Electrically induced Ca2+ transport across the membrane of Paramecium caudatum measured by means of flow-through technique

Transmembrane calcium fluxes related to excitation were studied in Paramecium caudatum. Radioactive (⁴⁵Ca²⁺) or inactive solution was flowed through a dense suspension of unlabelled or labelled cells, and radioactivity was monitored in the solution. The organisms were electrically stimulated by means of extracellular electrodes. As a result of stimulation Ca²⁺ uptake and release was measured. The uptake response dropped with increasing number of successive stimulation periods and increased with growing stimulus amplitude and duration. Maximum uptake was obtained at 20 V/cm and at least 60 s duration and for temperatures between 10 and 15°C. A Ca²⁺ influx of 700 pmol/1000 cells upon 1 min stimulation was measured at 15°C. This corresponds to an increment of the intraciliary [Ca²⁺] of about $\text{5 · 10}{}^{-4}\text{M}$. Ca²⁺ release was dependent on the stimulus amplitude in a similar manner as was Ca²⁺ uptake. Photographic recordings of the swimming behaviour of the organisms were used to interpret the flux data. At temperatures up to 15°C the cells swam backward perpendicular to the applied electric field of 10 to 20 V/cm. At 25°C they showed forward spiralling movement. For the first time evidence was brought for stimulated Ca²⁺ influx in Paramecium at physiological temperatures. It is concluded from the results that a strong active Ca²⁺ extrusion from the intraciliary space counteracts the influx. The Ca²⁺ pump rate must be at least $\text{8 · 10}{}^{12}$ calcium ions per s per cm² ciliary surface.     

Biochemical studies of the excitable membrane of Paramecium aurelia. I. 45Ca2+ fluxes across resting and excited membrane.

The characteristics of Ca2+ transport across the excitable membrane of Paramecium aurelia were studied by measuring 45Ca2+ influx and efflux. The intracellular concentration of free Ca2+ in resting P. aurelia was at least ten times less than the extracellular concentration. Ca2+ influx was easily measurable at 0 degrees C, but not at 23 degrees C. The influx of 45Ca2+ was stimulated by the same conditions which cause membrane depolarization and ciliary reversal. Addition of Na+ and K+ (which stimulate ciliary reversal) resulted in a 10-fold increase in the rate of Ca2+ influx. An externally applied, pulsed, electric field (1-2 mA/cm2 of electrode surface), caused the rate of Ca2+ influx to increase 3-5 times, with the extent of stimulation dependent on the current density and the pulse width. Ca2+ influx had the characteristics of a passive transport system and was associated with the chemically or electrically triggered Ca2+ "gating" mechanism, which has been studied electrophysiologically. In contrast, Ca2+ efflux appeared to be catalyzed by an active transport system. With cells previously loaded at 0 degrees C with 45Ca2+, Ca2+ efflux was rapid at 23 degrees C, but did not occur at 0 degrees C. This active Ca2+ efflux mechanism is probably responsible for maintaining the low internal Ca2+ levels in unstimulated cells.     

The Ca2+ permeability of sarcoplasmic reticulum vesicles II. Ca2+ efflux in the energized state of the calcium pump

Ca²⁺ efflux from sarcoplasmic reticulum vesicles was studied by measurements of net Ca²⁺ uptake, ⁴⁵Ca²⁺ flux and hydrolysis of energy-rich phosphate. The maximal Ca²⁺ uptake capacity (150–200 nmol/mg protein at pH 6.7, 10 mM MgCl₂ and μ=0.26) was independent of the nature and concentration of the energy-donating substrate (ATP or carbamyl phosphate) and of temperature (15–35°C), suggesting coupling between influx and efflux of Ca²⁺. In the presence of high concentrations of ATP, this efflux of Ca²⁺ was much higher than the passive Ca²⁺ permeation, measured after ATP or Ca²⁺ depletion of the reaction medium. Ca²⁺ efflux was imperceptible at vesicle filling levels below 35–40 nmol Ca²⁺/mg protein, and uncorrelated to the inhibition of the Ca²⁺-ATPase by high intravesicular Ca²⁺ concentrations. Analysis of the data indicated that Ca²⁺ efflux under our conditions probably is associated with one of the Ca²⁺-ATPase partial reactions occurring after dephosphorylation, rather than with a reversal of the Ca²⁺ translocation step in the phosphorylated state of the enzyme. Furthermore, passive Ca²⁺ permeation may be concurrently reduced during the enzymatically active state. It is proposed that both Ca²⁺ efflux and passive Ca²⁺ permeation (Ca²⁺ outflow) proceed via the same channels which are closed (occluded) during part of the Ca²⁺-ATPase reaction cycle.     

