A separation chamber to sort cells and cell organelles by weak physical forces: III. Preparative electrophoresis of cells in stationary density gradients at low electric field strength

An apparatus was designed for preparative density gradient electrophoresis of mammalian cells. In a low conductivity isotonic Ficoll density gradient of 1.5 cm length, human erythrocytes treated with neuraminidase were separated from untreated erythrocytes at an electric field strength of approximately 2.7 v/cm. Within 5 min two bands of erythrocytes were visible. Electrophoretic separation was completed within 25 min. The fractionation is performed in a design consisting of three Perspex circular plates, bottom and top plates of which can be displaced simultaneously relative to the stationary middle plate by a worm-gear mechanism. The middle plate contains a cylindrical separation chamber of 50 cm² and 1.5 cm high. Top and bottom plates contain cones and flow deflectors for the undisturbed thin layering of cell suspensions and for introduction of the density gradient. Also present in top and bottom plates are electrode compartments containing a large platinum electrode and a cellophane membrane that isolates the separation chamber hydrodynamically but not electrically from the electrode compartment. The electrode compartments were flushed with electrophoresis buffer to remove products of electrophoresis as well as the (low) generated Joule heat.     

A hydrological tracer study of water uptake depth in a Scots pine forest under two different water regimes

Little is known about the vertical distribution of water uptake by trees under different water supply regimes, the subject of this study, conducted in a Scots pine stand on sandy loam in northern Sweden. The objective was to determine the water uptake distribution in pines under two different water regimes, desiccation (no precipitation) and irrigation (2?mm day^?1 in July and 1?mm day^?1 in August), and to relate the uptake to water content, root and soil texture distributions. The natural ¹⁸O gradient in soil water was exploited, in combination with two added tracers, ²H at 10?cm and ³H at 20?cm depth. Extraction of xylem sap and water from the soil profile then enabled evaluation of relative water uptake from four different soil depths (humus layer, 0–10, 10–25 and 25–55?cm) in each of two 50-m² plots per treatment. In addition, water content, root biomass and soil texture were determined. There were differences in vertical water uptake distribution between treatments. In July, the pines at the irrigated and desiccated plots took up 50% and 30%, respectively, of their water from the upper layers, down to 25?cm depth. In August, the pines on the irrigated plots took up a greater proportion of their water from layers below 25?cm deep than they did in July. In a linear regression, the mean hydraulic conductivity for each mineral soil horizon explained a large part of the variation in relative water uptake. No systematic variation in the residual water uptake correlated to the root distribution. It was therefore concluded that the distribution of water uptake by the pines at Åheden was not a function of root density in the mineral soil, but was largely determined by the unsaturated hydraulic conductivity.     

A rapid method for seperation and identification of several hexuronic acids and hexuronic acid-containing oligosaccharides.

Five naturally occurring hexuronic acids and several hexuronic acid-containing oligosaccharides were separated and identified by high voltage paper electrophoresis, using one of the following buffers. (i) Pyridine-acetic acid-water (1:10:89, by volume), the pH of which was adjusted to 2.3–3.5 with 98% formic acid. (ii) Pyridine-water (1:90, by volume), the pH of which was adjusted to 3.5–4.0 with glacial acetic acid. The best separation of the five hexuronic acids and heparin disaccharides was observed at pH 2.7 after electrophoresis for 180 min at 100 V/cm. At pH 3 l-gulosyluronic acid-l-guluronic acid could be easily isolated from an acid hydrolysate of alginate by the present method.     

Adding Fe0 powder to enhance the anaerobic conversion of propionate to acetate

Propionate is an unfavorable substrate for the anaerobic digestion because it is thermodynamically difficult to be decomposed into acetate. An attempt to enhance the decomposition of propionate by adding Fe⁰ powder (10 g) into an acidogenic reactor (A1) with propionate as the sole carbon source was made in this study. The results showed that the propionate conversion rate (67–89%) in A1 were higher than that in a reference reactor (43–77%) without dosing of Fe⁰ (A2). The enhanced conversion of propionate caused both chemical oxygen demand removal (COD) (57–79%) and acetate production (178–328 mg/L) in A1 to increase significantly. Although Fe⁰ contributed the H₂ production chemically, the H₂ content of A1 was less than that of A2. The reason was ascribed to the enhanced utilization of H₂ for the homoacetogenesis. It was calculated that the Gibbs free energy in the decomposition of propionate was decreased by about 8.0–10.2% with the dosing of Fe⁰. Also, the activities of enzymes related to the acetogenesis were enhanced by 2–34-folds. Fluorescence in situ hybridization (FISH) and denaturing gradient gel electrophoresis (DGGE) analysis indicated that Fe⁰ increased the abundance of microbial communities, especially propionate-utilizing bacteria and homoacetogenic bacteria.     

