Trehalose uptake and dehydration effects on the cryoprotection of CHO–K1 cells expressing TRET1

Chinese hamster ovary cells (CHO–K1 cells) in which the trehalose transporter (TRET1) is expressed can have greater cryoprotection than ordinary CHO–K1 cells. This study examines the uptake characteristics of trehalose into cells via TRET1 and determines the influence of intracellular trehalose on the freeze–thaw viabilities. In our experiments, the intracellular trehalose concentration is controlled by the extracellular trehalose concentration and the immersion time in a freezing solution. In this freezing solution, both kinds of CHO–K1 cells are independently dispersed with various amount of trehalose, and then put into the CO₂ incubator for 0–6 h. After a set immersion time, the cell-suspended sample is cooled to 193 K, stored for 1 week, then quickly thawed at 310 K and its viability measured. The uptake amount of intracellular trehalose is measured before freezing. We find an upper limit for the uptake amount of trehalose when the extracellular trehalose concentration is about 400 mM, at which the freeze–thaw viability is the highest. When the extracellular trehalose concentration exceeds 400 mM, shorter immersion times are needed to obtain the maximum freeze–thaw viability. Also, longer immersion weakens the cells. Our analyses indicate that when the extracellular trehalose-concentration is less than 400 mM, the trehalose uptake occurs more slowly with less dehydration, resulting in less stress on the cell. When the extracellular trehalose concentration exceeds the saturation level, the cell is stressed by the excess dehydration due to the remaining osmotic pressure, with apoptosis occurring before freezing.     

High arctic heath soil respiration and biogeochemical dynamics during summer and autumn freeze‐in – effects of long‐term enhanced water and nutrient supply

In High Arctic NE Greenland, temperature and precipitation are predicted to increase during this century, however, relatively little information is available on the role of increased water supply on soil CO ₂ efflux in dry, high arctic ecosystems. We measured soil respiration (R_soil) in summer and autumn of 2009 in combination with microbial biomass and nutrient availability during autumn freeze‐in at a dry, open heath in Zackenberg, NE Greenland. This tundra site has been subject to fully factorial manipulation consisting of increased soil water supply for 14 years, and occasional nitrogen (N) addition in pulses. Summer watering enhanced R_soil during summer, but decreased R_soil in the following autumn. We speculate that this is due to intensified depletion of recently fixed plant carbon by soil organisms. Hence, autumn soil microbial activity seems tightly linked to growing season plant production through plant‐associated carbon pools. Nitrogen addition alone consistently increased R_soil, but when water and nitrogen were added in combination, autumn R_soil declined similarly to when water was added alone. Despite several freeze‐thaw events, the microbial biomass carbon (C) remained constant until finally being reduced by ~60% in late September. In spite of significantly reduced microbial biomass C and phosphorus (P), microbial N did not change. This suggests N released from dead microbes was quickly assimilated by surviving microbes. We observed no change in soil organic matter content after 14 years of environmental manipulations, suggesting high ecosystem resistance to environmental changes.     

Shifts of tundra bacterial and archaeal communities along a permafrost thaw gradient in Alaska

Understanding the response of permafrost microbial communities to climate warming is crucial for evaluating ecosystem feedbacks to global change. This study investigated soil bacterial and archaeal communities by Illumina MiSeq sequencing of 16S rRNA gene amplicons across a permafrost thaw gradient at different depths in Alaska with thaw progression for over three decades. Over 4.6 million passing 16S rRNA gene sequences were obtained from a total of 97 samples, corresponding to 61 known classes and 470 genera. Soil depth and the associated soil physical–chemical properties had predominant impacts on the diversity and composition of the microbial communities. Both richness and evenness of the microbial communities decreased with soil depth. Acidobacteria, Verrucomicrobia, Alpha‐ and Gamma‐Proteobacteria dominated the microbial communities in the upper horizon, whereas abundances of Bacteroidetes, Delta‐Proteobacteria and Firmicutes increased towards deeper soils. Effects of thaw progression were absent in microbial communities in the near‐surface organic soil, probably due to greater temperature variation. Thaw progression decreased the abundances of the majority of the associated taxa in the lower organic soil, but increased the abundances of those in the mineral soil, including groups potentially involved in recalcitrant C degradation (Actinomycetales, Chitinophaga, etc.). The changes in microbial communities may be related to altered soil C sources by thaw progression. Collectively, this study revealed different impacts of thaw in the organic and mineral horizons and suggests the importance of studying both the upper and deeper soils while evaluating microbial responses to permafrost thaw.     

