Abstract
The fluid flow in the lacunar-canalicular system of bone is an essential mechanical stimulation on the osteocyte networks. Due to the complexity of human physical activities, the fluid shear stress on osteocyte bodies and processes consists of both steady and oscillatory components. In this study, we investigated and compared the intracellular calcium ([Ca2+]i) responses of osteocytic networks under steady and oscillatory fluid flows. An in vitro osteocytic network was built with MLO-Y4 osteocyte-like cells using micro-patterning techniques to simulate the in vivo orderly organization of osteocyte networks. Sinusoidal oscillating fluid flow or unidirectional steady flow was applied on the cell surface with 20 dyne/cm2 peak shear stress. It was found that the osteocytic networks were significantly more responsive to steady flow than to oscillatory flow. The osteocytes can release more calcium peaks with higher magnitudes at a faster speed under steady flow stimulation. The [Ca2+]i signaling transients under the steady and oscillatory flows have significantly different spatiotemporal characters, but a similar responsive percentage of cells. Further signaling pathway studies using inhibitors showed that endoplasmic reticulum (ER) calcium store, extracellular calcium source, ATP, PGE2 and NO related pathways play similar roles in the [Ca2+]i signaling of osteocytes under either steady or oscillating flow. The spatiotemporal characteristics of [Ca2+]i transients under oscillating fluid flow are affected more profoundly by pharmacological treatments than under the steady flow. Our findings support the hypothesis that the [Ca2+]i responses of osteocytic networks are significantly dependent on the profiles of fluid flow.
Keywords: Osteocyte, Mechanotransduction, Calcium Response, Fluid Flow, Steady, Oscillatory
Introduction
Osteocyte networks in bone tissue can sense various mechanical stimuli generated by physical activities and act as an coordinator in the bone remodeling process by regulating both osteoclast and osteoblast activities [1–3]. The heterogeneous deformation across bone tissue induced by mechanical loading creates fluid pressure gradients in the lacunar-canalicular system (LCS), where the osteocytes reside in. This pressure gradient generates fluid flow across the LCS, which can induce shear stresses up to 50 dyne/cm2 upon the osteocyte membrane and processes [4–6]. Fluid flow is regarded as an essential mechanical stimulation in the mechanobiology of osteocytes. Due to the versatile nature of human daily activities, the profiles of mechanical loading on bones are complex. Therefore the fluid flow upon osteocytes could be a combination of various patterns, including oscillating fluid flow and unidirectional flow. The oscillating flow is often correlated to cyclic movement of the skeletal system such as walking and running. The unidirectional steady flow can represent a physiological but unusual mechanical stimulus, e.g., a posture change of the human body from sitting to standing [7]. Previous studies showed that the mechanically adaptive responses of bone are dominated by “abnormal” strain changes under unusual loading rather than by the numerous cycles of “normal” loadings [8]. Therefore osteocytes respond more actively to new patterns or types of mechanical loadings than to ordinary mechanical stimulation. Osteocytes are known to be able to differentiate the temporal pattern of flow stimulation with distinct biochemical activities to regulate bone remodeling [1, 9, 10].
Little is known about the mechanobiology effects of different fluid flow profiles on osteocytic networks. To date there has only been one study that compared the responses of osteoblastic cells under the stimuli of steady and oscillatory flows [7]. Significant difference in calcium signaling was revealed in osteoblasts under two flow patterns. The oscillating flow, assumed to be the major stimulation on bone cells, was a much less potent stimulator than the steady flow on osteoblastic cells. We recently found that osteocytic networks, as the dedicated mechanical sensors in bone, are much more sensitive to fluid shear stress than the osteoblasts [11]. The intracellular calcium ([Ca2+]i) signaling of osteocytes showed significantly different spatiotemporal characteristics with osteoblasts. Unlike the osteoblasts on bone surfaces, osteocyte networks are directly situated inside the LCS. Therefore it is important to understand and compare the responses of osteocytes under different flow patterns, which are associated with mechanical loading profiles on bone and further affect the bone remodeling process.