Preparative cell electrophoresis with D2O as a stabilizing agent.

The method of ascending preparative cell electrophoresis in a nonstabilized vertical column can be greatly improved by layering the cells on a starting cushion of buffer prepared in D2O and by stabilizing the liquid column above it with a D2O gradient. D2O/H2O mixtures have no apparent biochemical effects on the cells, and their physiochemical effects are short-lived and reversible. It was possible, by this method, to separate a mixture of glutaraldehyde-fixed erythrocytes of three species (rabbit, horse and chicken) into three distinct zones after 15 minutes of electrophoresis. It was also possible to obtain an enriched human lymphocyte fraction containing 96% T-cells, after 1 hour of electrophoresis.     

Flood effects on invertebrates, sediments and particulate organic matter in the hyporheic zone of a gravel-bed stream

1. We investigated the effects of a flood on the fauna and physical habitat of the hyporheic zone of the Kye Burn, a fourth order gravel‐bed stream in New Zealand. 2. Freeze core hyporheic samples (to 50 cm depth) and benthic samples (to 10 cm) were taken, along with measurements of vertical hydrological gradient, before, 2 days after and 1 month after the flood (estimated return period: 1.5 years, estimated Q_max = 10.4 m³ s^?1). 3. The composition of the hyporheos differed over the three sampling occasions with fewer taxa collected immediately postflood than preflood. The equitability of the community was higher on both postflood occasions, consistent with the reduced densities of two abundant taxa (Leptophlebiidae and Copepoda). 4. Total invertebrate abundance was lower on the postflood occasions than preflood in both benthic (0–10 cm) and hyporheic (10–50 cm) sediments. Several taxa, including asellotan isopods and amphipods, recovered within 1 month of the event. Hyporheic densities of larval Hydora and nematodes did not differ among the three sampling occasions, but the water mite Pseudotryssaturus was more abundant 1 month after the flood than preflood. There was no evidence of vertical movements (to 50 cm) by any taxa in response to the flood. 5. The proportion of fine sediments (<1 mm) in the subsurface sediments (10–50 cm) increased over the three sampling occasions and median particle size declined, but sediment porosity did not change. More particulate organic matter was found in the sediments after the flood. 6. Our study provides little evidence that the hyporheic zone (to 50 cm) acted as a significant refuge during the flood event, although movements to or recolonisation from sediments deeper than 50 cm could explain the recovery of many crustacean and mite taxa within 1 month.     

Trehalase from the cellular slime mold Dictyostelium discoideum: Purification and characterization of the homogeneous enzyme from myxamoebae

Trehalase (α-α′-trehalose 1-d-glucohydrolase, EC 3.2.1.28) was solubilized from myxamoebae of the cellular slime mold Dictyostelium discoideum by a freeze-thaw cycle and was subsequently purified to homogeneity using the techniques of ethanol fractionation, molecular sieve chromatography, DEAE-cellulose ion-exchange chromatography, chromatofocusing, and preparative polyacrylamide disc gel electrophoresis. The 1000-fold purified enzyme had a specific activity of about 104 units/mg, which was accompanied by a net recovery of 5 to 7% of the original activity. The purified enzyme was maximally active at pH 5.5, showed high specificity for trehalose, and exhibited a typical hyperbolic response as a function of trehalose concentration with a K_m of 1.2 mm. The enzyme was maximally active at 50 °C and had an energy of activation of 12–13 kcal/mol. Thermal stability studies demonstrated that full enzymatic activity was recovered following a 5-min incubation of trehalase at temperatures up to 45–50 °C. Analysis of various compounds for inhibitory effects indicated that Tris and urea were slightly effective, reducing enzymatic activity by 28 and 6% at concentrations of 100 and 10 mm, respectively. Of five heavy metals tested, HgCl₂ was the most inhibitory, reducing activity by 58% when present at a final concentration of 1.0 mm. Enzymatic activity was not affected by any adenine derivative examined (e.g., ATP, ADP, AMP, cAMP, adenosine, and adenine). The molecular weight of the native enzyme was determined by molecular sieve chromatography, pore gradient electrophoresis, and electrophoresis as a function of acrylamide concentration. All three methods yielded a value of about 10⁵ ± 5 × 10³. Estimation of the subunit or monomer molecular weight by sodium dodecyl sulfate-gel electrophoresis indicated a value of 95–100 × 10³. The isoelectric point as determined in 7.5% polyacrylamide gels with pH 3–10 ampholytes was 7.2–7.3. The purified enzyme adsorbed to concanavalin A-Sepharose in the presence of KCl (0.1 m) and was eluted with α-methylmannoside, thereby suggesting an association between trehalase and carbohydrate. In agreement with this conclusion was the observation that trehalase could be specifically stained for carbohydrate with the Alcian blue and periodic acid-Schiff's reagents following polyacrylamide disc gel electrophoresis.     

