me2SO to -16.8 degrees C in 2.0 M Me2SO for a cooling rate of 400 degrees C/min. However, the cooling rate (between 75 and 400 degrees C/min) did not significantly affect 50TIIF (-8.7 degrees C) in 0.5 M Me2SO. These results suggest that multistep protocols will be required for the cryopreservation of hepatocytes.     

The role of ice nucleation active bacteria in supercooling of citrus tissues

The frost sensitivity of Citrus sinensis in relation to the presence of biogenic ice nuclei was studied. In commercially managed citrus groves the ice nucleation active (INA) bacterium Pseudomonas syringae reached 6 × 10⁴ colony forming units (CFU) leaf⁻¹, a population sufficiently high to catalyze ice formation. However, a transient loss of bacterial nucleation activity was noticeable at subzero field temperatures, followed by resumption as temperatures rose. This loss was apparently due to a temporary transition of INA to ice nucleation inactive (INI) bacteria. Field application of Bordeaux mixture, copper hydroxide, streptomycin, and 2-hydroxypropylmethanethiolsulfonate (HPMTS), resulted in reduction of INA bacterial populations to detectability (≤ 10² CFU leaf⁻¹) limits. However, the corresponding reduction in ice nucleation events in treated samples as compared to controls at nucleation temperature ≥−3°C was not as dramatic. It ranged from approximately 7% in samples treated with the bactericide HPMTS, to 35% in samples treated with chemicals possessing combined bactericidal - fungicidal action (coppers). Since a quantitative relationship exists between ice nucleation events on individual leaves and the INA bacterial populations harbored by these leaves, these results suggest the co-existence of a bacterial and a proteinaceous, yet non-bacterial ice nucleating source in citrus, both active at ≥−3°C.