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At least 19 recordsLinked to original sources

Observations of the PCB distribution within and in-between ice, snow, ice-rafted debris, ice-interstitial water, and seawater in the Barents Sea marginal ice zone and the North Pole area.

To evaluate the two hypotheses of locally elevated exposure of persistent organic pollutants (POPs) in ice-associated microenvironments and ice as a key carrier for long-range transport of POPs to the Arctic marginal ice zone (MIZ), dissolved and particulate polychlorinated biphenyls (PCBs) were analyzed in ice, snow, ice-interstitial water (IIW), seawater in the melt layer underlying the ice, and in ice-rafted sediment (IRS) from the Barents Sea MIZ to the high Arctic in the summer of 2001. Ultra-clean sampling equipment and protocols were specially developed for this expedition, including construction of a permanent clean room facility and a stainless steel seawater intake system on the I/B ODEN as well as two mobile 370 l ice-melting systems. Similar concentrations were found in several ice-associated compartments. For instance, the concentration of one of the most abundant congeners, PCB 52, was typically on the order of 0.1-0.3 pg l(-1) in the dissolved (melted) phase of the ice, snow, IIW, and underlying seawater while its particulate organic-carbon (POC) normalized concentrations were around 1-3 ng gPOC(-1) in the ice, snow, IIW, and IRS. The solid-water distribution of PCBs in ice was well correlated with and predictable from K(ow) (ice log K(oc)-log K(ow) regressions: p<0.05, r2=0.78-0.98, n=9), indicating near-equilibrium partitioning of PCBs within each local ice system. These results do generally not evidence the existence of physical microenvironments with locally elevated POP exposures. However, there were some indications that the ice-associated system had harbored local environments with higher exposure levels earlier/before the melting/vegetative season, as a few samples had PCB concentrations elevated by factors of 5-10 relative to the typical values, and the elevated levels were predominantly found at the station where melting had putatively progressed the least. The very low PCB concentrations and absence of any significant concentration gradients, both in-between different matrices and over the Eurasian Arctic basin scale, suggest that ice is not an important long-range transport purveyor of POPs to the Arctic MIZ ecosystem.

Journal Article↗

Identification of actin as a substrate of ICE and an ICE-like protease and involvement of an ICE-like protease but not ICE in VP-16-induced U937 apoptosis.

Human leukemia U937 cells are induced to undergo apoptosis by several chemotherapeutic agents; however, the cellular components involved in the process have not yet been identified. We found that an actin-cleavage activity (ACA) was activated in the VP-16-treated U937 cytosolic fraction and 15K- and 30K-actin fragments were produced. This ACA was inhibited by inhibitors of interleukin-1 beta-converting enzyme (ICE)/ced-3 family proteases, such as Z-Asp-CH2-DCB, YVAD-CHO, TPCK, TLCK, and iodoacetamide. Differing from ICE, the ACA could not process pro-IL-1 beta to mature IL-1 beta. Although ICE can cleave actin in vitro, ICE activity was not activated in the VP-16 treated U937 cells. These results indicate that actin is a potential substrate of ICE and ICE-like proteases, and that VP-16 preferentially activate an ICE-like protease, but not ICE itself, in U937 cells.

Actins↗

Ice recrystallization inhibition in ice cream as affected by ice structuring proteins from winter wheat grass.

Ice recrystallization in quiescently frozen sucrose solutions that contained some of the ingredients commonly found in ice cream and in ice cream manufactured under commercial conditions, with or without ice structuring proteins (ISP) from cold-acclimated winter wheat grass extract (AWWE), was assessed by bright field microscopy. In sucrose solutions, critical differences in moisture content, viscosity, ionic strength, and other properties derived from the presence of other ingredients (skim milk powder, corn syrup solids, locust bean gum) caused a reduction in ice crystal growth. Significant ISP activity in retarding ice crystal growth was observed in all solutions (44% for the most complex mix) containing 0.13% total protein from AWWE. In heat-shocked ice cream, ice recrystallization rates were significantly reduced 40 and 46% with the addition of 0.0025 and 0.0037% total protein from AWWE. The ISP activity in ice cream was not hindered by its inclusion in mix prior to pasteurization. A synergistic effect between ISP and stabilizer was observed, as ISP activity was reduced in the absence of stabilizer in ice cream formulations. A remarkably smoother texture for ice creams containing ISP after heat-shock storage was evident by sensory evaluation. The efficiency of ISP from AWWE in controlling ice crystal growth in ice cream has been demonstrated.