Vertical distribution, biomass, production and turnover of fine roots along a topographical gradient in a sandy shrubland

In an artificial Salix gordejevii Chang et Skv. plantation of the Horqin sandy land, we investigated vertical distribution (in 0–100 cm depth), biomass (FRD), fine root production (FRP), fine root length density (FRLD) and turnover of fine roots (<2 mm diameter) at three sites (dune top, midslope and bottom of dune) along leeward slopes. Meanwhile, the correlation between FRP and soil available resources was analyzed. Our results indicate that more than 65% of total fine root biomass is distributed in 0–40 cm depth, and the patterns are different at three sites. The mean monthly FRD ranges from 227 to 324 g·m^?2, and they follows the order: dune top > midslope > bottom of dune. Ingrowth cores were harvested after 2, 3, 4, 5, 6 and 8 months of installation. At the first five sampling times, FRP and FRLD (0–40 cm) follows the same order with FRD along the topographical gradient, while FRP harvested after 8 months does not follow the same tendency, they are 348, 402 and 356 g·cm^?2 in dune top, midslope and bottom of dune, respectively. Fine root turnover ranges from 1.04–1.92 year^?1, and fine root turnover (20–40 cm) increases from dune top to bottom of dune along the topographical gradient. Correlation analysis between FRP and soil available resources indicates that only mean soil volumetric water content significantly correlates with annual FRP, which suggests that soil water content might be more crucial for shrub growth than fertility along the topographical gradient.     

Diversity and vertical distribution of magnetotactic bacteria along chemical gradients in freshwater microcosms

The vertical distribution of magnetotactic bacteria along various physico-chemical gradients in freshwater microcosms was analyzed by a combined approach of viable cell counts, 16S rRNA gene analysis, microsensor profiling and biogeochemical methods. The occurrence of magnetotactic bacteria was restricted to a narrow sediment layer overlapping or closely below the maximum oxygen and nitrate penetration depth. Different species showed different preferences within vertical gradients, but the largest proportion (63-98%) of magnetotactic bacteria was detected within the suboxic zone. In one microcosm the community of magnetotactic bacteria was dominated by one species of a coccoid "Alphaproteobacterium", as detected by denaturing gradient gel electrophoresis in sediment horizons from 1 to 10 mm depth. Maximum numbers of magnetotactic bacteria were up to 1.5 x 10(7) cells/cm3, which corresponded to 1% of the total cell number in the upper sediment layer. The occurrence of magnetotactic bacteria coincided with the availability of significant amounts (6-60 microM) of soluble Fe(II), and in one sample with hydrogen sulfide (up to 40 microM). Although various trends were clearly observed, a strict correlation between the distribution of magnetotactic bacteria and individual geochemical parameters was absent. This is discussed in terms of metabolic adaptation of various strains of magnetotactic bacteria to stratified sediments and diversity of the magnetotactic bacterial communities.     

产热凝胶土壤杆菌ATCC31749蛋白质组双向电泳图谱的构建

建立了热凝胶生产茵土壤杆茵茵体总蛋白的蛋白质提取方法和双向电泳方案,确定了使用蛋白质裂解液(7 mol/L尿素,2 mol/L硫脲,1%ASB-14去垢剂,40 mmol/L Tris,0.001%溴酚蓝,1 mmol/L EDTA,1%TBP和1%两性电解质)结合超声破碎法来提取茵体总蛋白的方案为最佳,选择17 cm...     

