Strontium as a tracer to study the transport of calcium in the epiphyseal growth plate (electronprobe microanalysis)

Summary At the mineralization front of the epiphyseal growth plate large quantities of calcium (Ca) are necessary to form the mineral (a Ca-phosphate). It is an unsolved problem, whether Ca is transported through the cells of the growth plate cartilage or extracellularly. Electronprobe microanalysis (EPMA) allows the quantitative, morphologically correlated analysis of elements. EPMA can discriminate only different elements. To investigate the transport of Ca, Strontium (Sr) is a very good tracer, as it resembles Ca in many biological reactions.Our results demonstrate that the transport of Sr from the blood into the growth plate and through the growth plate needs only one or a few minutes. The measured intracellular Sr and Ca concentrations are much lower than the extracellular ones, while the intracellular Sr/Ca ratio is not or only a little bit lower than the extracellular one. It must be concluded, that significant amounts of Ca are neither transported through nor accumulated in the cells of the growth plate cartilage. The main transport is an extracellular diffusion. Using Sr as a tracer for Ca new results on the behaviour of Ca could be received.Dedicated to Professor Dr. T.H. Schiebler on the occasion of his 65th birthday     

Zur Resorption von Calcium und Strontium im Dünndarm von Ratte,Maus und Meerschweinchen

The possible modes of permeation of Ca and Sr through the intestinal epithelium are discussed. The problems of the diffusion and the active transport were studied with prepared bags of duodenum, jejunum and ileum of normal but still immature animals (both sexes) in the Warburg apparatus, at body temperature and in some cases at 4° C. Active transport occurs under oxygen, whereas under nitrogen and blockade of the metabolism with cyanide, only diffusion takes place. Isotopes (⁴⁵Ca and⁹⁰Sr) of high specific activity were used. The diffusion of both elements shows the same ratio at low and at body temperature, with an higher intensity of course at 38° C. This ratio (Ca/Sr) is approximately 3 in the duodenum and in the proximal parts of the jejunum; in the distal parts of the intestine, it is approximately 2 or lower. During active transport there is no alteration in these ratios within the serosa in the tissue. Therefore the selection between the two elements takes place immediatly at the entrance in the mucosa. There are only small and negligible differences between rats and mice. In the intestine of guinea pigs, however, a remarkably higher permeation of Ca and lower retention in the tissue, and consequently higher quotients for Ca/Sr, can be observed. The application of Ca-salts (gluconate, lactate) enhances the permeation of Ca and diminishes the entrance of Sr in all animals. The fact that this alteration takes place during conditions of diffusion as well as of active transport supports the assumption that the selection is preferably dependent upon the differences of the physical state of the two ions (atom volume, hydratation of the ions) rather than on their chemical properties.     

Relation Between Simultaneous Ca and Sr Transport Rates in Isolated Segments of Vetch, Barley, and Pine Roots

Root segments of vetch, barley, and pine were exposed to a nutrient solution containing (85)Sr and (45)Ca tracers. Translocation was measured from solutions containing stable ions at concentrations of 2.5 mm Ca, and at either 0.5 mm or 2.5 mm Sr. Polar transport was established between 12 and 18 hr in barley, and between 16 and 22 hr in vetch. Acropetal transport remained below 5% of basipetal transport of tracer during these intervals. Transport in both vetch and barley usually declined before an elapsed time of 24 hr unlike corn, which maintained its steady state beyond 24 hr. Pine was radically different in that it showed no difference between acropetal and basipetal transport rates and had very low rates. Sr transport in all plants studied to date paralleled that of Ca and the ratio Sr:Ca transported was equal to the ratio Sr:Ca in the nutrient. In vetch, stable Ca transport was reduced to one-fifth when Sr concentration was increased from 0.5 mm to 2.5 mm. Yet stable Sr transport did not change, indicating that the effect on transport was not due to competitive inhibition. A similar effect was less pronounced in barley, but could not be detected in pine. The magnitude of the transport rates varied considerably among the various species, corn having the greatest followed by barley, vetch, and pine in decreasing order. Transport did not correlate with root weight or surface area; it amounted to from 0.03 to 0.60 nanomoles per hr in these experiments as compared to 7 nanomoles per hr previously established in corn (in all cases, 55 mm segments, sectioned 10 mm from apex).     