Intracellular calcium [Ca2+]i signaling is one of the earliest responses in bone cells under mechanical stimulation that initiates a number of essential downstream signaling pathways, e.g., ATP and PGE2 release, and is typically observed to oscillate dramatically within seconds after mechanical stimulation [4, 12–15]. This ubiquitous signaling molecule plays a critical role in a wide variety of physiological processes in bone cells including proliferation, differentiation, and cell responses to mechanical stimuli [16–18]. The calcium wave propagation across neighboring cells acts as an effective mechanism for the cell-cell communication in bone cell networks [14, 19, 20]. The characters of [Ca2+]i signaling of bone cells are shown to be dependent on the mechanical loading profiles [21]. We have shown that osteocytes can release multiple spike-like [Ca2+]i peaks under unidirectional fluid flow, up to 17 [Ca2+]i peaks during a 9-minute flow stimulation. The spatiotemporal properties of the [Ca2+]i transients are also found to be dependent on the magnitude of fluid flow. Therefore [Ca2+]i oscillations of osteocytes can be employed as a sensitive signaling pathway to correlate the cell responses with different external mechanical stimuli.
The fluid flow induced elevation of cytosolic calcium comes mainly from two sources: intracellular stores (e.g., endoplasmic reticulum, ER) and the extracellular environment [13, 22]. The release of ER calcium store is mainly regulated by the inositol trisphosphate (IP3) pathway, which can be initiated by the activation of purinergic receptors on the cell membrane [16, 17]. After the cytosolic calcium concentration is elevated to a critical level by intra/extracellular sources, the depleted intracellular calcium stores tend to recover their calcium reservation to original levels and become ready for the next release of calcium [16, 23]. When a bone cell is under fluid flow induced shear stress, the activation of gap junction hemichannels (connexin 43) induces ATP efflux from the cytosol to the pericellular environment [24]. Extracellular ATP can elicit a significant [Ca2+]i response by binding to the purinergic membrane receptors [25]. Fluid shear stress can also prompt the induction of COX-2 protein and further PGE2 release in osteoblast-like cells (Norvell et al., 2004). It was previously reported that fluid shear stress can elicit nitric oxide production in osteocytes and osteoblasts accompanied by an increased expression of nitric oxide synthase (NOS) [26, 27]. Nitric oxide modulates [Ca2+]i signaling via a cyclic guanosine monophosphate (cGMP) dependent pathway [28] or nitrosylation of proteins [29]. Moreover, nitric oxide could directly contribute to the [Ca2+]i release via triggering of an influx pathway that is, in part, responsible for the refilling of internal calcium stores [30].
Most studies of bone cell mechanotransduction under oscillatory flow used monolayer osteoblastic cells [7, 31–34]. The osteocytes, unlike the osteoblasts residing on the bone surface, are embedded inside the mineralized bone tissue with a regular pattern. The intercellular spacing and the topology of connection dendrites of osteocytes are relatively uniform across the tissue. The osteocytes are connected into an extensive network through the gap junctions on processes. Gap junctions are membrane-spanning channels, where each pair of connexons (i.e. hemichannels) forms a cylinder with a pore in the center through which small molecules (<1 kDa) can pass from one cell to another [35]. It is widely accepted that this intercellular connection plays a significant role in coordinating bone cell network activities. Messenger molecules mentioned previously, such as IP3 and calcium, can directly transfer between the neighboring cells through gap junctions and thereby mediate propagation of [Ca2+]i signaling in bone cells [20, 36]. The [Ca2+]i signaling of osteocytes within a controlled cell network connected by gap junctions under different flow stimuli has yet to be obtained experimentally.
In this study, we hypothesize that the [Ca2+]i signaling of osteocytic networks is dependent on the profiles of fluid flow. [Ca2+]i responses was employed as the primary outcome variable to compare the physiological responses of in vitro osteocytic networks under steady and oscillatory fluid flows. The roles of several essential intracellular signaling pathways in [Ca2+]i signaling of osteocytic networks were also investigated and compared under two different temporal flow profiles using pharmacological inhibitors.
Materials and Methods
Chemicals
Fetal bovine serum (FBS), calf serum (CS), and penicillin/streptomycin (P/S) were obtained from Hyclone Laboratories Inc (Logan, UT). Trypsin/EDTA, octadecanethiol, dimethyl sulfoxide (DMSO), fibronectin, 18α-glycyrrhetinic acid (18α-GA), suramin, and thapsigargin (TG) were obtained from Sigma-Aldrich Co (St. Louis, MO). Minimum essential alpha medium (α-MEM), calcium free Dulbecco's modified eagle medium (DMEM), and calcium-free Hank's balanced salt solution (HBSS) were obtained from Invitrogen Corporation (Carlsbad, CA). N-(2-Cyclohexyloxy-4-nitrophenyl) methanesulfonamide (NS-398) and NG-monomethyl-L-arginine (L-NMMA) were from EMD Chemicals Inc (San Diego, CA).
