Magnesium uptake by soybeans

Magnesium contents of soybean (Glycine max) roots increase and the K and Ca contents decrease with increased MgCl₂ concentrations in ambient solutions. The Mg uptake is inhibited when both Ca and K are present in the solution, but not by K or Ca alone. Chloride uptake, which is very low from the MgCl₂ solution, is greatly enhanced by the presence of K. The selectivity against Mg imparted by K + Ca appears to be at an external barrier for cation uptake as shown by its dependence on the presence of Ca in the external solution. The Ca content of roots is influenced only slightly by changes in external Ca concentrations from 10⁻⁴ to 10⁻²m, but that of shoots is greatly enhanced as the Ca concentration is increased or the K concentration is decreased. These effects on Ca contents are explained as arising from transport to the shoot without involvement of vacuoles of root cells.     

Effect of metabolic inhibitors and temperature on uptake and translocation of ca and k by intact bean plants

The dependence of Ca uptake and translocation by intact roots of Phaseolus vulgaris on concurrent root metabolism was investigated using ⁴⁵Ca-labeled Hoagland solutions at one-half and one-twentieth strength (2.5 and 0.25 mM Ca²⁺). Adsorbed and absorbed ⁴⁵Ca fractions in the roots were distinguished on the basis of the time course of exchange with the outer solution. Uptake of ⁴²K, of which the characteristics are better known, was measured for comparison. The absorbed ⁴⁵Ca fraction showed a markedly nonlinear increase with time in contrast to the near linear increase in ⁴²K. Exposure of roots to cyanide, arsenate, 2,4-dinitrophenol, or low temperatures caused only slight reductions in ⁴⁵Ca absorption by roots, but significant reductions of ⁴²K. In all treatments involving inhibitors and low temperatures, the translocation to shoots of both ⁴⁵Ca and ⁴²K was strongly inhibited. The conclusion that much of the absorbed ⁴⁵Ca fraction in the root tissue is taken up by processes which are not rate-limited by metabolism is discussed.     

Salinity-calcium interactions on growth and ionic concentration of Citrus plants

Two-year-old Navel orange scions (Citrus sinensis (L.) Osbeck) budded to either Cleopatra mandarin (C. reticulata) and Troyer citrange (C. sinensis × P. trifoliata) rootstocks were used in this experiment. Cleopatra manda in rootstock was considered more tolerant to salinity than Troyer citrange, and this property was attributed to a greater capacity to exclude chloride ions.Plants were grown under glasshouse conditions and supplied with nutrient solution containing either no or 45 mM NaCl. Calcium concentration was increased from 3 to 30 mM. Sodium, potassium, calcium and chloride concentrations in plant organs were analyzed after 90 days of treatment.Supplemental Ca was found to mitigate the adverse effects of salinity on plant growth, defoliation or leaf injury.Chemical analysis indicated that in plants grafted on Troyer citrange Ca restricted uptake and subsequent translocation of Na to the leaves and increased K concentration in both roots and leaves. However, in Cleopatra mandarin-grafted plants increasing Ca levels seemed to reduce transport of Na from roots to leaves, and Na accumulation in roots was associated with reduced concentration of K in this rootstock.Organ chloride analysis showed that Cl accumulation in leaves of plants grafted on both rootstocks was reduced when external Ca concentration increased, whereas Cl concentration in roots remained constant or increased. The data of distribution of Cl in plants showed that a high external Ca level increased Cl accumulation in the basal stem and roots, and reduced the transport of Cl from roots to leaves.     