Soil charcoal as long‐term pyrogenic carbon storage in Amazonian seasonal forests

Forest fires (paleo + modern) have caused charcoal particles to accumulate in the soil vertical profile in Amazonia. This forest compartment is a long‐term carbon reservoir with an important role in global carbon balance. Estimates of stocks remain uncertain in forests that have not been altered by deforestation but that have been impacted by understory fires and selective logging. We estimated the stock of pyrogenic carbon derived from charcoal accumulated in the soil profile of seasonal forest fragments impacted by fire and selective logging in the northern portion of Brazilian Amazonia. Sixty‐nine soil cores to 1‐m depth were collected in 12 forest fragments of different sizes. Charcoal stocks averaged 3.45 ± 2.17 Mg ha^?1 (2.24 ± 1.41 Mg C ha^?1). Pyrogenic carbon was not directly related to the size of the forest fragments. This carbon is equivalent to 1.40% (0.25% to 4.04%) of the carbon stocked in aboveground live tree biomass in these fragments. The vertical distribution of pyrogenic carbon indicates an exponential model, where the 0–30 cm depth range has 60% of the total stored. The total area of Brazil's Amazonian seasonal forests and ecotones not altered by deforestation implies 65–286 Tg of pyrogenic carbon accumulated along the soil vertical profile. This is 1.2–2.3 times the total amount of residual pyrogenic carbon formed by biomass burning worldwide in 1 year. Our analysis suggests that the accumulated charcoal in the soil vertical profile in Amazonian forests is a substantial pyrogenic carbon pool that needs to be considered in global carbon models.     

NITRATE UPTAKE BY LAMINARIA LONGICRURIS (PHAEOPHYCEAE)1,2

Laminaria longicrucis De la Pylaie took up exogenous nitrate under both summer and winter conditions. During July and August no NO₃^- was detected in the ambient water or in algal tissues although it was present in both in February. Discs (2.3 cm diam.) of thin blade tissue were incubated with NO₃^- at four temperatures, with and without illumination. Similar values Jor NO₃^- uptake were found for both summer and winter collected plants when measured in light at 0 C. An apparent K of 4–6 μM was recorded for both types of plants; the V_max ranged from 7 to 10 μmol h^-1 g^-1 dry wt measured in ca. 1800 μW cm^-2 of cool-white fluorescent light. Uptake rates at 5 C were 66%, and at 0 C 30% of those for controls run at 15 C. The alga scavenged NO₃- from solutions <0.5 μM. Ammonia did not inhibit NO₃- uptake. Antibiotic pretreatment reduced NO₃- uptake by a maximum of 12%. Nitrite uptake was inhibited in proportion to the concentration of NO₃- in the medium.     

Vertical gradients in regional lung density and perfusion in the supine human lung: the Slinky effect.

In vivo radioactive tracer and microsphere studies have differing conclusions as to the magnitude of the gravitational effect on the distribution of pulmonary blood flow. We hypothesized that some of the apparent vertical perfusion gradient in vivo is due to compression of dependent lung increasing local lung density and therefore perfusion/volume. To test this, six normal subjects underwent functional magnetic resonance imaging with arterial spin labeling during breath holding at functional residual capacity, and perfusion quantified in nonoverlapping 15 mm sagittal slices covering most of the right lung. Lung proton density was measured in the same slices using a short echo 2D-Fast Low-Angle SHot (FLASH) sequence. Mean perfusion was 1.7 +/- 0.6 ml x min(-1) x cm(-3) and was related to vertical height above the dependent lung (slope = -3%/cm, P < 0.0001). Lung density averaged 0.34 +/- 0.08 g/cm3 and was also related to vertical height (slope = -4.9%/cm, P < 0.0001). By contrast, when perfusion was normalized for regional lung density, the slope of the height-perfusion relationship was not significantly different from zero (P = 0.2). This suggests that in vivo variations in regional lung density affect the interpretation of vertical gradients in pulmonary blood flow and is consistent with a simple conceptual model: the lung behaves like a Slinky (Slinky is a registered trademark of Poof-Slinky Incorporated), a deformable spring distorting under its own weight. The greater density of lung tissue in the dependent regions of the lung is analogous to a greater number of coils in the dependent portion of the vertically oriented spring. This implies that measurements of perfusion in vivo will be influenced by density distributions and will differ from excised lungs where density gradients are reduced by processing.     