Antifreeze Proteins↗

Ecological Similarity and Coexistence of Epiphytic Ice-Nucleating (Ice) Pseudomonas syringae Strains and a Non-Ice-Nucleating (Ice) Biological Control Agent.

De Wit replacement series were used to study competitive interactions between epiphytic IcePseudomonas syringae strains and the biological frost control agents IceP. syringae TLP2del1 and Pseudomonas fluorescens A506. Mixtures containing two strains in different proportions but at a constant total population size were inoculated onto potato leaves. The population sizes of each strain and the total population size were determined when the community had reached equilibrium. A near-isogenic P. syringae strain pair exhibited an interaction similar to that expected for strains competing equally for limiting environmental resources. Replacement series with nonisogenic Ice and IceP. syringae strain pairs suggested that these strains competed for limiting resources according to their relative competitive abilities. There was no evidence of any niche differentiation between the IceP. syringae strains and the IceP. syringae strain. The growth responses of epiphytes following addition of nutrients to the phyllosphere indicated that the epiphytic P. syringae populations were nutrient limited and that, under growth chamber conditions, the populations were more limited by the availability of carbon than by the availability of nitrogen. Determination of in vitro carbon source utilization profiles provided further evidence for the lack of niche differentiation between the Ice and the IceP. syringae strains. Niche overlap indices calculated for the IceP. syringae strains with respect to IceP. syringae TLP2del1 were uniformly high, indicating ecological similarity, and were consistent with the observed low level of coexistence. The biological frost control agent P. fluorescens A506 replaced P. syringae. This was correlated with a high degree of niche overlap between these species.

Journal Article↗

Evidence for an interleukin-1beta converting enzyme (ICE)-like activity distinct from ICE and responsible for ICE and CPP32 cleavage during apoptosis.

IL-1beta converting enzyme (ICE) and ICE-related proteases (IRPs) have been suggested to play a central role in apoptosis. We report the use of peptidic ICE inhibitors to reassess the role of this enzyme in the apoptosis induced by Fas or TNFalpha receptor ligation in Jurkat cells, U937 cells or monocytes. Our results show that inhibition of IL-1beta processing can be dissociated from inhibition of apoptosis. Indeed, two out of three com-pounds active on ICE are not inhibitory for apoptosis. This shows that ICE is not required for progression in the apoptotic pathway, but that one or several IRPs are necessary. In addition, Western blot analysis of cell lysates shows that both ICE and CPP32 precursors disappear rapidly after apoptosis induction, while ICH-1L precursor remains intact. Concomitant appearance of cleavage products can be visualized for CPP32, but not for ICE, suggesting that the former is proteolytically activated. In addition, this precursor cleavage can be blocked by an ICE inhibitor active on apoptosis. Altogether, our data support the hypothesis that one or several IRPs are necessary for apoptosis and are responsible for ICE and CPP32 cleavage during this process.

Journal Article↗

Ice binding, recrystallization inhibition, and cryoprotective properties of ice-active substances associated with Antarctic sea ice diatoms.

Extracellular macromolecules associated with Antarctic sea ice diatoms were previously shown to have ice-binding activities. The function of these ice-active substances (IASs) has not been identified. Here we show that two of the IASs have a strong ability to inhibit the recrystallization of ice, possibly signifying a cryoprotectant function. To test this possibility, two species of marine diatom (one Antarctic and one temperate) were subjected to a single freeze-thaw cycle (approximately 20h at -4 or -5 degrees C) in the presence or absence of IAS. Viability, based on a double staining technique, was 15-29% higher in the presence of IAS. Etching of single crystal ice hemispheres grown from dilute IAS solutions indicated that the IASs bind to specific faces of ice and are incorporated into the ice lattice. Together, these results suggest that the IASs acts as a cryoprotectant, probably through some ice-binding mechanism.

Animals↗

Prediction of ice skating performance with off-ice testing in women's ice hockey players.