Relation Between Calcium and Strontium Transport Rates as Determined Simultaneously in the Primary Root of Zea mays

Root segments of Zea mays 55 mm long, were exposed to nutrient containing ⁸⁵Sr and ⁴⁵Ca tracers. Translocation rather than uptake was measured, using a newly-designed glass compartmentation system and validated tracer analytic model. Ca transport from solutions containing between 0.25 and 5.0 mm Ca was only slightly affected by concentration, but translocation from 0.25 to 0.05 mm solutions was markedly reduced. Maximum transport of strontium from nutrient containing 0.05 mm Ca was twice that from 2.5 mm Ca, and also twice the maximum calcium transported. Thus, under the condition simulating calcium depletion, i.e., 0.05 mm Ca, greater amounts of strontium were transported. In these cases the solutions also contained stable strontium at concentrations between 0.25 and 5.0 mm. In simultaneous determinations, the ratio of Sr to Ca moved was exactly equal to the ratio of their concentrations in nutrient solution, and there was no evidence of discrimination. Dinitrophenol reduced transport of Sr and Ca to an equivalent extent, amounting to between 2 and 9% of non-treated control levels.     

Role of the progressive ankylosis gene (ank) in cartilage mineralization

Mineralization of growth plate cartilage is a critical event during endochondral bone formation, which allows replacement of cartilage by bone. Ankylosis protein (Ank), which transports intracellular inorganic pyrophosphate (PP(i)) to the extracellular milieu, is expressed by hypertrophic and, especially highly, by terminally differentiated mineralizing growth plate chondrocytes. Blocking Ank transport activity or ank expression in terminally differentiated mineralizing growth plate chondrocytes led to increases of intra- and extracellular PP(i) concentrations, decreases of alkaline phosphatase (APase) expression and activity, and inhibition of mineralization, whereas treatment of these cells with the APase inhibitor levamisole led to an increase of extracellular PP(i) concentration and inhibition of mineralization. Ank-overexpressing hypertrophic nonmineralizing growth plate chondrocytes showed decreased intra- and extracellular PP(i) levels; increased mineralization-related gene expression of APase, type I collagen, and osteocalcin; increased APase activity; and mineralization. Treatment of Ank-expressing growth plate chondrocytes with a phosphate transport blocker (phosphonoformic acid [PFA]) inhibited uptake of inorganic phosphate (P(i)) and gene expression of the type III Na(+)/P(i) cotransporters Pit-1 and Pit-2. Furthermore, PFA or levamisole treatment of Ank-overexpressing hypertrophic chondrocytes inhibited APase expression and activity and subsequent mineralization. In conclusion, increased Ank activity results in elevated intracellular PP(i) transport to the extracellular milieu, initial hydrolysis of PP(i) to P(i), P(i)-mediated upregulation of APase gene expression and activity, further hydrolysis and removal of the mineralization inhibitor PP(i), and subsequent mineralization.     

Uptake and intracellular sequestration of divalent cations in resting and methacholine-stimulated mouse lacrimal acinar cells. Dissociation by Sr2+ and Ba2+ of agonist-stimulated divalent cation entry from the refilling of the agonist-sensitive intracellular pool

The abilities of various divalent cations to enter the cytoplasm of mouse lacrimal acinar cells was examined under resting and agonist-stimulated conditions, by monitoring their effects on the fluorescence of cytosolic fura-2. In vitro, Ni2+, Co2+, and Mn2+ quenched the fura-2 fluorescence, whereas Sr2+, Ba2+, and La3+ produced an excitation spectrum and maximum brightness similar to Ca2+. Stimulation of mouse lacrimal acinar cells with methacholine (MeCh) caused a biphasic elevation of intracellular Ca2+ concentration [( Ca2+]i) resulting from a release of Ca2+ from intracellular pools followed by a sustained entry of extracellular Ca2+. Neither La3+ nor Ni2+ entered the cells under resting or stimulated conditions, but both blocked Ca2+ entry. Although both Co2+ and Mn2+ entered unstimulated cells, this process was not increased by MeCh. Both Sr2+ and Ba2+ were capable of supporting a sustained increase in fura-2 fluorescence in response to MeCh, indicating that these cations can enter the cells through the agonist-regulated channels. However, Sr2+, but not Ba2+, was capable of refilling the agonist-sensitive intracellular stores. These findings demonstrate dissociation of agonist-induced Ca2+ entry from intracellular Ca2+ pool refilling and thereby provide strong support for the recently modified version of the capacitative Ca2+ entry model according to which influx into the cytoplasm occurs directly across the plasma membrane and does not require a specialized cation channel directly linking the extracellular space and the intracellular Ca2+ stores.     

