Extracellular fluid flow and chloride content modulate H+ transport by osteoclasts
© Morethson. 2015
Received: 26 February 2015
Accepted: 28 July 2015
Published: 15 August 2015
Bone resorption takes place within the basic multicellular units (BMU), and the surface to be resorbed is isolated from adjacent bone surfaces by a sealing zone between osteoclast membrane and bone matrix, which defines the limits of the resorption lacuna. Considering that the extracellular fluid (ECF) in both BMU and the resorption lacuna can be isolated from its surroundings, I hypothesize that flow and ion composition of the bone ECF in these sites might contribute to the regulation of osteoclast H+ secretion. To investigate this hypothesis, I evaluated the H+ secretion properties of individual osteoclasts and osteoclast-like cells (OCL-cells) and investigated whether changes in flow or chloride content of the extracellular solution modify the H+ secretion properties in vitro.
The results show that 1) osteoclasts are unable to secrete H+ and regulate intracellular pH (pHi) under continuous flow conditions and exhibit progressive intracellular acidification; 2) the cessation of flow coincides with the onset of H+ secretion and subsequent progressive intracellular alkalinization of osteoclasts and OCL-cells; 3) osteoclasts exhibit spontaneous rhythmic oscillations of pHi in non-flowing ECF, 4) pHi oscillations are not abolished by concanamycin, NPPB, or removal of extracellular Na+ or Cl−; 5) extracellular Cl− removal modifies the pattern of oscillations, by diminishing H+ secretion; 6) pHi oscillations are abolished by continuous flowing of ECF over osteoclasts and OCL-cells.
The data suggest, for the first time, that ECF flow and Cl− content have direct effects on osteoclast H+ secretion and could be part of a mechanism determining the onset of osteoclast H+ secretion required for bone resorption.
Bone resorption is important for maintaining mineral homeostasis, adapting to functional loading, and healing damaged and fractured sites. The process of bone consumption is regulated by the number of osteoclasts, and relies heavily on the ability of individual osteoclasts to secrete H+ through the ruffled border, thus lowering the extracellular pH (pHo) at a delimited bone surface.
The first demonstration of an acidic area adjacent to osteoclasts utilized the fluorescent probe acridine orange . Later, it was shown—using pH microelectrodes—that osteoclasts can acidify the contact zone with a culture dish to less than pH 3 within a few minutes . It has been proposed that extracellular acidification is a key step for the dissolution of the apatite-containing mineralized matrix [3, 4] and osteoclast intracellular pH (pHi) regulation [5–8]; in addition, H+ secretion creates a suitable pH, in the resorption lacuna, for enzymes to degrade the organic matrix . Therefore, bone resorption depends on the expression and activity of H+-secreting proteins at the osteoclast ruffled border.
Several mechanisms have been implicated in contributing to the acidification of the resorption lacuna; such as: H+ secretion through vacuolar H+-ATPase (V-ATPase)  and a H+-coupled Cl− secretion, by chloride channel 7 (ClC-7) . Furthermore, the Na+/H+ exchanger, NHE-10 isoform , and a H+ conductance have been reported to regulate pHi by means of acid secretion [5, 6, 13].
Osteoclast activity and function depends on chemical signaling from cellular and paracrine interactions between osteoclasts and osteoblasts, as well as bone marrow and immune cells, and is regulated by several hormones and cytokines . One of the most important signals for induction of osteoclast differentiation and function is the receptor activator of nuclear kappa-B ligand (RANK-L).
Physical stimuli, for instance functional loading and exercise, also play a role in controlling bone formation, resorption and remodeling. Mechanical loading of bone promotes osteocyte responses to fluid shear stress, which results in changes in the osteocyte activity [21–24] and indirect inhibition of osteoclast formation and bone resorption .
Despite the crucial role of osteoclasts in physiological mineral homeostasis and bone adaptive responses, direct effects of flow and ECF ion composition on osteoclast function are otherwise not known. The primary goal of this work is to investigate the effect of extracellular fluid flow rate (5 mL/min versus 0 mL/min) and Cl− content on osteoclast H+ secretion. The results show that both extracellular fluid flow and Cl− content modify osteoclast H+ transport.