Off-ice predictors of skating performance have not been investigated for women's hockey players. The purpose of this study was to identify the off-ice variables associated with high-performance skating acceleration, speed, agility, and on-ice anaerobic capacity and power in women's ice hockey players. Sixty-one women's ice hockey players between the ages of 8 and 16 years (x age = 12.18 +/- 2.05 years, x playing experience = 4.68 +/- 2.69 years) participated in the study. Subjects were 1-4 months postseason. Some players were continuing to play once per week during the off-season. Skating tests (ST) included (a) 6.10-m acceleration, (b) 47.85-m speed, (c) agility cornering S turn, and (d) modified repeat skate test (MRS). Two trials of each ST were measured with a photoelectric timing system (except MRS, which was measured with 1 trial). The off-ice variables that were evaluated included age, years of playing experience, height, body mass, predicted fat percentage, sit-and-reach flexibility, vertical jump height, 40-yd dash time, and 1-minute timed sit-ups and push-ups. The results of this study show that 40-yd dash time is the strongest predictor of skating speed in women's hockey players ages 8-16 years old. From the regression procedure the best prediction equation was speed = 4.913 - (0.0107 x kilograms) + (0.4356 x 40-yd dash time).

Adolescent↗

Thermal evolution of acetic acid nanodeposits over 123-180 K on noncrystalline ice and polycrystalline ice studied by FTIR reflection-absorption spectroscopy: hydrogen-bonding interactions in acetic acid and between acetic acid and ice.

Acetic acid vapor-deposited on ultrathin noncrystalline ice (NCI) and polycrystalline ice (PCI) films (less than 6 nm thick) under ultrahigh vacuum conditions has been investigated by using Fourier Transform Infrared Reflection-Absorption Spectroscopy. Pristine acetic acid deposited at 123 K (on a copper support) appears as an amorphous solid, which undergoes an irreversible phase transformation to a more structurally ordered (polycrystalline) form upon annealing to 153 K. Acetic acid is found to adsorb on NCI and PCI films initially through hydrogen bonding between C=O and dangling OH (of ice), followed by the formation of multilayers at 123 K. Thermal evolution studies of a low exposure of acetic acid on the ultrathin NCI and PCI films show that acetic acid undergoes coevaporation with water likely as an acetic acid hydrate at 155 K, which continues until the entire ice film has been exhausted at 165 K. Above 165 K, the remaining acetic acid solid appears to evaporate without undergoing the phase transformation, in contrast to the case of a high acetic acid exposure. Coevaporation of acetic acid with water is also found to proceed at a faster rate than the subsequent evaporation of acetic acid, which is consistent with the weaker interactions observed in the H-bonded acetic acid hydrate than that in acetic acid solid.

Journal Article↗

Formation of high density amorphous ice by decompression of ice VII and ice VIII at 135 K.

Monte Carlo computer simulations of ice VII and ice VIII phases have been undertaken using the four-point transferable intermolecular potential model of water. By following thermodynamic paths similar to those used experimentally, ice is decompressed resulting in an amorphous phase. These phases are compared to the high density amorphous phase formed upon compression of ice Ih and are found to have very similar structures. By cooling liquid water along the water/Ih melting line a high density amorphous phase was also generated.

Journal Article↗

Amorphous ice: stepwise formation of very-high-density amorphous ice from low-density amorphous ice at 125 K.

On compressing low-density amorphous ice (LDA) at 125 K up to 1.6 GPa, two distinct density steps accompanied by heat evolution are observable in pressure-density curves. Samples recovered to 77 K and 1 bar after the first and second steps show the x-ray diffraction pattern of high-density amorphous ice (HDA) and very HDA (VHDA), respectively. The compression of the once formed HDA takes place linearly in density up to 0.95 GPa, where nonlinear densification and HDA --> VHDA conversion is initiated. This implies a stepwise formation process LDA--> HDA --> VHDA at 125 K, which is to the best of our knowledge the first observation of a stepwise amorphous-amorphous-amorphous transformation sequence. We infer that the relation of HDA and VHDA is very similar to the relation between LDA and HDA except for a higher activation barrier between the former. We discuss the two options of thermodynamic versus kinetic origin of the phenomenon.

Journal Article↗

Ice-active characteristics of soil bacteria selected by ice-affinity.