Effects of adenosine diphosphate on Ca2+ fluxes and Ca2+ accumulation of sarcoplasmic reticulum

Ca²⁺ transport by sarcoplasmic reticulum vesicles was examined by incubating sarcoplasmic reticulum vesicles (0.15 mg/ml) at 37°C in, either normal medium that contained 0.15 M sucrose, 0.1 M KCl, 60 μM CaCl₂, 2.5 mM ATP and 30 mM Tes at pH 6.8, or a modified medium for elimination of ADP formed from ATP hydrolysis by including, in addition, 3.6 mM phosphocreatine and 33 U/ml of creatine phosphokinase. In normal medium, Ca²⁺ uptake of sarcoplasmic reticulum vesicles reached a plateau of about 100 nmol/mg. In modified medium, after this phase of Ca²⁺ uptake, a second phase of Ca²⁺ accumulation was initiated and reached a plateau of about 300 nmol/mg. The second phase of Ca²⁺ accumulation was accompanied by phosphate uptake and could be inhibited by ADP. Since, under these experimental conditions, there was no significant difference of the rates of ATP hydrolysis in normal medium and modified medium, extra Ca²⁺ uptake in modified medium but not in normal medium could not be explained by different phosphate accumulation in the two media. Unidirectional Ca²⁺ influx of sarcoplasmic reticulum near steady state of Ca²⁺ uptake was measured by pulse labeling with ⁴⁵Ca²⁺. The Ca²⁺ efflux rate was then determined by subtracting the net uptake from the influx rate. At the first plateau of Ca²⁺ uptake in normal medium, Ca²⁺ influx was balanced by Ca²⁺ efflux with an exchange rate of 240 nmol/mg per min. This exchange rate was maintained relatively constant at the plateau phase. In modified medium, the Ca²⁺ exchange rate at the first plateau of Ca²⁺ uptake was about half of that in normal medium. When the second phase of Ca²⁺ uptake was initiated, both the influx and efflux rates started to increase and reached a similar exchange rate as observed in normal medium. Also, during the second phase of Ca²⁺ uptake, the difference between the influx and efflux rates continued to increase until the second plateau phase was approached. In conditions where the formation of ADP and inorganic phosphate was minimized by using a low concentration of sarcoplasmic (7.5 μg/ml) and/or using acetyl phosphate instead of ATP, the second phase of Ca²⁺ uptake was also observed. These data suggest that the Ca²⁺ load attained by sarcoplasmic reticulum vesicles during active transport is modulated by ADP accumulated from ATP hydrolysis. ADP probably exerts its effect by facilitating Ca²⁺ efflux, which subsequently stimulates Ca²⁺ exchange.     

Quantitation of CaP2+ fluxes in chick calvaria

This report utilizes an Ussing-type apparatus to quantitative the unidirectional fluxes of Ca²⁺ across the periosteal and endosteal membranes of frontal bones derived from calvaria of 20-day chick embryos. The influx was found to be proportional to the concentration of Ca²⁺ and equal to 0.31 μmoles/cm² per h at a concentration of ultrafiltrable Ca²⁺ of 1.75 mM. There were observable differences in the influx measured from periosteal or endosteal sides. The influx was found to be inversely proportional to decreasing temperature and increasing viscosity. The influx increased to 150% of the control flux when the incubation medium contained iodoacetate at a concentration of 1 mM and increased to 200% of control flux when the endosteum or periosteum was removed. These characteristics support the view that the influx is a passive flow with the integrity of cellular layer a controlling factor. The endosteal efflux was greater by a factor of 2 when compared to the periosteal efflux at 37 °C. When the temperature was reduced to 6 °C the endosteal to periosteal efflux ratio decreased to 1.26 indicating a temperature-sensitive component in the endosteal efflux.     