Results and discussion
H+ secretion after acid load varies among cells in the absence of extracellular solution flow
It was observed that osteoclasts do not properly regulate pHi after the NH4Cl prepulse in the presence of continuous ECF flow; these cells exhibited a progressive intracellular acidification (n = 6) after discrete recovery from the acid load, which is evidenced by the small ΔpHi (Fig. 2a.) In contrast, when ECF flow was stopped, the osteoclasts secreted H+ at different rates (dpHi/dt) after the acid load (Fig. 2b), resulting in a higher value of ΔpHi in comparison to that obtained under continuous ECF flow. During the first two minutes following the acid load, the dpHi/dt varies from 0.01 to 0.58 pH units/min (n = 27). The values for each osteoclast studied are presented in Additional file 2. The rates of H+ secretion do not appear to be related to cell size; however, there is a positive correlation (r = 0.4522, p = 0.0089, n = 27; one-tailed Pearson) between dpHi/dt and the magnitude of acidification (i.e. the difference between initial pHi and the lowest pHi recorded after NH4Cl solution removal). This correlation was also reported by Ravesloot et al.  and may be related to the amount of H+ to be transported after the acid load.
Osteoclasts and OCL-cells exhibit an oscillatory pHi in non-flowing extracellular solution
Under no ECF flow conditions, H+ secretion after the acid load causes intracellular alkalinization to a maximal pHi value. Subsequently, the cells initiate a period of spontaneous cellular acidification to a minimal pHi value; then the alkalization restarts. This oscillatory pattern is repeated in regular periods of spontaneous acidification and alkalinization (Fig. 3a). These rhythmic pHi fluctuations were observed in both osteoclasts and OCL-cells, and were observed in 92 % of experiments performed in the absence of ECF flow. Different patterns of pHi oscillation, with different amplitudes and periods, were also observed (Fig. 3b). In osteoclasts, the period of the oscillations—the time interval between two maximum pHi values—ranged from 12 to 45 min (n = 35), and the amplitude of the pHi oscillations—the difference between the maximum and minimum pHi in each cycle—ranged from 0.12 to 1.43 pH units, the lowest and the highest values recorded, respectively. This huge variation in capability of H+ secretion among osteoclasts could be due to unequally expression of H+-transporting proteins at the plasma membrane, and can be taken as an additional evidence for the osteoclast heterogeneity regarding resorptive machinery already reported by Everts et al. in . Despite the fact that osteoclasts differ from each other in values for period and amplitude of oscillations, one osteoclast analyzed individually exhibits a regular, rhythmic, oscillation, maintaining the range of pHi fluctuation from one cycle to the following and maintaining the period of the oscillations.
The present study is not the first one to report oscillations related to pHi in osteoclasts. In fact, an in situ study using microelectrodes to simultaneously measure H+ currents and pH in the microenvironment beneath adherent osteoclasts, showed that there were pH fluctuations in that compartment . Despite the methodological differences—extracellular versus intracellular measurements—both processes detect pH changes directly related to H+ transported by the osteoclast.
Inhibition of H+-transporting proteins does not abolish the pHi oscillation, but the absence of extracellular Cl− modifies its patterns
While this may come as a surprise, this is not the first time such an observation has been reported. Grano et al.  demonstrated that in OCL-cells, Na+/H+ exchanger inhibition did not completely eliminate the ability of these cells to regulate pHi. Another study also showed that total replacement of extracellular Na+ had no effect on H+ transport in inside-out vesicles derived from the ruffled border of avian osteoclasts . Furthermore, it has been reported that 40 % of osteoclasts containing at least 10 nuclei facilitate pH recovery from acid load through H+-ATPase, without any participation from the Na+/H+ exchanger . While this latter observation is in contrast to our observed results with concanamycin, our data is in accordance with Nordström et al. , which reported that in the absence of HCO3 −, pHi regulation by H+-ATPase is negligible in cells under physiological pH.
The removal of extracellular Cl− (n = 3) or application of NPPB (n = 3), inhibitor of chloride channels, also did not abolish the pHi oscillations (Fig. 4c and d). However, it should be noted that the removal of extracellular Cl− resulted in noticeable difference in the oscillation pattern (n = 3) (Fig. 4d). In control solution, the difference between two maximum values of pHi (pHi max; Fig. 4e) in two consecutive cycles was −0.03 ± 0.004, whilst in the absence of extracellular Clˉ, the difference between two consecutive values of pHi max raised to −0.10 ± 0.007, indicating a compromised ability to secrete H+. The mean time of intracellular acidification (T; Fig. 4e) was ~6 min under control conditions and was increased to ~9 min in the absence of extracellular Clˉ, which may be related to a decreased ability to secrete H+. The mean time of intracellular alkalinization (t; Fig. 4e) was ~15 min under control conditions and was reduced to ~12 min in the absence of extracellular Clˉ, thus shortening the time of H+ secretion by 20 %. In control solution, the difference between two minimum values of pHi (pHi min; Fig. 4e) in two consecutive cycles was −0.01 ± 0.007, whilst in the absence of extracellular Clˉ, the difference between two consecutive values of pHi min raised to −0.12 ± 0.003, indicating further intracellular acidification. Lastly, the mean rate of intracellular alkalinization (dpHi/dt; Fig. 4e) was 0.004 pH units/min under control conditions versus 0.0008 pH unit/min in the absence of extracellular Clˉ, which corresponds to a 5-fold decrease in the H+ secretion rate. Since the experiments were performed in the absence of HCO3 − and because the variations in pHi and dpHi/dt are related to H+ transport, the reduced ability to secrete H+ in the absence of extracellular Cl− could be due to a impaired exchange of external Cl− for internal H+ by a Cl−/H+ exchanger.