CHLOROTETRACYCLINE-ASSOCIATED FLUORESCENCE CHANGES DURING CALCIUM UPTAKE AND RELEASE BY RAT BRAIN SYNAPTOSOMES1

Abstract– The fluorescent divalent metal chelate-probe, chlorotetracycline (CTC), was used as a dynamic monitor of calcium association with rat brain snynaptosomes. The determined fluorescence excitation and emission maxima, 412 nm and 522 nm respectively, were used to monitor membrane-calcium interactions as a function of various parameters. Positive correlations were observed between increased or decreased fluorescence quantum yield and the uptake of both CTC and ⁴⁵Ca by synpatosomes. The divalent metal ionophore A23187 enhanced fluorescence as well as probe and ⁴⁵Ca uptake. Whereas, the polar chelator, EGTA, markedly reduced fluorescence, and the synaptosomal bound CTC and ⁴⁵Ca. The CTC fluorescence changes also demonstrated the saturable manner in which ⁴⁵Ca bound synaptosomes. At concentrations greater than 100μg/ml, CTC bound to the synaptosomes in a manner which quenched fluorescence at 522 nm. Also, CTC, at concentrations above 15 μg/ml, enhanced the uptake of ⁴⁵Ca. At CTC concentrations between 10 and 15 μg/ml the quenching and iono-phoretic properties of the probe were minimized without affecting the capability of using the probe to visualize calcium interactions with synaptosomal membranes. Also, at a low CTC concentration (12.5 μg/ml) the inhibition of calcium uptake by increasing monovalent ion concentrations was clearly demonstrated.     

Characteristics of ouabain binding to isolated trout hepatocytes

Summary Na⁺, K⁺ exchanges were studied in isolated hepatocytes of the rainbow trout, Salmo gairdneri. Ouabain at 10^–4 M produced maximal inhibition (95%) of K⁺ uptake and enhanced intracellular Na⁺ accumulation, showing that active fluxes account for a very large proportion of Na⁺ and K⁺ exchanges. Inhibition of the Na–K pump by ouabain was significant at low concentrations (10^–8 M). When external K⁺ concentration was reduced from 7 mM to 0.5 mM, half maximum inhibition (IC₅₀) of K⁺ uptake was obtained at a 22-fold lower concentration of ouabain confirming that ouabain and potassium compete at the same pump site. Time-course analysis of [³H]ouabain binding indicated a two-component kinetics: one component saturable and dependent on K⁺ concentration in the medium, the other linear and independent of external K⁺. The ouabain binding site number, determined by Scatchard plots, remained constant (ca. 2.5·10⁵ per cell) and independent of the external K⁺ concentration (7, 0.5 or 0 mM), while the dissociation constant (K_D) decreased from 4.2 M to 7.3 nM when K⁺ was removed from the Hank's medium. These ouabain binding sites are characterized by an exceptionally low turnover rate (400 min^–1), as estimated from ouabain-sensitive K⁺ flux, in comparison to those described in other cell types of higher vertebrates. At each external K⁺ concentration studied, the inhibition of K⁺ uptake and ouabain binding measured as a function of ouabain concentration indicated a strict correlation between the degree of K pump inhibition and the amount of bound glycoside.     

Intracellular Calcium Movements of Frog Skeletal Muscle during Recovery from Tetanus

Radioautographs of ⁴⁵Ca-labeled frog skeletal muscles have been prepared using freeze-dry and vapor fixation techniques to avoid displacement of the isotope during the preparation of the radioautographs. ⁴⁵Ca has been localized in resting muscles exposed to ⁴⁵Ca Ringer's for 5 min or 5 hr and in isotopically labeled muscles recovering from tetanic stimulation at room temperature or at 4°C. In muscles soaked at rest for 5 min ⁴⁵Ca was present almost exclusively in the terminal cisternae. In all other muscles there were three sites at which the isotope was concentrated: (a) the terminal cisternae, (b) the intermediate cisternae and the longitudinal tubules, and (c) the A band portion of the myofibrils. The terminal cisternae were labeled more rapidly than the myofibrils, but both exchanges were accelerated by electrical stimulation. The amount of ⁴⁵Ca in the longitudinal tubules and the intermediate cisternae decreased with time after a tetanus as the amount in the terminal cisternae increased. It is proposed that electrical stimulation releases calcium from the terminal cisternae and that relaxation occurs from the binding of the released calcium by the longitudinal tubules and the intermediate cisternae. Complete recovery from mechanical activity involves the transport of this bound calcium into the reticulum and its subsequent binding by the terminal cisternae. Resting exchange of calcium occurs primarily between the terminal cisternae and the transverse tubules.     