Cell Culture and Osteocytic Network
Osteocyte-like MLO-Y4 cells (a gift from Dr. Lynda Bonewald, University of Missouri-Kansas City, Kansas City, MO) were cultured on type I rat tail collagen (BD Biosciences, San Jose, CA, USA) coated Petri-dish in α-MEM supplemented with 5% FBS, 5% CS and 1% P/S [37]. Cells were maintained at 37°C and 5% CO2 in a humidified incubator and not allowed to exceed 70–80% confluence in order to maintain the dendritic characteristic of MLO-Y4 cell line. Micro-contact printing and self-assembled monolayer (SAM) surface chemistry technologies were employed to construct in vitro osteocytic networks to best simulate the osteocyte network in LCS. The detailed protocol was presented in previous studies [12, 38, 39]. In brief, a grid mesh cell pattern was printed on a chromium mask, and then the pattern was replicated to a master, made of positive photoresist (Shipley 1818, MicroChem Corp, Newton, MA). Polydimethylsiloxane (PDMS, Sylgard 184, Dow Corning, Midland, MI) stamps were made using the master. To build an osteocytic network on a glass slide, an adhesive SAM (octadecanethiol) was inked onto a gold coated glass slide with the stamp. Ethylene glycol terminated SAM solution (HS-C11-EG3; Prochimia, Sopot, Poland) was then added onto the slide to form a non-adhesive SAM in non-stamped regions, in order to effectively resist cell adhesion. To further improve the cell attachment on the adhesive SAM inked regions, the glass slide was incubated in a 1% fibronectin solution for one hour before cell seeding. Fibronectin can only attach on the adhesive SAM region. After the monolayer printing, MLO-Y4 cell suspension medium was dropped onto the slide for cell seeding. Fig. 1A shows a fluorescent image of a typical osteocytic network, in which each cell resides on a round island, which is connected with four neighboring islands through fibronectin coated lines. The cells extend their dendrites through these lines to establish gap junctions with the neighboring cells [38].
Figure 1.
Micro-patterned osteocytic network, laminar fluid flow chamber, profiles of shear stress stimulation and the definition of spatial-temporal parameters of [Ca2+]i transients. (A) Fluorescent image of a typical MLO-Y4 cell network used for fluid flow test. The cells were loaded with Fura-2 AM to indicate intracellular calcium ions. Each cell attaches on a round island and connects with four neighboring cells through functional gap junctions. The round island for cell attachment is 15 µm in diameter, while the cell-cell distance is 50 µm. Each island was connected with four neighboring islands through 2 µm width lines. Scale bar = 30 µm. (B) The glass slide with micro-patterned osteocytic network was mounted in a laminar fluid flow chamber. The flow rate was generated by a high-resolution magnetic gear pump (for steady flow) or a motor driven Hamilton syringe (for oscillatory flow) to apply 20 dyne/cm2 shear stress on the cell surface. The fluid flow rate and shear stress are correlated through Poiseuille’s equation. (C) The profiles of shear stress generated by steady and oscillatory fluid flow. The frequency of oscillatory flow is 1 Hz, and the peak stress is ±20 dyne/cm2. (D) Spatiotemporal parameter definition in a typical [Ca2+]i intensity history of MLO-Y4 cells under fluid flow stimulation. [Ca2+]i responses of bone cells were recorded for ten minutes: one minute for baseline and nine minutes during fluid flow stimulation. The [Ca2+]i intensity was represented by average image intensity inside cell normalized over its baseline level. Number of [Ca2+]i peaks, magnitude of 1st peak m1, time to 1st peak t1, and relaxation time of 1st peak t2 were defined in this figure.