Effect of temperature on membrane fluidity and calcium conductance of the excitable ciliary membrane from Paramecium

Fluorescence anisotropy and average fluorescence lifetime of diphenylhexatriene were measured in artificial lipid membrane vesicles. Within the temperature range investigated (15–52°C) both parameters correlate and can be used interchangeably to measure membrane fluidity. Fluorescence anisotropy of DPH in membrane vesicles of cilia from the protozoan Paramecium tetraurelia decreased slightly from 5 to 37°C, yet, no phase transition was observed. An estimated flow activation energy of approx. 2 kcal/mol indicated that the ciliary membrane is very rigid and not readily susceptible to environmental stimuli. The ciliary membrane contains two domains of different membrane fluidity as indicated by two distinct fluorescence lifetimes of diphenylhexatriene of 7.9 and 12.4 ns, respectively. Ca²⁺ flux into ciliary membrane vesicles of Paramecium as measured with the Ca²⁺ indicator dye arsenazo III showed a nonlinear temperature dependency from 5 to 35°C with a minimum around 15°C and increasing flux rates at higher and lower temperatures. The fraction of vesicles permeable for Ca²⁺ remained unaffected by temperature. The differences in temperature dependency of Ca²⁺ conductance and membrane fluidity indicate that the Ca²⁺ permeability of the ciliary membrane is a membrane property which is not directly affected by the fluidity of its lipid environment.     

Changes in Rb+ and Ca2+ influx in winter wheat roots before, during and after exposure to low temperature and short days

Influx of Rb⁺(⁸⁶Rb⁺) and Ca²⁺ (⁴⁵Ca²⁺) in roots of intact winter wheat (Triticum aestivum L. cv. Weibulls Starke II) was determined at intervals before, during and after exposure to cold acclimation conditions (2°C and 8 h light period). The plants were grown in nutrient medium of two ionic strengths. During the initial two weeks of growth at 16°C and 16 h light period, Rb⁺ influx into roots decreased with increasing age, probably as a consequence of a decreasing proportion of metabolically active roots. The presence of 10^?4M 2,4-dinitrophenol (DNP) reduced Rb⁺ influx to a low and constant level, indicating that metabolic influx was the dominant process. In contrast, Ca²⁺ influx in plants grown in full strength nutrient solution was higher in the presence than in the absence of DNP. This effect may have been due to an active extrusion mechanism mediating re-export of absorbed Ca²⁺(⁴⁵Ca²⁺) during the uptake experiment. With the metabolic uncoupler inhibiting such extrusion the Ca²⁺(⁴⁵Ca²⁺) influx mesured would increase. During cold treatment, Rb⁺ influx remained at a low level, and was further decreased when DNP was present in the uptake solution. This effect may have been due to inhibition of residual active influx of Rb⁺ at 2°C by the uncoupler and/or to a decrease in membrane permeability. In contrast to Rb⁺, Ca²⁺ influx increased during cold treatment, which could again be explained as inhibition of re-export. The presence of DNP reduced Ca²⁺ influx at 2°C, indicating decreased membrane permeability by DNP at low temperature. After transfer of plants from cold acclimation conditions to 16°C, Rb⁺ and Ca²⁺ influx increased in plants grown at both ionic strengths. Influx levels were independent of the length of the cold acclimation period (1, 6 and 8 weeks), but the patterns were different for the two ions. After each of the cold acclimation periods, Rb⁺ influx increased during the first week and decreased or remained at the same level during the second week, while Ca²⁺ influx always decreased during the second week of post-cold treatment.     