Calcium distribution and exchange in the rat uterus

The calcium content and distribution of the rat uterus were determined employing flame photometry and Ca⁴⁵ determinations. The total uterine calcium concentration was found to be 2.25 millimoles (mmoles) per kilogram wet weight, 0.45 of which was inexchangeable. The exchangeable Ca could be divided into 0.8 mmole/kg wet weight extracellular and 1.0 mmole/kg wet weight intracellular. The concentration of ionic Ca in rat serum was obtained by equilibrium dialysis as 1.5 mM or 53 % of the total serum Ca. The observed Ca distribution required that its active transport be postulated, since the membrane was shown to be permeable to Ca and the internal Ca concentration was far below its electrochemical equilibrium value. Metabolic inhibition by iodoacetate or dinitrophenol caused a net Ca uptake, but cooling to 4°C and ouabain did not. Iodoacetate did not affect the Ca⁴⁵ efflux, but did increase the influx, suggesting that active Ca transport is accomplished by an exclusion mechanism. In experiments with varied external sodium concentrations, no evidence was obtained that sodium competes with calcium for inward transport. Cellular Ca binding was measured under conditions of prolonged metabolic inhibition, which abolished both active transport and the membrane potential. The association constants obtained were compatible with intracellular Ca binding to proteins, but insufficient to account for the low level of intracellular ionic Ca believed essential for relaxation. Hence metabolically dependent intracellular Ca binding was postulated. The Ca⁴⁵ efflux was slowed down by Ca-free efflux media. The presence of Sr or EDTA could completely prevent this decrease in efflux rate, and Ba could partly prevent it. Changes in Mg and Na concentration did not affect the rate of Ca⁴⁵ efflux. A model to explain Ca exchange across smooth muscle membranes has been proposed.     

Urease activity in soils

Summary The availability of Ca from different levels of gypsum and calcium carbonate in a non-saline sodic soil has been investigated. Different levels of tagged gypsum (Ca⁴⁵SO₄.2H₂O) and calcium carbonate (Ca⁴⁵CO₃) (i.e. 0, 25, 50, 75, and 100 per cent of gypsum requirement) were mixed thoroughly in 3.5 Kg of a non-saline alkali soil (ESP, 48.4; ECe, 2.68 millimhos/cm). Dhaincha (Sesbania aculeata) — a legume and barley (Hordeum vulgare L.) — a cereal were taken as test crops. Increasing levels of gypsum caused a gradual increase in the yield of dry matter, content of Ca and K in the plant tops and Ca:Na and (Ca+Mg):(Na+K) ratios in both the crops. Application of calcium carbonate caused a slight increase in the dry matter yield, content of Ca and Mg and Ca:Na and (Ca+Mg):(Na+K) ratios in barley, however, in case of dhaincha there was no such effect. Gypsum application caused a gradual decrease in the content of Na and P in both the crops. Total uptake of Ca, Mg, K, N and P per pot increased in response to gypsum application. The effect of calcium carbonate application on the total uptake of these elements was much smaller on dhaincha, but in barley there was some increasing trend.Increasing application of tagged gypsum and calcium carbonate caused a gradual increase in the concentration and per cent contribution of source Ca in both the crops, although, the rate of increase was considerably more in dhaincha. The availability of Ca from applied gypsum was considerably more than that from applied calcium carbonate. Efficiency of dhaincha to utilize Ca from applied sources was considerably more (i.e. about five times) than that of barley     

Influence of Nitrogen Supply on Uptake and Translocation of Strontium and Calcium in Wheat Seedlings

Supplying nitrate to N-depleted wheat seedlings (Triticum vulgare cv. Knox) stimulated the uptake and translocation of both ⁸³Sr and ⁴⁵Ca. Since the increase in ⁴⁵Ca accumulation was greater, the ⁸⁵Sr/⁴⁵Ca ratio in the plant tissue was decreased. Nitrate had relatively little influence on the amount of the divalent cations and ⁸⁵Sr/⁴⁵Ca ratio in the exchangeable fraction on the root surfaces, whereas it greatly increased the uptake into root tissue and translocation to shoots. The increase in percent transported to shoots occurred largely in the period of most rapid nitrate uptake. A split root study indicated that nitrate was ineffective when it was supplied to a different portion of the root system than that exposed to ⁸⁵Sr and ⁴⁵Ca. Nevertheless, ammonium and urea also increased the translocation of the two cations, indicating that the effects of nitrate could not entirely be ascribed to a direct effect of the nitrate anion.     