Cytosolic free calcium concentrations in avian growth plate chondrocytes

Isolated avian growth plate chondrocytes convert the acetoxymethyl ester (AM) form of Fura-2 quickly and efficiently to the Ca2(+)-sensitive pentacarboxylic acid (FA) form. Control experiments indicate that the Kd for intracellular Fura-2/FA is very close to that of extracellular Fura-2/FA at the same ionic strength and pH and that the Fura-2/FA fluorescence from indicator converted by intracellular organelles is quite small. Correcting for the effects of extracellular Fura-2/FA and partial hydrolysis products has improved the accuracy of determination of intracellular [Ca2+] over earlier measurements in chondrocytes. Cytosolic [Ca2+] in isolated growth plate chondrocytes (containing cells from each maturational stage) is found to require approximately 9 hours to recover from the isolation process. After this recovery period, cytosolic [Ca2+] in these cells converges to approximately 70 nM regardless of the [Ca2+] of the recovery medium, suggesting regulation of cytosolic [Ca2+] to a set point. Chondrocytes that are separated into maturationally distinct fractions using countercurrent centrifugal elutriation show an increase in cytosolic [Ca2+] with cellular maturation. The least mature resting cells have a [Ca2+] near 57 nM, while the most mature hypertrophic cells are around 95 nM.     

Rapid mobilization of cellular Ca2+ in bovine parathyroid cells evoked by extracellular divalent cations. Evidence for a cell surface calcium receptor

The concentration of intracellular free Ca2+ ([Ca2+]i) was measured in dissociated bovine parathyroid cells using the fluorescent indicator quin-2 or fura-2. Small increases in the concentration of extracellular Ca2+ produced relatively slow, monophasic increases in [Ca2+]i in quin-2-loaded cells, but rapid and transient increases followed by lower, yet sustained (steady-state), [Ca2+]i increases in fura-2-loaded cells. The different patterns of change in [Ca2+]i reported by quin-2 and fura-2 appear to result from the greater intracellular Ca2+-buffering capacity present within quin-2-loaded cells, which tends to damp rapid and transient changes in [Ca2+]i. In fura-2-loaded parathyroid cells, other divalent cations (Mg2+, Sr2+, Ba2+) also evoked transient increases in [Ca2+]i, and their competitive interactions suggest that they all affect Ca2+ transients by acting on a common site. In contrast, divalent cations failed to cause increases in steady-state levels of cytosolic Ca2+. Low concentrations of La3+ (0.5-10 microM) depressed steady-state levels of cytosolic Ca2+ elicited by extracellular Ca2+ but were without effect on transient increases in [Ca2+]i elicited by extracellular Ca2+, Mg2+ or Sr2+, suggesting that increases in the steady-state [Ca2+]i arise from the influx of extracellular Ca2+. Mg2+- and Sr2+-induced cytosolic Ca2+ transients persisted in the absence of extracellular Ca2+ but were abolished by pretreatment with ionomycin. These results show that cytosolic Ca2+ transients arise from the mobilization of cellular Ca2+ from a nonmitochondrial pool. Extracellular divalent cations thus appear to act at some site on the surface of the cell, and this site can be considered a "Ca2+ receptor" which enables the parathyroid cell to detect small changes in the concentration of extracellular Ca2+.     

Intracellular ionic changes in normal and transformed human fibroblasts after extracellular Ca2+ deprivation.

The lowering of extracellular Ca2+ concentration in the growth medium reversibly blocks normal, but not SV40-transformed WI38 diploid fibroblasts in the early G1/G0 phase of the cell cycle. This growth response is characterized by specific changes in ionic content and transport. Ca2+ deprivation (0.03 mM) has little effect on the K+ content of either normal or transformed cells. Na+ content, however, is increased nearly 2-fold in the normal cells. This increase is presumably due to a 3-fold increase in unidirectional Na+ influx in Ca2+-deprived cells. The increased intracellular Na+ also gives rise to a nearly 3-fold enhancement of the active (ouabain-sensitive) Na+ efflux. Ca2+ deprivation causes only slight increases in Na+ influx, ouabain-sensitive Na+ efflux and intracellular Na+ in the transformed cell. In contrast, the transformed cells lose nearly 60% of their intracellular Ca2+ on deprivation, whereas normal WI38 cells lose only 10%. The data suggest that the growth arrest exhibited by the normal cell but not the transformed cell may be related to different membrane-transport and permeability changes in response to Ca2+ deprivation.     