The importance of Cl− transporting proteins (channels) in bone resorption emerged when Blair et al.  demonstrated that in avian osteoclasts the H+ secretion through H+-ATPase was dependent on an anion conductance, and non-linearly related to the external concentration of Cl−. In fact several Cl−-transporting proteins are expressed at the osteoclast ruffled border in different species, including ClC-3, ClC-7, and CLIC5 [32–34]. Cl− secretion through these proteins would dissipate the transmembrane potential generated by H+-ATPase activity .
According to my hypothesis, the absence of extracellular Cl− reduces the exchange of Clˉ by intracellular H+, therefore reducing H+ secretion, without any participation of H+-ATPase. This is supported by data demonstrating that the knockdown of ClC-7 expression by interfering RNA reduces the ability of lysosomal acidification in vivo, concluding that ClC-7 is the most important protein for lysosomal acidification . It is also important to consider that bone ECF is not in equilibrium with the bulk extracellular fluid, but instead there is evidence of such a compartimentalization . Higher concentrations of Cl− in bone ECF compared to other extracellular compartments in the body can be taken as evidence that an important physiological role for Cl− exists in bone.
Taken together, the literature and my results provide evidence supporting the following assertion: ClC-7 may itself secrete H+ through the ruffled border at the bone-osteoclast interface. This new functional role for ClC-7 presented here is in contrast with the function of charge dissipation, in which Cl− ions would leave the cell in parallel with protons transported by H+-ATPase . On the other hand, my hypothesis is in accordance with the first documented biophysical properties of chloride-transporting proteins located at the ruffled border, which was shown to be outward rectifying channels . My proposal of a direct role of ClC-7 in secreting H+ at the ruffled border is also in accordance with studies showing that the resorption lacuna of cultured osteoclasts lacking ClC-7 is less acidic .
Fluid flow abolishes pHi oscillations and causes intracellular acidification, but the cessation of flow coincides with the onset of the H+ secretion
As previously described in this work, osteoclasts and OCL-cells exhibited spontaneous pHi oscillations in the absence of ECF flow, even in the presence of inhibitors of H+ secreting proteins. However, when the ECF was applied at 5 mL/min—value in accordance to the normal intraosseous blood flow rate range reported by Laroche (2002) —the oscillations of pHi were completely abolished in both osteoclasts and OCL-cells. Furthermore, H+ secretion after the acid load was absent or brief and not sustained, in both osteoclasts and osteoclast-like cells (OCL-cells) (Fig. 2a).
This regulation of H+ transport by fluid dynamics of ECF may be relevant during BMU assembly, whereby the canopy over the site to be resorbed isolates local conditions from that in the bulk ECF. In addition, it provides new evidence for a role to intraosseous circulation in regulating the events occuring in the BMU, as highlighted by Parfitt (2000) . The modulation of osteoclast H+ secretion by the fluid dynamics here described, along with the regulation of osteoclast function by hypoxia described by Arnett et al. (2003) , may also serve as regulatory mechanisms for bone resorption in situations where there is stasis or a disruption of the blood supply, such as that occuring in bone fractures or in compression sites during orthodontic treatments.
In summary, I observed that in the presence of ECF flow, osteoclasts and OCL-cells appear to be unable to secrete H+ and the pHi continuously falls. In contrast, when extracellular fluid flow is stopped the cells begin to secrete H+ and pHi increases as extracellular pH reduces. The oscillations in osteoclast pHi could be due to the reversion of ion fluxes (i.e. H+ and Cl−) across the osteoclast plasma membrane. Therefore, it is hypothesized that extracellular Cl− alters the rate of H+ secretion by the exchange of Cl− and H+ mediated by ClC-7 at the ruffled border. This provides novel evidence for the participation of ClC-7 in osteoclast H+ secretion and bone resorption.
My data highlight, for the first time, that flow and Cl− content of the ECF both modulate H+ secretion by the osteoclast, independently of H+-ATPase, and suggest different and potentially more important roles for ClC-7 in bone resorption than previously recognized. Further studies must be performed in order to better understand these aspects of osteoclast biology.