The influence of ionic strength on potassium contractures and calcium movements in frog muscle

Frog toe muscles were bathed in isotonic, sodium-free Tris chloride, methanesulfonate, or sulfate solutions containing sucrose or mannitol and varying in ionic strength from 0.006 to 0.291. By decreasing the ionic strength the curve relating the peak tension of the K contractures to the log [K] was reversibly shifted to lower [K]. Increasing the [Ca] from 1 to 4 mM almost abolished this effect. The resting uptake of ⁴⁵Ca was increased more than two times by decreasing the ionic strength from 0.125 to 0.039. It was not increased significantly by raising [Ca] from 1 to 4 mM at low or normal ionic strength. The additional uptake of ⁴⁵Ca during contractures provoked by 120 mM K was not significantly different at the two levels of ionic strength. The rate of emergence of ⁴⁵Ca from muscles loaded with ⁴⁵Ca at reduced ionic strength, was decreased. The effects of low ionic strength are discussed in terms of changes in the potential difference across a membrane with fixed negative charges on the outer surface.     

Coral calcification: autoradiography of a scleractinian coral Galaxeafascicularis after incubation in 45Ca and 14C

 The uptake of ⁴⁵Ca and/or ¹⁴C by the skeleton of coral colonies has been commonly used to investigate the processes of calcification. This study reports the differential uptake of these tracers within different regions of the skeleton and tissues of individual corallites and polyps of the hermatypic coral Galaxea fascicularis. Incubation in ⁴⁵Ca in the light resulted in 80 percent of the ⁴⁵Ca taken up being deposited in the skeleton. Autoradiography of transverse and longitudinal slices of freeze-substituted polyps and corallites showed that in the light ⁴⁵Ca was incorporated into the exsert septa, the outside of the thecal walls of the corallite and the inner edges of the septa. Incorporation did not occur in the costae. The radioactivity in the skeleton was considerably greater than in the tissues. In the dark, or in the presence of the photosynthetic inhibitor Diuron, ⁴⁵Ca was taken up by the exsert septa and was patchily distributed in the corallite walls which suggests that it was not a result of isotopic exchange. The differential incorporation of ⁴⁵Ca onto the exsert septa was confirmed by scintillation counting. Negligible radioactivity remained in the extrathecal coelenteron after a brief 5 min rinse in non-radioactive seawater. Only 0.1% of ¹⁴C taken up in the light was incorporated into the skeleton and this was confirmed by autoradiography. In the presence of Diuron or in the dark, very little ¹⁴C was incorporated into tissues or skeleton and in autoradiographs was either not evident in the skeleton or the distribution was similar to that seen in autoradiographs of ⁴⁵Ca uptake. These results show that the deposition of ⁴⁵Ca, and therefore calcium carbonate, occurs at specific loci on the skeleton of a corallite. In the dark, deposition occurs specifically at the growing points of the corallite. Differential deposition of calcium carbonate within individual corallites has not been previously reported. Accepted: 27 May 1997     

Regulatory changes of membrane transport and ouabain binding during progesterone-induced maturation ofXenopus oocytes

Summary During progesterone-stimulated maturation of defolliculated full-grownXenopus oocytes, the activities of the transport systems forl-alanine, thymidine, chloride, phosphate, and alkali ions decrease. Differences of the extent and time course of these changes suggest that they are controlled by at least partially independent mechanisms.A closer investigation of the Na-K ATPase has shown that in unstimulated oocytes, ouabain produces maximal inhibition when 8–12×10⁹ molecules are bound per cell. This number is bound during the first phase of a diphasic uptake process. Since this phase can be suppressed by increasing the concentration of external K⁺ to 45 mmol/liter or more, it is concluded that it refers to binding to the Na–K pump in the plasma membrane. Ouabain bound prior to progesterone-induced germinal vesicle breakdown (GVBD) remains bound after the breakdown, although the Na–K pump loses the capacity to bind ouabain after GVBD in oocytes that had not been exposed to ouabain preceding GVBD. In the presence of Mg⁺⁺ membranes isolated before regulatory inhibition of pumping and ouabain binding show a Na⁺-dependent incorporation of³²P from -[³²P]-ATP that can be reversed by the addition of K⁺. The phosphorylation site migrates on LiDS-polyacrylamide gel electropherograms at about 98,000 daltons and can be identified as a Commassie blue-stainable band.     