Collagen/annexin V interactions regulate chondrocyte mineralization

Physiological mineralization in growth plate cartilage is highly regulated and restricted to terminally differentiated chondrocytes. Because mineralization occurs in the extracellular matrix, we asked whether major extracellular matrix components (collagens) of growth plate cartilage are directly involved in regulating the mineralization process. Our findings show that types II and X collagen interacted with cell surface-expressed annexin V. These interactions led to a stimulation of annexin V-mediated Ca(2+) influx resulting in an increased intracellular Ca(2+) concentration, [Ca(2+)](i), and ultimately increased alkaline phosphatase activity and mineralization of growth plate chondrocytes. Consequently, stimulation of these interactions (ascorbate to stimulate collagen synthesis, culturing cells on type II collagen-coated dishes, or overexpression of full-length annexin V) resulted in increase of [Ca(2+)](i), alkaline phosphatase activity, and mineralization of growth plate chondrocytes, whereas inhibition of these interactions (3,4-dehydro-l-proline to inhibit collagen secretion, K-201, a specific annexin channel blocker, overexpression of N terminus-deleted mutant annexin V that does not bind to type II collagen and shows reduced Ca(2+) channel activities) decreased [Ca(2+)](i), alkaline phosphatase activity, and mineralization. In conclusion, the interactions between collagen and annexin V regulate mineralization of growth plate cartilage. Because annexin V is up-regulated during pathological mineralization events of articular cartilage, it is possible that these interactions also regulate pathological mineralization.     

Activation of contractility and occurrence of aftercontractions in Ca2+ and Sr2+-solutions during the postnatal development of the rat heart

Activation of isometric contractile force and induction of aftercontractions by different extracellular Ca- and Sr-concentrations during the early postnatal development of the rat heart were studied. In the neonatal (1-15 days) rat heart activation of contractility by [Ca]0 and [Sr]0 were similar when a dose-response curve for Ca was determined before Sr, but if the experiment was performed in the reverse order of the dose-response curve for Sr was shifted to the left. In either case the maximal developed tension was about the same. In the adult (3-5 months) rat heart [Ca]0 higher than 4 mM was inhibitory, whereas contractile force increased up to 16 mM [Sr]0 without any signs of force depression. The dose-response curve for Sr was shifted to the right compared to that of Ca and the maximal developed tension was clearly higher in Sr-solution than in Ca-solution. Aftercontractions appeared for the first time on the 13th and 24th postnatal days for 16 mM [Ca]0 and [Sr]0, respectively. In the adult rat ventricle lower Ca concentrations were needed to induce aftercontractions compared to Sr. Based upon these observations it is suggested that the appearance of aftercontractions during the third postnatal week of rat heart development is due to the maturation of intracellular Ca stores which become available for contractile activation by the development of the T-system. The absence of a negative inotropic effect in elevated Sr concentrations may be due to the slowing down of the transport processes of the sarcoplasmic reticulum (SR) by Sr and to the greater ability of the SR to store Sr over Ca.     

Two modes of inhibition of the Ca2+ pump in red cells by Ca2+

Two different and independent modes of inhibition of the Ca2+ pump by Ca2+ can be detected measuring active Ca2+ extrusion from resealed ghosts of human red cells: one requires extracellular and the other requires intracellular Ca2+. Ki for inhibition by extracellular Ca2+ is about 10 mM. Extracellular Mg2+ replaces Ca2+ in inhibiting Ca2+ transport but with an apparent affinity for inhibition about 3-times less than that for Ca2+. Inhibition by external Ca2+ is not affected by Na+ or K+ at both surfaces of the cell membrane, external EGTA, internal Ca2+ or ATP. The apparent affinity for external Ca2+ progressively raises as pH increases. The effects of extracellular Ca2+ and Mg2+ are consistent with the idea that for Ca2+ pumping to proceed, external sites in the pump must be protonated and not occupied by extracellular Ca2+ or Mg2+. Inhibition by intracellular Ca2+ takes place with a Ki of about 1 mM and is independent of external Ca2+. The inhibitory effects of intracellular Ca2+ can be accounted for if Ca2+ and CaATP were competitive inhibitors of the activation of the pump by Mg2+ and MgATP, respectively.     