Natural Electrotransformation of Lightning-Competent Pseudomonas sp. Strain N3 in Artificial Soil Microcosms

The lightning-competent Pseudomonas sp. strain N3, recently isolated from soil, has been used to study the extent of natural electrotransformation (NET) or lightning transformation as a horizontal gene transfer mechanism in soil. The variation of electrical fields applied to the soil with a laboratory-scale lightning system provides an estimate of the volume of soil affected by NET. Based on the range of the electric field that induces NET of Pseudomonas strain N3, the volume of soil, where NET could occur, ranges from 2 to 950 m³ per lightning strike. The influence of DNA parameters (amount, size, and purity) and DNA soil residence time were also investigated. NET frequencies (electrotransformants/recipient cells) ranged from 10⁻⁸ for cell lysate after 1 day of residence in soil to 4 × 10⁻⁷ with a purified plasmid added immediately before the lightning. The electrical field gradient (in kilovolts per cm) also played a role as NET frequencies ranging from 1 × 10⁻⁵ at 2.3 kV/cm to 1.7 × 10⁻⁴ at 6.5 kV/cm.     

Purification and Properties of a Lytic Enzyme from Streptomyces griseus H-402

A lytic enzyme which was capable of lysing cells of Streptococcus mutans was purified from the culture filtrate of Streplomyces griseus H–402 by Amberlite CG–50 treatment, CM-cellulose and hydroxylapatite column chromatographies, and Sephadex G–150 gelfiltration. The lytic enzyme was obtained in a crystalline form which was homogeneous in polyacrylamide gel electrophoresis. The molecular weight was estimated to be 2×10⁴ by the thin-layer gel-filtration method on Sephadex G–75, and 2.3 × 10⁴ by the method of polyacrylamide gel electrophoresis in the presence of sodium dodecyl sulfate. The enzyme was found to be a N-acetylmuramidase whose activity was lost by N-bromosuccinimide as an inhibitor.     

Isolation of plasma membranes from the bovine retinal pigment epithelium

Retinal pigment epithelium plasma membranes have been isolated by differential and density gradient centrifugation of glass-bead-bound, collagenase-treated cells. Electron microscopic evidence indicates that the glass-bead-bound cells were devoid of red blood cells, rod outer segments and other ocular cell contaminants. The plasma membranes were recovered in 4–6 μg/eye yields and purified 10-fold by 5′-nucleotidase and alkaline phosphodiesterase 1, and 6.5-fold by (Na⁺ + K⁺)-ATPase. Plasma membrane purity as measured by covalent labeling of the epithelial cell plasma membrane proteins with p-(diazonium) benzene[³²S]sulfonic acid was 8–19-fold. In purified plasma membranes contamination by mitochondria was undetectable and lysosomal contamination reduced 100-fold, while endoplasmic reticulum was 2-fold enriched. SDS-polyacrylamide gel electrophoresis of the plasma membrane proteins revealed 23–26 major bands by Coomassie blue staining and 12–16 major bands by radioactive labeling. The plasma membranes exhibited a 3-fold lower concentration of docosahexaenoic acid, a 3-fold higher cholesterol/phosphate ratio, and were 10-fold enriched in cholesterol per μg protein when compared to the whole cell fraction. Retinal epithelial plasma membranes contain an average of 1 mol cholesterol per mol of lipid phosphorus, a high palmitic acid concentration (39 mol%) and a low concentration of docosahexaenoic acid (2 mol%). The lipid profile of the retinal pigment epithelial plasma membranes indicates that they are typical of plasma membranes from many other cell types and that they appear to be less fluid than total rod outer segment membranes.     

Preparative Electrophoresis of Human Lymphocytes I. Purification of Non-Immunoglobulin-Bearing Lymphocytes by Electrophoretic Levitation

When 10–30 × 10⁶ human peripheral lymphocytes are electrophoresed in an upward direction in a vertical column for 1 to 1–1/2 hour at 12 V/cm at pH 7.1, the fastest migrating fraction of 3–10 × 10 lymphocytes consists of 98–100%. non-immunoglobulin-bearing lymphocytes, as determined by immunofluorescence with anti-human immunoglobulin conjugate. The method can be applied to fresh human lymphocytes as well as to lymphocytes that have been frozen and thawed and, if glycerol is added to the buffer as a cryoprotectant, the fast “T” cell fraction can be frozen immediately, to be stored for later use. Similar separations can be obtained with lymphocytes from human tonsils.     