Influence of low temperature on regulation of Rb+ and Ca2+ influx in roots of winter wheat

Influx of Rb⁺(⁸⁶Rb⁺) and Ca²⁺(⁴⁵Ca²⁺) was determined in roots of winter wheat (Triticum aestivum L. cv. Weibulls Starke II) after 14 days at 16°C/16 h light, after 1 and 8 weeks of cold acclimation (2°C/8 h light) and at intervals after deacclimation (16°C/16 h light) for up to 14 days. The plants were cultivated at 3 ionic strengths: 100, 10 and 1% of a full strength nutrient solution, containing 3.0 mM K⁺ and 1.0 mM Ca²⁺. K⁺ concentrations in roots and shoots increased during cold treatment, while Ca²⁺ in the roots decreased. In the shoots Ca²⁺ concentrations remained the same. Influx of Rb⁺ as a function of average K⁺ concentration in the roots of 14-day-old, non-cold-treated plants was high at a certain K⁺ level in the root and decreased at higher root K⁺ levels (negative feedback). The pattern for Ca²⁺ influx versus average concentration of Ca²⁺ in the root was the reverse. Independent of duration of treatment (1–8 weeks), cold acclimation partly changed the regulation of Rb⁺ influx, so that it became less dependent upon negative feedback and more dependent on the ionic strength of the cultivation solution. After exposure to 2°C, Ca²⁺ influx increased at high Ca²⁺ concentrations in the root as compared with influx in roots of 14-day-old non-cold-treated plants. Under deacclimation, Ca²⁺ influx gradually decreased again, and reached the level observed before cold treatment within 7–14 days at 16°C; the number of days depending on the exposure time at 2°C. It is suggested that Rb⁺(K⁺) influx became adjusted to low temperature and that abscisic acid (ABA) may be involved in this mechanism. It is also suggested that extrusion of Ca²⁺ was impaired and/or Ca²⁺ channels were activated at 2°C in roots of plants grown in the full-strength solution and that extrusion was gradually restored and/or Ca²⁺ channels were closed under deacclimation conditions.     

Stimulation of Ca2+ efflux by N-formyl chemotactic peptides in guinea-pig peritoneal macrophages

Effects of N-formyl chemotactic peptides on the Ca²⁺ influx and efflux were investigated in guinea-pig peritoneal macrophages using an isotope tracer. fMet-Leu-Phe did not enhance the influx of ⁴⁵Ca²⁺ into macrophages, whereas it stimulated the efflux of ⁴⁵Ca²⁺ from macrophages at concentrations ranging from 10^?10 M to 10^?7 M. fMet-Met-Met and fMet-Leu also stimulated the ⁴⁵Ca²⁺ efflux, albeit at much higher concentrations, while there was no stimulation with fMet. The mitochondrial inhibitors, oligomycin and NaN₃, did not modify the ⁴⁵Ca²⁺ efflux induced by the chemoattractants, yet they did induce the release of ⁴⁵Ca²⁺ from the mitochondria. On the other hand, higher concentrations of the calmodulin antagonists, chlorpromazine and trifluoperazine, induced the release of ⁴⁵Ca²⁺ from the NaN₃-insensitive Ca²⁺ store site and mimicked the enhancement of the ⁴⁵Ca²⁺ efflux by N-formyl chemotactic peptides. Thus, N-formyl chemotactic peptides appear to increase the levels of intracellular free Ca²⁺ in guinea-pig peritoneal macrophages, probably by inducing the release of Ca²⁺ from the NaN₃-insensitive Ca²⁺ store site.     