An essential role of the yeast pheromone-induced Ca2+ signal is to activate calcineurin.

Previous studies showed that, in wild-type (MATa) cells, alpha-factor causes an essential rise in cytosolic Ca2+. We show that calcineurin, the Ca2+/calmodulin-dependent protein phosphatase, is one target of this Ca2+ signal. Calcineurin mutants lose viability when incubated with mating pheromone, and overproduction of constitutively active (Ca(2+)-independent) calcineurin improves the viability of wild-type cells exposed to pheromone in Ca(2+)-deficient medium. Thus, one essential consequence of the pheromone-induced rise in cytosolic Ca2+ is activation of calcineurin. Although calcineurin inhibits intracellular Ca2+ sequestration in yeast cells, neither increased extracellular Ca2+ nor defects in vacuolar Ca2+ transport bypasses the requirement for calcineurin during the pheromone response. These observations suggest that the essential function of calcineurin in the pheromone response may be distinct from its modulation of intracellular Ca2+ levels. Mutants that do not undergo pheromone-induced cell cycle arrest (fus3, far1) show decreased dependence on calcineurin during treatment with pheromone. Thus, calcineurin is essential in yeast cells during prolonged exposure to pheromone and especially under conditions of pheromone-induced growth arrest. Ultrastructural examination of pheromone-treated cells indicates that vacuolar morphology is abnormal in calcineurin-deficient cells, suggesting that calcineurin may be required for maintenance of proper vacuolar structure or function during the pheromone response.     

Selectivity in biomineralization of barium and strontium

The desmid green alga Closterium moniliferum belongs to a small number of organisms that form barite (BaSO₄) or celestite (SrSO₄) biominerals. The ability to sequester Sr in the presence of an excess of Ca is of considerable interest for the remediation of ⁹⁰Sr from the environment and nuclear waste. While most cells dynamically regulate the concentration of the second messenger Ca²⁺ in the cytosol and various organelles, transport proteins rarely discriminate strongly between Ca, Sr, and Ba. Herein, we investigate how these ions are trafficked in C. moniliferum and how precipitation of (Ba,Sr)SO₄ crystals occurs in the terminal vacuoles. Towards this goal, we simultaneously visualize intracellular dynamics of multiple elements using X-ray fluorescence microscopy (XFM) of cryo-fixed/freeze-dried samples. We correlate the resulting elemental maps with ultrastructural information gleaned from freeze-fracture cryo-SEM of frozen-hydrated cells and use micro X-ray absorption near edge structure (micro-XANES) to determine sulfur speciation. We find that the kinetics of Sr uptake and efflux depend on external Ca concentrations, and Sr, Ba, and Ca show similar intracellular localization. A highly ion-selective cross-membrane transport step is not evident. Based on elevated levels of sulfate detected in the terminal vacuoles, we propose a “sulfate trap” model, where the presence of dissolved barium leads to preferential precipitation of (Ba,Sr)SO₄ due to its low solubility relative to SrSO₄ and CaSO₄. Engineering the sulfate concentration in the vacuole may thus be the most direct way to increase the Sr sequestered per cell, an important consideration in using desmids for phytoremediation of ⁹⁰Sr.     

Evidence of high Ca uptake by cyanobacteria forming intracellular CaCO3 and impact on their growth