Enchytraeid numbers,biomass and respiratory metabolism in a beech woodland - Wytham Woods,Oxford

Summary The mean annual population density of enchytraeids in the litter and upper 6 cm of soil was found to be 14,590 m^-2. Mean individual weights approximated 116, 158 and 151 g wet wt. in the litter, 0–3 cm and 3–6 cm strata respectively. The mean biomass was estimated to be 1.908 g wet wt m^-2. Vertical migration was shown to occur, the upward migration in late Autumn was a response to temperatures in the litter being temporarily higher than those of the 0–3 cm stratum. As a result of upward vertical migration and possibly recruitment, numbers reached a maximum in the litter during Winter. On an annual basis the litter, 0–3 and 3–6 cm strata contained 41.43, 46.44 and 12.12% respectively of the extracted enchytraeids. The equivalent biomass values were 33.18, 52.46 and 14.36%. Total numbers and biomass revealed a general picture of high values in late Autumn to Winter which gradually decreased through Spring and Summer except for a minor peak in May–June. The annual oxygen consumption of the enchytraeids approximated 4.285 l O₂ m^-2 yr^-1 (20.461 kcal85.610 kJ) and accounted for 1.63% of the total soil metabolism. A production/biomass (P/B) ratio of 4.93 was estimated as was a net population efficiency of 32%. For this site the contribution by enchytraeids to total soil respiration is about one-third that of the earthworms and an order of magnitude greater than that of the nematodes.     

Initial differentiation of vertical soil organic matter distribution and composition under juvenile beech (Fagus sylvatica L.) trees

In a lysimeter experiment with juvenile beech trees (Fagus sylvatica L.) we studied the development of depth gradients of soil organic matter (SOM) composition and distribution after soil disturbance. The sampling scheme applied to the given soil layers (0–2 cm, 2–5 cm, 5–10 cm and 10–20 cm) was crucial to study the subtle reformation of SOM properties with depth in the artificially filled lysimeters. Due to the combination of physical SOM fractionation with the application of ¹⁵N-labelled beech litter and ¹³C-CPMAS NMR spectroscopy we were able to obtain a detailed view on vertical differentiation of SOM properties. Four years after soil disturbance a significant decrease of the mass of particulate OM (POM) with depth could be found. A clear depth distribution was also shown for carbon (C) and nitrogen (N) within the SOM fractions related to bulk soil. The mineral fractions <63 µm clearly dominated C storage (between 47 to 60% of bulk soil C) and N storage (between 68 to 86% of bulk soil N). A drastic increase in aliphatic C structures concomitant to decreasing O/N-alkyl C was detected with depth, increasing from free POM to occluded POM. Only a slight depth gradient was observed for ¹³C but a clear vertical incorporation of ¹⁵N from the applied labelled beech litter was demonstrated probably resulting from faunal and fungal incorporation. We clearly demonstrated a significant reformation of a SOM depth profile within a very short time of soil evolution. One important finding of this study is that especially in soils with reforming SOM depth gradients after land-use changes selective sampling of whole soil horizons can bias predictions of C and N dynamics as it overlooks a potential development of gradients of SOM properties on smaller scales.     

Expression of voltage-gated calcium channels augments cell susceptibility to membrane disruption by nanosecond pulsed electric field

We compared membrane permeabilization by nanosecond pulsed electric field (nsPEF) in HEK293 cells with and without assembled CaV1.3 L-type voltage-gated calcium channel (VGCC). Individual cells were subjected to one 300-ns pulse at 0 (sham exposure); 1.4; 1.8; or 2.3 kV/cm, and membrane permeabilization was evaluated by measuring whole-cell currents and by optical monitoring of cytosolic Ca²⁺. nsPEF had either no effect (0 and 1.4 kV/cm), or caused a lasting (>80 s) increase in the membrane conductance in about 50% of cells (1.8 kV/cm), or in all cells (2.3 kV/cm). The conductance pathway opened by nsPEF showed strong inward rectification, with maximum conductance increase for the inward current at the most negative membrane potentials. Although these potentials were below the depolarization threshold for VGCC activation, the increase in conductance in cells which expressed VGCC (VGCC+ cells) was about twofold greater than in cells which did not (VGCC− cells). Among VGCC+ cells, the nsPEF-induced increase in membrane conductance showed a positive correlation with the amplitude of VGCC current measured in the same cells prior to nsPEF exposure. These findings demonstrate that the expression of VGCC makes cells more susceptible to membrane permeabilization by nsPEF. Time-lapse imaging of nsPEF-induced Ca²⁺ transients confirmed permeabilization by a single 300-ns pulse at 1.8 or 2.3 kV/cm, but not at 1.4 kV/cm, and the transients were expectedly larger in VGCC+ cells. However, it remains to be established whether larger transients reflected additional Ca²⁺ entry through VGCC, or were a result of more severe electropermeabilization of VGCC+ cells.