K+(Rb+) and Ca2+ fluxes in young winter wheat plants exposed to sub-zero temperatures

Ice crystal formation temperature was determined in the region of the crown in one group of 7-day-old intact unhardened high-salt plants of winter wheat (Triticum aestivum L. cv. Weibulls Starke II) with TA (Thermal Analysis) and DTA (Differential Thermal Analysis) methods. After exposure of another group of plants, grown for the first 7 days in the same way as the first group, to various sub-zero temperatures (-1 to 5°C), influx in roots of Rb⁺(⁸⁶Rb⁺) and Ca²⁺(⁴⁵Ca²⁺) and contents of K⁺ and Ca²⁺ were determined at intervals during 7 days of recovery. Ice crystal formation in the crown tissue was probably extracellular and took place at about -4°C. There was a large loss of K⁺ from the roots after treatment at sub-zero temperatures. This loss increased as the temperature of the sub-zero treatment decreased. During recovery, roots of plants exposed to -1, -2 and -3°C gradually reabsorbed K⁺. Reabsorption of K⁺ in roots of plants exposed to -4°C was greatly impaired. Rb⁺ influx decreased and Ca²⁺ influx increased after sub-zero temperature treatments of the plants. Active Rb⁺ influx mechanisms and active extrusion of Ca²⁺ were impaired or irreversibly damaged by the exposure. While Rb⁺ influx mechanisms were apparently repaired during recovery in plants exposed to temperatures down to -3°C, Ca²⁺ extrusion mechanisms were not. The temperature for ice crystal formation in the region of the crown tissue coincides with the temperature at which the plants lost the ability to reabsorb K⁺ and to repair Rb⁺ influx mechanisms during the recovery period. Plants were lethally damaged at temperatures below ?4°C.     

Concanavalin a binding and Ca2+ fluxes in rat spleen cells

Addition of the mitogenic lectin concanavalin A to rat spleen cells results in a small increase in the steady-state Ca²⁺ content of the cells. ⁴⁵Ca²⁺ fluxes were measured under conditions where artifacts due to Ca²⁺ binding to concanavalin A could be excluded. Both ⁴⁵Ca²⁺ influx into and efflux from these cells are significantly activated by the lectin. If ⁴⁵Ca²⁺ is added 30 min after concanavalin A the rate of influx is further enhanced. The increase in ⁴⁵Ca²⁺ influx correlates well with binding of concanavalin A to the cells. At low concentrations (optimal mitogenic) of the lectin (1 and 3 μg/ml) no significant increase in ⁴⁵Ca²⁺ influx occurs but an increase in ⁴⁵Ca²⁺ efflux is still observed. The results suggest that concanavalin A binding to the cell surface causes an increase in Ca²⁺ influx into the cells and that activation of Ca²⁺ efflux occurs as a response to an increase in the cytosolic Ca²⁺ activity. Thus, Ca²⁺ may well play a role in triggering lymphocyte activation.     

The lipid integrity of membranes of guinea pig alveolar macrophages studied by nanosecond fluorescence decay of 1,6-diphenyl-1,3,5-hexatriene: The effect of stimulation by concanavalin A and formyl peptides1

Time-resolved fluorescence anisotropy of 1,6-diphenyl-1,3,5-hexatriene was used to monitor physical changes in the membranes of guinea pig alveolar macrophages following stimulation by N-formyl peptides (either N-formylmethionylphenylalanine (FMP) or N-formyl methionyl leucylphenylalanine (FMLP)) and concanavalin A. The anisotropy of diphenylhexatriene in macrophages showed a dependence on stimulation both in the rate of decay and in the value of anisotropy at infinite time. Subtle differences were observed between the effect of concanavalin A and FMLP on the membrane lipid fluidity as detected by fluorescence anisotropy. Concanavalin A stimulation of macrophages decreased the value of the anisotropy at infinite times in the range of 0–20 °C and increased the value at 25–40 °C; and at all temperatures it decreased the rate of decay of anisotropy. At temperatures below 25 °C, the response to FMLP was similar to concanavalin A, but above 25 °C, FMLP only slightly modified the anisotropy decay profile. Another physical parameter, calcium permeability, was examined because Ca⁺² fluxes are dependent upon membrane properties. The temperature-dependent profiles of concanavalin A and FMP-stimulated ⁴⁵Ca⁺² efflux from alveolar macrophages were similar. The rate and extent of ⁴⁵Ca⁺² efflux increased from 4 to 22 °C, with no further increases observed up to 37 °C. This pattern correlated well with observed changes in membrane fluidity.     