Does endogenous cyclic GMP inhibit potassium stimulated 45Ca uptake by P2 fraction from rat brain?

The effects of sodium azide (NaN₃), hydroxylamine (NH₂OH) and sodium nitroprusside on potassium-stimulated ⁴⁵Ca uptake (K-stimulated ⁴⁵Ca uptake) by P₂ fraction of Gray and Whittaker from rat brain were investigated. During preincubation with these reagents, the contents of cyclic GMP in synaptosomes increased, reaching maximum levels within 2 min. On preincubation for 2 min, NaN₃, an activator of membrane bound guanylate cyclase, inhibited K-stimulated ⁴⁵Ca uptake, but NH₂OH and sodium nitroprusside did not affect it. Sodium cyanide, another metabolic inhibitor, had no effect on K-stimulated ⁴⁵Ca uptake. There was a correlation between inhibition of K-stimulated ⁴⁵Ca uptake and increase in the cGMP level on preincubation with NaN₃ for various periods. Based on these results role of cGMP in or around the membrane was discussed in relation to the K-stimulated ⁴⁵Ca uptake by P₂ fraction.     

Effect of Na+ on Ca-uptake of the synaptic plasma membrane

Synaptic plasma membranes prepared from rat brain synaptosomes bound ⁴⁵Ca by an ATP-dependent process. The amount of ⁴⁵Ca taken up by the membranes was increased by addition of K⁺ or Rb⁺ but decreased by addition of Na⁺. The inhibitory effect of Na⁺ was more remarkable in presence of KCI than its absence. Furthermore, rapid release of ⁴⁵Ca was observed on addition of Na⁺ (100 meq) to membranes which had been incubated with ⁴⁵Ca and ATP and more than half of the membrane bound ⁴⁵Ca was released within 10 sec under our experimental conditions. The physiological significance of this finding is discussed.     

The release of membrane-bound calcium by radiation and sulfhydryl reagents

Effects of ionizing radiation and of sulfhydryl reagents on the ⁴⁵Ca binding of red cell membranes were studied. Corresponding effects of these agents on potassium leak from intact red cells were also determined. Essentially all the ⁴⁵Ca associated with the ghosts appeared to be bound. Calcium binding could be described by assuming two independent groups of binding sites with dissociation constants of about 6 × 10^?4 m and 2 × 10^?4 m. The total binding capacity was about 2.5 × 10^?4 moles/g ghost protein. Membrane calcium was decreased by radiation and by the two sulfhydryl reagents, p-chloromercuribenzoate (PCMB) and N-ethyl maleimide (NEM). The tightly bound calcium fraction appeared to be most affected by these agents. Changes in potassium leak evoked by varying doses of agents appeared to parallel effects on membrane calcium. These investigations suggest that the increased cation permeability observed after exposure or red cells to radiation or sulfhydryl reagents may be related to alterations in the calcium-binding properties of the cell membrane.     

An experimental study of 226Ra and 45Ca accumulation from the aquatic medium by freshwater turtles (fam. Chelidae) under varying Ca and Mg water concentrations