As an initial screen for microorganisms that produce ice-active macromolecules, ice-affinity was used to select microorganisms from soil consortia originating from three temperate regions. Once selected and subsequently purified to single colonies, these microbes were putatively identified by 16S ribosomal RNA sequencing and assayed for various ice-active properties. Ice-affinity selection appeared to select for bacteria with ice-associating activities: inhibition of ice recrystallization; ice nucleation; ice shaping. Although none of these activities were observed in Paenibacillus amyloliticus C8, others such as Chryseobacterium sp. GL8, demonstrated both ice recrystallization inhibition and ice-shaping activities. Pseudomonas borealis DL7 was classified as a type I ice nucleator, Flavobacterium sp. GL7, was identified as a type III ice nucleator and Acinetobacter radioresistens DL5 demonstrated ice recrystallization inhibition. In all, 19 different culturable bacteria were selected from the thousands of microbes in late-summer collected soil samples. Many of the selected microbes have been previously reported in glacial ice cores or polar sea ice, and of five isolates that were further characterized, four showed ice-associating activities. These results indicate the significant potential of ice-affinity selection even with temperate climate soils, suggesting that sampling in more extreme and remote areas is not required for the isolation of ice-active bacteria.

Acinetobacter↗

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.

Antarctic Regions↗

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 degrees 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. warm ice nucleus-deficient 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 polypeptide. 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.

Amino Acid Sequence↗

Safety in Canadian junior ice hockey: the association between ice surface size and injuries and aggressive penalties in the Ontario Hockey League.

OBJECTIVE: To investigate the associations between ice surface size and injuries and aggressive penalties in Canadian junior hockey. DESIGN: Injury (all injuries and neurotraumas) and penalty data (aggressive and nonaggressive) were categorized into the ice surface size on which they occurred: larger than standard (LTS), standard (S), and smaller than standard (STS). PARTICIPANTS: There were 328 injury records and 538 penalty records collected for all 16 teams in the Ontario Hockey League (OHL) during the 1993-94 season. The OHL is a junior A league comprised of amateur players aged approximately 16-20 years. MAIN OUTCOME MEASURE: In the absence of any evidence, the null hypotheses of no association between injuries and ice surface size and penalties and ice surface size were tested. RESULTS: The rates of injury per game were inversely related to ice surface sizes (95% confidence intervals: LTS, 0.33 +/- 0.20; S: 0.58 +/- 0.08; and STS, 0.76 +/- 0.06). The associations for all of the paired comparisons of these rates with ice surface size were statistically significant (p < 0.01). Neurotraumas per game and aggressive penalty rates showed no significant relationship with ice surface size (p < 0.05). CONCLUSIONS: It was concluded that ice surface size is a risk factor to consider in assessing overall injury rate. The larger the ice surface is, the lower is the rate of injury. It appears that the medical community was correct in suspecting ice surface size as a factor in creating a safer environment for ice hockey players. Penalty data do not appear to be important factors in relation to ice surface size.

Adolescent↗

Sea Ice Microbial Communities: Distribution, Abundance, and Diversity of Ice Bacteria in McMurdo Sound, Antarctica, in 1980.

An abundant and diverse bacterial community was found within brine channels of annual sea ice and at the ice-seawater interface in McMurdo Sound, Antarctica, in 1980. The mean bacterial standing crop was 1.4 x 10 cells m (9.8 mg of C m); bacterial concentrations as high as 1.02 x 10 cells m were observed in ice core melt water. Vertical profiles of ice cores 1.3 to 2.5 m long showed that 47% of the bacterial numbers and 93% of the bacterial biomass were located in the bottom 20 cm of sea ice. Ice bacterial biomass concentration was more than 10 times higher than bacterioplankton from the water column. Scanning electron micrographs showed a variety of morphologically distinct cell types, including coccoid, rod, fusiform, filamentous, and prosthecate forms; dividing cells were commonly observed. Approximately 70% of the ice bacteria were free-living, whereas 30% were attached to either living algal cells or detritus. Interactions between ice bacteria and microalgae were suggested by a positive correlation between bacterial numbers and chlorophyll a content of the ice. Scanning and transmission electron microscopy revealed a close physical association between epibacteria and a dominant ice alga of the genus Amphiprora. We propose that sea ice microbial communities are not only sources of primary production but also sources of secondary microbial production in polar ecosystems. Furthermore, we propose that a detrital food web may be associated with polar sea ice.