Aluminium interactions with K+(86Rb+) and 45Ca2+ fluxes in three cultivars of sugar beet (Beta vulgaris)

Three cultivars of sugar beet (Beta vulgaris L.), which are sensitive to aluminium (Al) in the order Primahill > Monohill > Regina, were grown in water culture for 2 weeks. Nutrients were supplied at 15% increase of amounts daily, corresponding to the nutrient demand for maximal growth. The 2.4-dinitrophenol (DNP)-sensitive (metabolic) and DNP-insensitive (non-metabolic) uptake of aluminium, phosphate. ⁴⁵Ca²⁺ and K⁺(⁸⁶Rb⁺) in roots were measured as well as transport to shoots of intact plants. All 3 cultivars absorbed more aluminium if DNP was present during the aluminium treatment than in its absence. It is suggested that sugar beets are able to extrude aluminium activity or that they possess an active mechanism to keep Al outside the cell. The presence of Al in the medium during the 1-h experiment affected the metabolic and non-metabolic fluxes of ⁴⁵Ca²⁺ and K⁺(⁸⁶Rb⁺) in different ways. In the presence of DNP, the influx of both ⁴⁵Ca²⁺ and K⁺(⁸⁶Rb⁺) and the efflux of ⁴⁵Ca²⁺ were inhibited by Al in a competitive way. At inhibition of ⁴⁵Ca²⁺ influx, 2 Al ions are probably bound per Ca²⁺ uptake site in cv. Regina (Al-tolerant), but in cvs Primahill and Monohill only one Al ion is bound (more Al sensitive). Aluminium competitively inhibited the active efflux of ⁴⁵Ca²⁺ (absence of DNP) in almost the same way in the 3 cultivars. In contrast, aluminium stimulated the influx of K⁺(⁸⁶Rb⁺) in cvs Primahill, Monohill and Regina in the absence of DNP. Thus, the Al effects on active and passive K⁺(⁸⁶Rb⁺) influx are different. The total influx of K⁺(⁸⁶Rb⁺) increased in the presence of Al and might be connected to an active exclusion of Al. Regina is the least Al-sensitive cultivar, probably because Al interferes less with the Ca²⁺ fluxes and because this cultivar actively excludes phosphate in the presence of Al. Thus Al-phosphate precipitation within the plant could be avoided.     

H-mediated coupling of transmembrane Ca fluxes in vegetative Trichoderma viride mycelia suggested by the study of ageing and adaptation to extreme Ca concentrations

The adaptation to extreme concentrations of Ca²⁺ and its consequence on the properties of the ⁴⁵Ca²⁺ transport were studied in submerged mycelia of Trichoderma viride. The adaptation to low [Ca²⁺]_o did not cause changes in kinetic parameters of the ⁴⁵Ca²⁺ influx but the adaptation to high [Ca²⁺]_o increased the K_M(Ca2+). The V_max of the ⁴⁵Ca²⁺ influx decreased with the age of (non-adapted) mycelia with concomitant decrease of the K_M(Ca2+) these changes were prevented in mycelia adapted to high Ca²⁺. High [Ca²⁺]_o decreased the stimulation by the uncoupler, 3, 3′, 4′, 5-tetrachloro salicylanilide (TCS) (30 μM), as compared to the control, whereas the Ca²⁺ chelator, EGTA, stimulated it. In the aged mycelia, the stimulation by TCS of the ⁴⁵Ca²⁺ influx faded away, in parallel with the activity of the H⁺-ATPase. The ⁴⁵Ca²⁺ efflux from mycelia was affected by TCS in a similar way as the ⁴⁵Ca²⁺ influx. The results demonstrate the adaptive responses of transport processes participating in the mycelial Ca²⁺ homeostasis and ageing are in agreement with a notion that both Ca²⁺-influx and-efflux are coupled by the H⁺-homeostasis at the plasma membrane.     