Several species of cyanobacteria biomineralizing intracellular amorphous calcium carbonates (ACC) were recently discovered. However, the mechanisms involved in this biomineralization process and the determinants discriminating species forming intracellular ACC from those not forming intracellular ACC remain unknown. Recently, it was hypothesized that the intensity of Ca uptake (i.e., how much Ca was scavenged from the extracellular solution) might be a major parameter controlling the capability of a cyanobacterium to form intracellular ACC. Here, we tested this hypothesis by systematically measuring the Ca uptake by a set of 52 cyanobacterial strains cultured in the same growth medium. The results evidenced a dichotomy among cyanobacteria regarding Ca sequestration capabilities, with all strains forming intracellular ACC incorporating significantly more calcium than strains not forming ACC. Moreover, Ca provided at a concentration of 50 μM in BG‐11 was shown to be limiting for the growth of some of the strains forming intracellular ACC, suggesting an overlooked quantitative role of Ca for these strains. All cyanobacteria forming intracellular ACC contained at least one gene coding for a mechanosensitive channel, which might be involved in Ca influx, as well as at least one gene coding for a Ca²⁺/H⁺ exchanger and membrane proteins of the UPF0016 family, which might be involved in active Ca transport either from the cytosol to the extracellular solution or the cytosol toward an intracellular compartment. Overall, massive Ca sequestration may have an indirect role by allowing the formation of intracellular ACC. The latter may be beneficial to the growth of the cells as a storage of inorganic C and/or a buffer of intracellular pH. Moreover, high Ca scavenging by cyanobacteria biomineralizing intracellular ACC, a trait shared with endolithic cyanobacteria, suggests that these cyanobacteria should be considered as potentially significant geochemical reservoirs of Ca.     

Kinetics and pH-dependence of glycine-proton symport in Saccharomyces cerevisiae

Interactions between intracellular pH (pHi) and H+-coupled transmembrane transport of glycine have been studied by means of 31P-NMR, using both aerobic and 'energy starved' cells of the yeast Saccharomyces cerevisiae. The general features of glycine transport in the yeast strain used (NCYC 239) are similar to those already reported for Saccharomyces carlsbergensis and S. cerevisiae, there being two kinetically distinct glycine uptake systems, with pH-independent K1/2 values near 14 and 0.4mM, respectively, but pH-dependent maximal velocities. Glycine transport itself has no measurable effect on pHi in aerobic cells, and only a marginal effect in energy-starved cells, but changes of pHi, imposed by extracellular addition of butyric acid, strongly influence glycine transport. Indeed, the dependence of glycine influx (in energy-starved cells) upon cytoplasmic H+ concentration appears to be third order, showing Hill slopes of 2.7-3.0. A crucial kinetic role for cytoplasmic pH in glycine transport is further indicated by a proportionality between the decline of flux and the decline of pHi produced by various metabolic inhibitors and uncouplers. Extracellular pH (pHo), by contrast, has only a weak effect on glycine influx, showing a Hill slope of 0.5. The major observations can be accommodated by a simple cyclic carrier scheme, in which 2 or more protons are transported along with glycine, but only one extracellular proton binding site dissociates in the testing range, with a pK near 5.5. The model requires a finite membrane potential, which must be somewhat sensitive to both pHi and pHo, and accommodates the discrepancy between measured net proton flux (one per glycine) and the kinetically required proton flux (two or more per glycine) by shunting through other proton-conducting pathways in the yeast membrane.     

Ca2+-dependent potentiation of the nonselective cation channel TRPV4 is mediated by a C-terminal calmodulin binding site

Most Ca2+-permeable ion channels are inhibited by increases in the intracellular Ca2+ concentration ([Ca2+]i), thus preventing potentially deleterious rises in [Ca2+]i. In this study, we demonstrate that currents through the osmo-, heat- and phorbol ester-sensitive, Ca2+-permeable nonselective cation channel TRPV4 are potentiated by intracellular Ca2+. Spontaneous TRPV4 currents and currents stimulated by hypotonic solutions or phorbol esters were reduced strongly at all potentials in the absence of extracellular Ca2+. The other permeant divalent cations Ba2+ and Sr2+ were less effective than Ca2+ in supporting channel activity. An intracellular site of Ca2+ action was supported by the parallel decrease in spontaneous currents and [Ca2+]i on removal of extracellular Ca2+ and the ability of Ca2+ release from intracellular stores to restore TRPV4 activity in the absence of extracellular Ca2+. During TRPV4 activation by hypotonic solutions or phorbol esters, Ca2+ entry through the channel increased the rate and extent of channel activation. Currents were also potentiated by ionomycin in the presence of extracellular Ca2+. Ca2+-dependent potentiation of TRPV4 was often followed by inhibition. By mutagenesis, we localized the structural determinant of Ca2+-dependent potentiation to an intracellular, C-terminal calmodulin binding domain. This domain binds calmodulin in a Ca2+-dependent manner. TRPV4 mutants that did not bind calmodulin lacked Ca2+-dependent potentiation. We conclude that TRPV4 activity is tightly controlled by intracellular Ca2+. Ca2+ entry increases both the rate and extent of channel activation by a calmodulin-dependent mechanism. Excessive increases in [Ca2+]i via TRPV4 are prevented by a Ca2+-dependent negative feedback mechanism.     