Permafrost collapse alters soil carbon stocks,respiration, CH4, and N2O in upland tundra

Release of greenhouse gases from thawing permafrost is potentially the largest terrestrial feedback to climate change and one of the most likely to occur; however, estimates of its strength vary by a factor of thirty. Some of this uncertainty stems from abrupt thaw processes known as thermokarst (permafrost collapse due to ground ice melt), which alter controls on carbon and nitrogen cycling and expose organic matter from meters below the surface. Thermokarst may affect 20–50% of tundra uplands by the end of the century; however, little is known about the effect of different thermokarst morphologies on carbon and nitrogen release. We measured soil organic matter displacement, ecosystem respiration, and soil gas concentrations at 26 upland thermokarst features on the North Slope of Alaska. Features included the three most common upland thermokarst morphologies: active‐layer detachment slides, thermo‐erosion gullies, and retrogressive thaw slumps. We found that thermokarst morphology interacted with landscape parameters to determine both the initial displacement of organic matter and subsequent carbon and nitrogen cycling. The large proportion of ecosystem carbon exported off‐site by slumps and slides resulted in decreased ecosystem respiration postfailure, while gullies removed a smaller portion of ecosystem carbon but strongly increased respiration and N₂O concentration. Elevated N₂O in gully soils persisted through most of the growing season, indicating sustained nitrification and denitrification in disturbed soils, representing a potential noncarbon permafrost climate feedback. While upland thermokarst formation did not substantially alter redox conditions within features, it redistributed organic matter into both oxic and anoxic environments. Across morphologies, residual organic matter cover, and predisturbance respiration explained 83% of the variation in respiration response. Consistent differences between upland thermokarst types may contribute to the incorporation of this nonlinear process into projections of carbon and nitrogen release from degrading permafrost.     

Kinetics for glutamine-synthetase inhibition by phosphinothricin and measurement of other enzyme activities in situ in isolated asparagus cells using a freeze-thaw technique

Kinetics for the inhibition of glutamine synthetase (EC 6.3.1.2) in situ by the herbicidal glutamate analogue, phosphinothricin, have been generated, and produce an inhibitor dissociation constant (K_i) of 6.5 M. This has been achieved through the development of a rapid technique for the isolation of mesophyll cells from the cladophylls of young asparagus (Asparagus sprengeri) plants to provide starting material for the direct measurement of enzyme activities in situ. A modification of the technique developed by Rhodes and Stewart (Planta 118, 133–144 (1974) for the direct determination of enzyme activities in higher-plant tissues has been applied to these asparagus cells. Treatment of the cells by a single freezing in liquid nitrogen for a very short period (10 s), followed by thawing, alters the permeability of cell and organelle membranes allowing enzymes to become accessible to many small molecules, and yet remain concentrated and active within the cell. The activities of enzymes known to be located specifically in the organelles as well as the cytoplasm can be measured in asparagus cells treated in this way. Comparisons have been made between the activity and inhibition of glutamine synthetase in situ, and the enzyme isolated and partially purified from asparagus cells by fast protein liquid chromatography. Similarities in K_m and K_i values obtained between these two emphasize the efficacy of the freeze-thaw technique. There is only a single glutamine-synthetase isoenzyme in asparagus mesophyll cells, which copurifies with the one normally associated with the chloroplast (GS2).Abbreviation FPLC fast protein liquid chromatography     

Identification and classification of genes required for tolerance to freeze-thaw stress revealed by genome-wide screening of Saccharomyces cerevisiae deletion strains

Yeasts used in bread making are exposed to freeze-thaw stress during frozen-dough baking. To clarify the genes required for freeze-thaw tolerance, genome-wide screening was performed using the complete deletion strain collection of diploid Saccharomyces cerevisiae. The screening identified 58 gene deletions that conferred freeze-thaw sensitivity. These genes were then classified based on their cellular function and on the localization of their products. The results showed that the genes required for freeze-thaw tolerance were frequently involved in vacuole functions and cell wall biogenesis. The highest numbers of gene products were components of vacuolar H(+)-ATPase. Next, the cross-sensitivity of the freeze-thaw-sensitive mutants to oxidative stress and to cell wall stress was studied; both of these are environmental stresses closely related to freeze-thaw stress. The results showed that defects in the functions of vacuolar H(+)-ATPase conferred sensitivity to oxidative stress and to cell wall stress. In contrast, defects in gene products involved in cell wall assembly conferred sensitivity to cell wall stress but not to oxidative stress. Our results suggest the presence of at least two different mechanisms of freeze-thaw injury: oxidative stress generated during the freeze-thaw process, and defects in cell wall assembly.     

Impact of freezing on pH of buffered solutions and consequences for monoclonal antibody aggregation

Freezing of biologic drug substance at large scale is an important unit operation that enables manufacturing flexibility and increased use‐period for the material. Stability of the biologic in frozen solutions is associated with a number of issues including potentially destabilizing pH changes. The pH changes arise from temperature‐associated change in the pK_as, solubility limitations, eutectic crystallization, and cryoconcentration. The pH changes for most of the common protein formulation buffers in the frozen state have not been systematically measured. Sodium phosphate buffer, a well‐studied system, shows the greatest change in pH when going from +25 to ?30°C. Among the other buffers, histidine hydrochloride, sodium acetate, histidine acetate, citrate, and succinate, less than 1 pH unit change (increase) was observed over the temperature range from +25 to ?30°C, whereas Tris‐hydrochloride had an ～1.2 pH unit increase. In general, a steady increase in pH was observed for all these buffers once cooled below 0°C. A formulated IgG2 monoclonal antibody in histidine buffer with added trehalose showed the same pH behavior as the buffer itself. This antibody in various formulations was subject to freeze/thaw cycling representing a wide process (phase transition) time range, reflective of practical situations. Measurement of soluble aggregates after repeated freeze–thaw cycles shows that the change in pH was not a factor for aggregate formation in this case, which instead is governed by the presence or absence of noncrystallizing cryoprotective excipients. In the absence of a cryoprotectant, longer phase transition times lead to higher aggregation. © 2009 American Institute of Chemical Engineers Biotechnol. Prog., 2010     