Biophysical effects of the natural product euplotin C on the <Emphasis Type="Italic">Paramecium</Emphasis> membrane

The effect of euplotin C—a cytotoxic secondary metabolite produced by the protist ciliate Euplotes crassus—on the voltage-dependent Ca²⁺ channel activity was studied in a single-celled system by analyzing the swimming behavior of Paramecium. When the intraciliary Ca²⁺ concentration associated with plasma membrane depolarization increases, a reversal in the direction of ciliary beating occurs, and consequently the swimming direction changes. The ciliary reversal duration is correlated with the amount of Ca²⁺ influx. The present study demonstrates that the duration of continuous ciliary reversal (CCR), triggered by high external KCl concentrations, is longer in euplotin C-treated cells. Using selective Ca²⁺ channel blockers, we demonstrate that euplotin C modulates Ca²⁺ channels similar to the T- and L-types that occur in mammalian cells. Indeed, the increase of CCR duration significantly decreased when flunarizine and nimodipine-verapamil blockers were employed. Membrane fluidity measurements using a fluorescent dye, 6-lauroyl-2-dimethylaminonaphtalene (laurdan), indicated that membranes in euplotin C-treated cells are more tightly packed and ordered than membranes in control cells. Our data suggest that euplotin C enhances backward swimming in our unicellular model system by interacting with the ciliary Ca²⁺ channel functions through the reduction of cell membrane fluidity.     

Transport and control of Ca2+ by pigeon erythrocytes. III. A ‘paradoxical’ expulsion of Ca2+ induced by a low dose of A23187 at 0° C

Pigeon erythrocytes expelled preloaded ⁴⁵Ca²⁺ in response to a low dose of A23187 at 0° C. We call this phenomenon ‘paradoxical’ expulsion. Within the first minute, 1.85 ± 0.38 μmol/l cell water was expelled; after that the internal ⁴⁵Ca²⁺ began to rise. The rises in Ca²⁺ uptake with and without A23187 addition were essentially paralleled. No premonitory rise of ⁴⁵Ca²⁺ upon the addition of A23187 was observed. Expulsion of ⁴⁵Ca²⁺ in response to A23187 was probably by the action of the Ca²⁺ pump and not by Na⁺-Ca²⁺ exchange since vanadate inhibited, but K⁺ replacement of Na⁺ in the medium had no effect. Lysophosphatidylcholine (lysoPC) caused an abrupt increase in ⁴⁵Ca²⁺ influx by cells at 0° C and was dose dependent. However, a very low dose of lysoPC induced expulsion of preloaded ⁴⁵Ca²⁺ similar to that by A23187, the response was fast and transitory, without any premonitory rise in ⁴⁵Ca²⁺ uptake. The results lend support to the suggestion that the signal to which cells respond may be a sudden change in Ca²⁺ influx per se rather than a change in internal Ca²⁺ concentration. These features of ‘paradoxical’ ⁴⁵Ca²⁺ expulsion induced by A23187 and lysoPC are not expected from mass-action equilibria but, instead, agree with the characteristics of an energy-dissipating control mechanism.     

Cultured cells from renal cortex of hibernators and nonhibernators. Regulation of cell K+ at low temperature

Cells were grown as primary monolayer cultures from kidney cortex of guinea pigs (nonhibernators), hamsters and ground squirrels (both hibernating species). When plates of cells were placed at 5 °C, cells of guinea pigs lost 37% of their K⁺ in 2 h and those of the hibernator lost about 10%.Uptake of ⁴²K into the cells exhibited a simple, single exponential time course at both temperatures. Unidirectional efflux of K⁺ was equal to K⁺ influx in all cultures at 37 °C and, within limits of error, in hibernator cells at 5 °C. Efflux was 3- to 5-fold greater than influx in guinea pig cells at 5 °C.After 2 h in the cold the ouabain-sensitive K⁺ influx remaining (7–15% of that at 37 °C) was about the same in the cells of the 3 species. Cells from active hamsters and from hibernating ground squirrels, however, exhibited significantly greater pump activity after 45 min in the cold (19 and 14%, respectively). The stimulation of K⁺ influx by increasing [K⁺]_o did not show an increase in K_m⁺ at 5 °C in cells of guinea pigs and ground squirrels. Lowering [K⁺]_c and/or raising [Na⁺]_c by treatment in low- and high-K⁺ media caused only slight stimulation of K⁺ influx, except in cells of ground squirrels at 5 °C in which the stimulation was at least 11-times greater than at 37 °C or in cells of guinea pigs at either temperature.This altered kinetic response of K⁺ transport to cytoplasmic ion stimulation with cooling accounted for about one-third of the improved regulation of K⁺ at 5 °C in ground squirrel cells; the other two-thirds was attributable to a greater decrease in K⁺ leak with cooling. The inhibition of active transport by cold in all 3 species was much less severe than that previously seen in any (Na⁺ + K⁺)-ATPase of mammalian cells.     