Journal Article↗

IL-1 beta-converting enzyme (ICE) is present and functional in human alveolar macrophages: macrophage IL-1 beta release limitation is ICE independent.

Tissue macrophages readily produce intracellular pro-IL-1beta in response to stimuli such as LPS, but are limited in mature IL-1beta release compared with blood monocytes. The mechanism of this IL-1beta control may provide important insights into the physiology of IL-1beta at the tissue level. Since it has been hypothesized that IL-1beta processing by the IL-1beta-converting enzyme (ICE) regulates IL-1beta release, we compared human alveolar macrophages and human blood monocytes for relative ICE expression and activation. Using immunoblots and enzyme-linked immunoassay for ICE, we demonstrate that alveolar macrophages do not differ from blood monocytes in antigenic p45 ICE. Furthermore, an indirect assay for functional ICE documents similar ICE activities in both monocytes and alveolar macrophages, i.e., similar concentrations of soluble synthetic ICE inhibitor (IC50 values of 0.3 +/- 0.01 and 0.6 +/- 0.2 microM, respectively) are required to block mature IL-1beta generation. However, as has been reported for THP-1 myelomonocytic cells, neither alveolar macrophages nor blood monocytes contain directly quantifiable levels of functional ICE forms (p22/p20 and p10) when assayed by immunoblots or by a sensitive capture ELISA that uses an irreversible, biotinylated ICE inhibitor. These findings document that the macrophage limitation in mature IL-1beta release is not due to a lack of ICE or to an inability to activate ICE. Finally, using a staged release assay, the time to half-maximum mature IL-1beta release is significantly depressed in macrophages compared with that in monocytes. Taken together, these findings suggest that macrophage IL-1beta export is regulated independently of ICE activation.

Adenosine Triphosphate↗

Comparison of plain ice and flavoured ice for preventing oral mucositis associated with the use of 5 fluorouracil.

AIMS AND OBJECTIVES: The study aimed to compare the use of plain ice, flavoured ice and standard care, to evaluate the effect on mucositis and to determine patients' perceptions of the two forms of oral cryotherapy. BACKGROUND: Despite evidence that oral cryotherapy is useful in preventing mucositis in patients receiving 5-fluorouracil, concerns have been expressed about its clinical utility, due to potential side effects and negative perceptions. DESIGN: A randomized, controlled, crossover trial was conducted in the outpatient chemotherapy department of an acute care teaching hospital in Perth, Western Australia. Patients were randomized to receive each of three interventions across three cycles of chemotherapy: standard care alone; standard care plus plain ice; and standard care plus flavoured ice. METHODS: Oral mucositis was assessed by nurses prior to each of the three chemotherapy cycles and 15 days after each intervention. Two assessment tools were used, the Oral Assessment Guide, and the Western Consortium Cancer Nursing Research Scale. Participants completed a questionnaire to determine their comfort and satisfaction with oral cryotherapy, as well as factors affecting compliance. RESULTS: Findings from 67 patients revealed that when participants used standard care alone, they were significantly more likely to experience symptoms of mucositis than when they used either plain or flavoured ice. Odds ratios were at least threefold higher for standard care alone, varying according to the instrument used. The two main concerns reported were the taste of flavoured ice and the time required to complete the cryotherapy interventions. Side effects such as nausea, sensitivity and headache were reported more frequently for flavoured ice (n = 11) compared with plain ice (n = 5) and standard care (n = 1). CONCLUSIONS: Both forms of oral cryotherapy were effective in reducing the severity of oral mucositis after chemotherapy and were more effective than standard care alone. Flavoured ice was associated with the highest frequency of side effects. RELEVANCE TO CLINICAL PRACTICE: The benefits of cryotherapy appear to outweigh the problems in this sample of patients. The intervention should be tailored to individual patients, based on preferences for plain versus flavoured ice and small chips vs. larger blocks. Unsweetened frozen fruit juices should be evaluated. Time constraints could be addressed by providing transportable containers of ice.

Antimetabolites, Antineoplastic↗