Snapping turtles Elseya dentata (Gray) from Magela Creek, Northern Territory, were exposed under laboratory conditions for up to 30 days to waters resembling the inorganic composition of Magela Creek water during the Wet season, with background and elevated Ca and Mg concentrations, that were labelled with ²²⁶Ra and ⁴⁵Ca. The resulting concentrations of ⁴⁵Ca in muscle, skin, gut, liver, shell bone and leg bone of E. dentata equilibrated or approached equilibrium by 12–18 days. Among the experiments, the concentrations of ⁴⁵Ca in all six tissues were inversely related to turtle mass. An increase in the Ca water concentration by a factor of 15 increased the ⁴⁵Ca concentration in all six tissues. The arithmetic factors of increase in the concentration in each tissue were proportional or more than proportional to the factor of increase in Ca water concentration; this factor was highest for muscle tissue (26.6). An increase in the Mg water concentration by a factor of 48 reduced the ⁴⁵Ca concentration in all tissues except skin where it increased. The concentration of ²²⁶Ra in each tissue (except the gut) was positively related to its ⁴⁵Ca concentration and inversely related to turtle mass in muscle, skin and liver. With the exception of the skin, the increased Ca water concentration did not reduce the ²²⁶Ra in the tissues but increased the ²²⁶Ra concentration in bone and muscle. The increased Mg water concentration had an inverse effect on the ²²⁶Ra concentrations in all tissues except shell. With the exception of the skin the effects of increased Ca and Mg water concentrations and turtle size on ²²⁶Ra concentrations in the tissues of E. dentata were similar to their effects on ⁴⁵Ca tissue concentrations, indicating the similar metabolic behaviour of ²²⁶Ra and ⁴⁵Ca in E. dentata.Exposures of the species Elseya latisternum (Gray), Emydura signata (Ahl) and Chelodina longicollis (Shaw), which are the same or closely related to species reported to occur in Magela Creek, to ⁴⁵Ca-labelled Sydney tap water for 7 days demonstrated their ability to also accumulate ⁴⁵Ca from their aquatic medium. The patterns of ⁴⁵Ca concentrations in the tissues of these species indicated that they were inversely related to turtle mass, as demonstrated in E. dentata. The concentrations of ⁴⁵Ca accumulated in the tissues were also comparable to those found in single specimens of E. dentata and E. victoriae (Gray) that were exposed for 7 days to simulated Magela Creek water. The data also indicated the larger long-necked C. longicollis accumulated less ⁴⁵Ca per gram of tissue than similar-sized, short-necked species E. signata and E. latisternum, suggesting that long-necked turtles from Magela Creek would accumulate less ²²⁶Ra from their aquatic medium than similar-sized short-necked species.The capacity of E. dentata to accumulate ²²⁶Ra from the aquatic medium is about two orders of magnitude less than that of the tissue of the freshwater mussel Velesunio angasi (Sowerby) exposed under similar experimental conditions.     

Calcium isotope fractionation by intracellular amorphous calcium carbonate (ACC) forming cyanobacteria

The formation of intracellular amorphous calcium carbonate (ACC) by various cyanobacteria is a widespread biomineralization process, yet its mechanism and importance in past and modern environments remain to be fully comprehended. This study explores whether calcium (Ca) isotope fractionation, linked to ACC-forming cyanobacteria, can serve as a reliable tracer for detecting these microorganisms in modern and ancient settings. Accordingly, we measured stable Ca isotope fractionation during Ca uptake by the intracellular ACC-forming cyanobacterium Cyanothece sp. PCC 7425. Our results show that Cyanothece sp. PCC 7425 cells are enriched in lighter Ca isotopes relative to the solution. This finding is consistent with the kinetic isotope effects observed in the Ca isotope fractionation during biogenic carbonate formation by marine calcifying organisms. The Ca isotope composition of Cyanothece sp. PCC 7425 was accurately modeled using a Rayleigh fractionation model, resulting in a Ca isotope fractionation factor (Δ⁴⁴Ca) equal to −0.72 ± 0.05‰. Numerical modeling suggests that Ca uptake by these cyanobacteria is primarily unidirectional, with minimal back reaction observed over the duration of the experiment. Finally, we compared our Δ⁴⁴Ca values with those of other biotic and abiotic carbonates, revealing similarities with organisms that form biogenic calcite. These similarities raise questions about the effectiveness of using the Ca isotope fractionation factor as a univocal tracer of ACC-forming cyanobacteria in the environment. We propose that the use of Δ⁴⁴Ca in combination with other proposed tracers of ACC-forming cyanobacteria such as Ba and Sr isotope fractionation factors and/or elevated Ba/Ca and Sr/Ca ratios may provide a more reliable approach.     