H+ Fluxes at Plasmalemma Level: In Vivo Evidence for a Significant Contribution of the Ca2+-ATPase and for the Involvement of its Activity in the Abscisic Acid-Induced Changes in Egeria Densa Leaves

Abstract: The features of Ca²⁺ fluxes, the importance of the Ca²⁺ pump‐mediated H⁺/Ca²⁺ exchanges at plasmalemma level, and the possible involvement of Ca²⁺‐ATPase activity in ABA‐induced changes of H⁺ fluxes were studied in Egeria densa leaves. The results presented show that, while in basal conditions no net Ca²⁺ flux was evident, a conspicuous Ca²⁺ influx (about 1.1 ìmol g^?1 FW h^?1) occurred. The concomitant efflux of Ca²⁺ was markedly reduced by treatment with 5 íM eosin Y (EY), a specific inhibitor of the Ca²⁺‐ATPase, that completely blocked the transport of Ca²⁺ after the first 20 ‐ 30 min. The decrease in Ca²⁺ efflux induced by EY was associated with a significant increase in net H⁺ extrusion (?ÄH⁺) and a small but significant cytoplasmic alkalinization. The shift of external [Ca²⁺] from 0.3 to 0.2 mM (reducing Ca²⁺ uptake by about 30 %) and the hindrance of Ca²⁺ influx by La³⁺ were accompanied by progressively higher ?ÄH⁺ increases, in agreement with a gradual decrease in the activity of a mechanism counteracting the Ca²⁺ influx by an nH⁺/Ca²⁺ exchange. The ABA‐induced decreases in ?ÄH⁺ and pH_cyt were accompanied by a significant increase in Ca²⁺ efflux, all these effects being almost completely suppressed by EY, in line with the view that the ABA effects on H⁺ fluxes are due to activation of the plasmalemma Ca²⁺‐ATPase. These results substantially stress the high sensitivity and efficacy of the plasmalemma Ca²⁺ pump in removing from the cytoplasm the Ca²⁺ taken up, and the importance of the contribution of Ca²⁺ pump‐mediated H⁺/Ca²⁺ fluxes in bringing about global changes of H⁺ fluxes at plasmalemma level.     

Inactivation of Ca2+-induced ciliary reversal by high-salt extraction in the cilia of Paramecium

Intracellular Ca²⁺ induces ciliary reversal and backward swimming in Paramecium. However, it is not known how the Ca²⁺ signal controls the motor machinery to induce ciliary reversal. We found that demembranated cilia on the ciliated cortical sheets from Paramecium caudatum lost the ability to undergo ciliary reversal after brief extraction with a solution containing 0.5 M KCl. KNO₃, which is similar to KCl with respect to chaotropic effect; it had the same effect as that of KCl on ciliary response. Cyclic AMP antagonizes Ca²⁺-induced ciliary reversal. Limited trypsin digestion prevents endogenous A-kinase and cAMP-dependent phosphorylation of an outer arm dynein light chain and induces ciliary reversal. However, the trypsin digestion prior to the high-salt extraction did not affect the inhibition of Ca²⁺-induced ciliary reversal caused by the high-salt extraction. Furthermore, during the course of the high-salt extraction, some axonemal proteins were extracted from ciliary axonemes, suggesting that they may be responsible for Ca²⁺-induced ciliary reversal.