Calcium-calcium and calcium-strontium exchange across the membrane of human red cell ghosts

Summary Stationary and nonstationary state⁴⁵Ca fluxes as well as Sr–Ca exchange movements were studied in energy-depleted human erythrocyte ghosts at different intra-and extracellular Ca concentrations. Influx and efflux followed the kinetics of a closed two-compartment system. The influx and efflux rate constants (k _in andk _out, respectively, fractions of total extra- or intracellular⁴⁵Ca that move in one direction per unit time) were similar in magnitude. They decreased with increasing Ca concentration on the cisside and increased with increasing Ca concentration on the trans-side of the membrane. Hence, the fluxes in both directions were characterized by saturation kinetics and appeared to be partially caused by an exchange diffusion mechanism. In the presence of a moderate inward (up to 8mm) or outward (up to 2mm) Ca concentration gradient, k_in andk _out did not vary in the course of an experiment and did not differ significantly from rates which were measured under stationary state conditions. Extracellular Sr induced an outward transport of intracellular Ca against the concentration gradient (counter-transport). The resulting inward Ca concentration gradient (maximal inside-to-outside concentration ratio as 1 to 3) persisted since extra- and intracellular Sr did not equilibrate. Analogous results were obtained studying⁴⁵Ca–⁴⁰Ca countertransport. In net flow experiments Ca–Sr exchange proved to occur on a one-for-one basis. Ca–Sr exchange was additive to the noncoupled Ca and Sr net downhill movements. The experimental results suggest that a specific ATP-independent Ca transfer system exists in the erythrocyte membrane which acts symmetrically on the two sides of the membrane and is restricted to a tightly coupled one-for-one exchange diffusion.     

The extracellular calcium-sensing receptor and cell-cell signaling in epithelia

In multicellular organisms, cells are crowded together in organized communities, surrounded by an interstitial fluid of extremely limited volume. Local communication between adjacent cells is known to occur through gap junctions in cells that are physically connected, or through the release of paracrine signaling molecules (e.g. ATP, glutamate, nitric oxide) that diffuse to their target receptors through the extracellular microenvironment. Recent evidence hints that calcium ions may possibly be added to the list of paracrine messengers that allow cells to communicate with one another. Local fluctuations in extracellular [Ca2+] can be generated as a consequence of intracellular Ca2+ signaling events, owing to the activation of Ca2+ influx and efflux pathways at the plasma membrane. In intact tissues, where the interstitial volumes between cells are much smaller than the cells themselves, this can result in significant alterations in external [Ca2+]. This article will explore emerging evidence that these extracellular [Ca2+] changes can be detected by the extracellular calcium-sensing receptor (CaR) on adjacent cells, forming the basis for a paracrine signaling system. Such a mechanism could potentially provide CaR-expressing cells with the means to sense the Ca2+ signaling status of their neighbors, and expand the utility of the intracellular Ca2+ signal to a domain outside the cell.     

S-Nitrosothiols: cellular formation and transport

This review will focus on the transport and intracellular formation of S-nitrosothiols in cell culture models. The major points made in this article are: (1) S-Nitrosothiols are actively metabolized by cells. (2) S-Nitrosothiols affect cells in ways distinctly different from those of nitric oxide and can act through mechanisms that do not involve the intermediacy of nitric oxide. (3) Some S-nitrosothiols (S-nitrosocysteine, S-nitrosohomocysteine) can be taken up into cells via amino acid transport system L, whereas others (S-nitrosoglutathione, S-nitroso-N-acetylpenicillamine) are not directly transported, but require the presence of cysteine and/or cystine before the nitroso functional group is transported. (4) Proteomic detection of intracellular S-nitrosothiols is currently possible only if cells are loaded with high levels of S-nitrosothiols, and methodological advances are required in order to examine the S-nitrosated proteome after exposure of cells to physiological levels of nitric oxide.