Protection of osteoblastic cells from freeze/thaw cycle-induced oxidative stress by green tea polyphenol

Green tea polyphenol (GTP) together with dimethylsulphoxide (DMSO) were added to a freezing solution of osteoblastic cells (rat calvarial osteoblasts and human osteosarcoma cells) exposed to repeated freeze/thaw cycles (FTC) to induce oxidative stress. When cells were subjected to 3 FTCs, freezing medium containing 10% (v/v) DMSO and 500 μg GTP ml⁻¹ significantly (p < 0.05) suppressed cell detachment and growth inhibition by over 63% and protected cell morphology. Furthermore, the alkaline phosphatase activity of osteoblastic cells was appreciably maintained after 2 and 3 FTCs in this mixture. Polyphenols may thus be of use as a cell cryopreservant and be advantageous in such fields as cell transplantation and tissue engineering.     

Short‐ and long‐term effects on mAb‐producing CHO cell lines after cryopreservation

Cryopreservation provides the foundation for research, development, and manufacturing operations in the CHO‐based biopharmaceutical industry. Despite its criticality, studies are lacking that explicitly demonstrate that the routine cell banking process and the potential stress and damage during cryopreservation and recovery from thaw have no lasting detrimental effects on CHO cells. Statistics are also scarce on the decline of cell‐specific productivity (Q_p) over time for recombinant CHO cells developed using the glutamine synthetase (GS)‐based methionine sulfoximine (MSX) selection system. To address these gaps, we evaluated the impact of freeze‐thaw on 24 recombinant CHO cell lines (generated by the GS/MSX selection system) using a series of production culture assays. Across the panel of cell lines expressing one of three monoclonal antibodies (mAbs), freeze‐thaw did not result in any significant impact beyond the initial post‐thaw passages. Production cultures sourced from cryopreserved cells and their non‐cryopreserved counterparts yielded similar performance (growth, viability, and productivity), product quality (size, charge, and glycosylation distributions), and flow cytometric profiles (intracellular mAb expression). However, many production cultures yielded lower Q_p at increased cell age: 17 of the 24 cell lines displayed ≥20% Q_p decline after ～2–3 months of passaging, irrespective of whether the cells were previously cryopreserved. The frequency of Q_p decline underscores the continued need for understanding the underlying mechanisms and for careful clone selection. Because our experiments were designed to decouple the effects of cryopreservation from those of cell age, we could conclusively rule out freeze‐thaw as a cause for Q_p decline. © 2018 American Institute of Chemical Engineers Biotechnol. Prog., 34:463–477, 2018     

Advanced hepatic tissue destruction in ablative cryosurgery: potentials of intermittent freezing and selective vascular inflow occlusion

Recent studies indicate that cryosurgery represents a promising approach to treat non-resectable liver tumors. To improve parenchymal tissue destruction, a variety of modifications of the freeze-thaw procedure have been suggested, including repetitive freezing and portal-triad cross-clamping. The aim of the present study was to analyze whether intermittent freezing by application of a double freeze-thaw procedure or selective vascular inflow occlusion are more effective than a single freeze-thaw cycle to achieve complete hepatic tissue destruction. Using a porcine model, intrahepatic cryolesions were induced by freezing the hepatic tissue for a total of 15 min (n=6, SF). Additional animals (n=6) underwent a double freeze-thaw cycle of 7.5 min each (DF). A third group of animals (n=6) was treated by a single 15-min freeze-thaw cycle during selective vascular inflow occlusion (VO-SF). Seven days after freezing, DF did not change the volume of the cryolesion (25.4+/-1.7 cm(3)) compared to SF (29.9+/-3.7 cm(3)), however, resulted in enhanced destruction of hepatocyte nuclear morphology (DF-score: 2.4+/-0.2 versus SF-score: 1.1+/-0.3; p<0.05) and attenuated leukocyte infiltration within the margin of the cryolesion (DF-score: 1.5+/-0.2 versus SF-score: 2.8+/-0.1; p<0.05). VO-SF was also effective to significantly enhance destruction of hepatocyte nuclear morphology (2.8+/-0.1; p<0.05 versus SF), but, additionally, markedly increased the volume of the cryolesions (43.3+/-5.3 cm(3); p<0.05 versus SF and DF). Interestingly, VO-SF further increased the number of apoptotic cells, while leukocyte infiltration (2.3+/-0.3) was not affected compared to that after SF-treatment. Thus, our data indicate that both DF and VO-SF are effective to enhance parenchymal cell destruction within the margin of the cryolesion. VO-SF additionally increases the volume of the lesion and may therefore be most attractive for successful clinical application.