A possible role of the phosphorylation of synaptic membrane proteins in the control of calcium ion permeability

Incubation of synaptosomes under conditions which result in complete phosphorylation of membrane bound accepter proteins does not affect the permeability to Na⁺ or K⁺ as measured by a spectrophotometric method. This technique was not, however, sensitive enough to determine permeability to Ca²⁺ which was thus estimated using ⁴⁵Ca²⁺. It was found that although phosphorylation did not affect the equilibrium binding of ⁴⁵Ca it did lower the rate of both Ca²⁺ uptake and efflux. The most likely interpretation of these results is that phosphorylation of proteins in the synaptic membrane lowers the permeability of the membrane to Ca²⁺. This could have a role in the regulation of synaptic transmission.     

Calcium efflux from human erythrocyte ghosts

Summary The passive Ca efflux from human red cell ghosts was studied in media of differing ion compositions and compared to the ATP-dependent Ca efflux. Cells were loaded with⁴⁵Ca during reversible hemolysis, and the loss of radioactivity into the non-radioactive incubation medium was measured, usually for 3 hr at 37°C. Analysis of the efflux curves revealed that⁴⁵Ca efflux followed the kinetics of a simple two-compartment system. In the concentration range between 0 and 1mm Ca in the external solution ([Ca⁺⁺] _o ), the rate constant of passive Ca efflux (k min^–1, fraction of⁴⁵Ca lost per minute into the medium) increased from 0.00732 to 0.0150 min^–1. There was no further increase at higher [Ca⁺⁺] _o . The relation between the rate constant of Ca efflux and [Ca⁺⁺] _o is thus characterized by saturation kinetics. The passive transfer system for Ca could also be activated by Sr. The alkali metal ions Na, K and Li did not seem to have any significant influence on passive Ca transfer. The passive Ca efflux was slightly inhibited by Mg and strongly inhibited by Pb. Under most experimental conditions, a fraction of 15 to 50% of the intracellular Ca seemed to be inexchangeable. The inexchangeable fraction decreased with increasing [Ca⁺⁺] _o and increased with increasing [Ca⁺⁺] _i . It was not influenced by alkali metal ions, CN or Pb, but it could be completely removed from the cells by the addition of 0.1mm Mersalyl to the incubation medium or by hemolysis with addition of a detergent. The active ATP-dependent Ca transport differed characteristically from passive transfer; the rate constant decreased with increasing [Ca⁺⁺] _o , and the inexchangeable Ca fraction increased with increasing [Ca⁺⁺] _o . The experimental results suggest that there exists a carrier-mediated Ca–Ca exchange diffusion in the erythrocyte membrane and that only a fraction of the ghost cell population participates in the Ca exchange diffusion.     

Uptake and release of 45Ca by Myxicola axoplasm

The binding and release of 45Ca by axoplasm isolated from Myxicola giant axons were examined. Two distinct components of binding were observed, one requiring ATP and one not requiring ATP. The ATP- dependent binding was largely prevented by the addition of mitochondrial inhibitors, whereas the ATP-independent component was unaffected by these inhibitors. The ATP-independent binding accounted for roughly two-thirds of the total 45Ca uptake in solutions containing an ionized [Ca2+] = 0.54 microM and was the major focus of this investigation. This fraction of bound 45Ca was released from the axoplasm at a rate that increased with increasing concentrations of Ca2+ in the incubation fluid. The ions Cd2+ and Mn2+ were also able to increase 45Ca efflux from the sample, but Co2+, Ni2+, Mg2+, and Ba2+ had no effect. The concentration-response curves relating the 45Ca efflux rate coefficients to the concentration of Ca2+, Cd2+, and Mn2+ in the bathing solution were S-shaped. The maximum rate of efflux elicited by one of these divalent ions could not be exceeded by adding a saturating concentration of a second ion. Increasing EGTA concentration in the bath medium from 100 to 200 microM did not increase 45Ca efflux; yet increasing the concentration of the EGTA buffer in the uptake medium from 100 to 200 microM and keeping ionized Ca2+ constant caused more 45Ca to be bound by the axoplasm. These results suggest the existence of high-affinity, ATP-independent binding sites for 45Ca in Myxicola axoplasm that compete favorably with 100 microM EGTA. The 45Ca efflux results are interpreted in terms of endogenous sites that interact with Ca2+, Cd2+, or Mn2+.