Isolation of osteoclasts from long bones
Generation of OCL-cells in vitro
For differentiation of precursor cells in OCL-cells, marrow cells were collected from long bones of 6 to 8 weeks-old Wistar rats. All experimental procedures were performed in accordance with the guidelines of the Standing Committee on Animal Research of the University of São Paulo (Protocol No. 090-35/02). Osteoclast-like cells were generated as described by Arnett et al.  with modifications; briefly, by using 50 ng/mL of recombinant mouse macrophage colony stimulating factor (rmM-CSF) (R&D Systems, Minneapolis, MN) and 10 ng/mL of recombinant mouse receptor activator of nuclear factor kappa B ligand (rmRANK-L) (R&D Systems). Cells were maintained in 300 mOsm/L α-MEM containing 20 IU/L penicillin G, 20 μg/L streptomycin and 0.05 μg/L of amphotericin B, 10 % of fetal calf serum and 20 mM HEPES on plastic coverslips, in a CO2 incubator (Lab-Line Instruments, India) at 5 % CO2, pH 7.4 at 37 °C, for up to 7 days. The culture medium was changed every 3 or 4 days.
Experimental solutions and chemicals
All pHi experiments were performed in the absence of NaHCO3, in order to avoid activity of proteins involved in base transport (i.e. Na+-HCO3 − cotransporters). The composition of experimental solutions is shown as additional data. The experimental solutions were maintained at 37 °C regardless of flow conditions.
Concanamycin (Sigma-Aldrich, St. Louis, MO), the H+-ATPase inhibitor, was used at a final concentration of 100 mM . NPPB [5-Nitro-2-(3-phenylpropylamino) benzoic acid] (Tocris Bioscience, Bristol, UK), the chloride channel inhibitor, was used at a final concentration of 100 μM . ZnCl2 (Sigma-Aldrich, St. Louis, MO), the proton channel inhibitor, was used at a final concentration of 100 μM .
The changes in cellular pHi were monitored by measuring the change in 12 μM BCECF-AM (Molecular Probes, Eugene, OR) fluorescence on an Olympus IX70 microscope. The emitted fluorescence after excitation at 490 nm (EF 490 nm) is related to pHi, and that emitted after excitation at 440 nm is insensitive to pHi, but indicates dye concentration and dye loss by photobleaching during fluorescence records. The pHi was analyzed in the presence or absence of inhibitors of H+ ATPase, proton channels and ClC-7; in the presence or absence of extracellular Na+ or Cl−, in order to inhibit Na+ and Cl−-dependent mechanisms, respectively; and in the presence (5 mL/min) or absence (0 mL/min) of extracellular fluid flow. The flow and/or exchange of the ECF were controlled using syringe pump (Warner Instruments, Hamden, CT).
I also investigated the effect of acid loading the osteoclasts by exposing the cells to a solution of 20 mM NH4Cl for 1–2 min . The entry of NH3 into the cell causes a transient alkalinization of pHi due to the reaction of NH3 with intracellular H+ forming the ion NH4 +; subsequently, the entry of NH4 leads to intracellular acidification. The replacement of NH4Cl solution for a standard HEPES-buffered solution (pH 7.4, at 37 °C) causes the pHi to fall abruptly. The osteoclasts ability to secrete H+ after the acid load was investigated over time in the presence or absence of ECF flow. The rates of H+ secretion were calculated as the linear regression—dpHi/dt—for the two first minutes after the lowest pHi value induced by the NH4Cl prepulse was obtained, or for the entire period in the analysis of pHi oscillations.
The ratiometric approach was used to generate a parameter related to pH rather than dye concentration . Briefly, the emitted light (above 510 nm) after excitation at 490 nm (EF490) and 440 nm (EF440) was recorded using the MetaFluor 7.1 software. The emitted fluorescence after excitation at 490 nm is sensitive to both dye concentration and pHi, and the emitted fluorescence after excitation at 440 nm (isosbestic wavelength) is not sensitive to changes in pHi. The fluorescence ratio values (R = EF490/EFI440) were converted to pHi using a calibration technique involving the use of high-[K+]/nigericin (10 μM) Invitrogen, Waltham, MA) as previously described . Detailed calibration was performed on a set of cells and a single-point calibration was routinely performed at the end of all the pHi records. Representative pHi values of individual osteoclasts and OCL during the course of the experiments were plotted versus time.
At the Department of Physiology and Biophysics, Institute of Biomedical Sciences, University of Sao Paulo, I would like to thank Drs. Gerhard Malnic, Margarida de Mello Aires and Raif Musa Aziz for thoughtful discussions and for making their laboratory available for experiments. At University College of London, I would like to thank to Dr. Timothy Arnett for helpful advice on osteoclast research protocols.
This work was supported by the Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq), Brasil. PM was recipient of fellowship from CNPq (Process N. 142097/2006-3).
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