[Ca2+]i Imaging and Fluid Flow Stimulation
To indicate the fluctuation of [Ca2+]i intensity, the osteocytic network was loaded with 10 µM Fura-2 AM (Molecular Probes, Eugene, OR) for 45 minutes and then rinsed with fresh working medium (phenol-red free α-MEM with 2% FBS and 2% CS) three times. The glass slide with cells was mounted into a parallel plate flow chamber for laminar fluid flow stimulation tests (Fig. 1B) [13]. The chamber was mounted on an inverted fluorescent microscope (Olympus IX71, Melville, NY), and left undisturbed for 15 minutes, which has been shown to be sufficient for bone cells to recover from mechanical disturbances and to generate repetitive [Ca2+]i response [40]. The fluorescent images of the osteocytic network were recorded by a high-speed CCD camera (ORCA-ER-1394, Hamamatsu Photonics K.K., Hamamatsu City, Japan) for a 10-minute period, one minute for baseline and 9 minutes after the onset of fluid flow. Fura-2 340 nm/380 nm ratio images were used to obtain the fluctuation history of [Ca2+]i by measuring the average image intensity of each cell using MetaMorph and MetaFluor Imaging Software 7.0 (Molecular Devices, Downingtown, PA). The intensity of [Ca2+]i was normalized by the baseline of each cell.
To generate steady fluid flow in the laminar flow chamber, a magnetic gear pump was connected to the chamber with rigid walled tubing to push the fresh working medium through with a desired constant flow rate. The oscillatory flow was driven by a Hamilton glass syringe which was connected to a crank-rocker mechanism. The rocker was driven by a DC motor rotating at 1 Hz which results in a sinusoidal oscillatory laminar flow in the chamber [7]. The shear stress of the steady flow or peak shear stress of oscillatory flow on cell surfaces was controlled at 20 dyne/cm2. The profiles of oscillatory and steady flow were illustrated in Fig. 1C.
[Ca2+]i Signaling Related Pathways
To identify the potential cellular mechanisms activated by different fluid flow profiles, the osteocytic networks were separated into eight groups for each flow pattern. With exception to the untreated and vehicle (DMSO) control groups, the fluid flow experiments were performed with the presence of six specific pathway inhibitors. Each inhibitor can block a major [Ca2+]i signaling related pathway in bone cells (Fig. 2). (1) Extracellular calcium depletion: Calcium-free DMEM and calcium-free HBSS were used to replace the regular medium in flow tests. (2) ER calcium store depletion: Cell networks were incubated in 1 µM thapsigargin medium to deplete the calcium in the ER store a half hour before flow tests [25]. (3) PGE2 blocking: Cell networks were treated with 10 µM NS-398 for 24 hours before and during the flow test, which can selectively inhibit the COX-2 enzyme activity and further block the PGE2 release [41]. (4) NO blocking: 100 µM L-NMMA was introduced into the cell culture medium one day before seeding the cells on slides and continuously presented in medium afterwards. L-NMMA inhibits the production of nitric oxide via competitively inhibiting all three isoforms of nitric oxide synthase (NOS) [42]. (5) Gap junction blocking: 75 µM 18α-GA, a reversible gap junction blocker which binds to membrane proteins and causes disassembly of gap junction plaques [43], was supplied in fluid flow medium to investigate the roles of gap junction in calcium wave propagation [36]. (6) Extracellular ATP pathway blocking: 100 µM suramin, a general P2 purinergic receptor blocker, was applied to the cell networks 30 minutes before fluid flow stimulation [44]. The concentrations of above agents were selected according to the relevant literature where they have been demonstrated to be effective on bone cells. We have used both 18α-GA and NS-398 in bone explant studies for long term (up to 4 weeks) and have not observed osteocyte cell death (Chan et al 2009). Each individual group included more than three slides with patterned cell networks. The numbers of total analyzed cells in each group were summarized in Table 1.
Figure 2.
A schematic of calcium signaling pathways in osteocytes investigated in present study. The increase of Ca2+ intensity in cytoplasm has two major sources, the extracellular Ca2+ in medium and intracellular calcium store in ER. Ion channels, such as voltage gated calcium channels, ligand gated ion channels and stretch-activated ion channels can transfer Ca2+ between intra- and extracellular environments. The calcium in ER store can be released by activation of IP3 sensitive channels. [Ca2+]i signaling in bone cells can induce ATP release through hemi-channels on membrane. ATP can further activate the purinergic receptors which are correlated with PLC and IP3 pathway. Gap junction between neighboring cells provides a physical channel for small molecules (e.g., IP3 and Ca2+) to diffuse between two connected cells. As two of the essential signaling pathways involved in bone mechanotransduction, PGE2 and NO pathways were investigated to identify their correlations with mechanical loading induced [Ca2+]i responses.
Table 1.
Number of analyzed cells in different experimental groups.
| Pathway | Untreated | NO | ATP | Ca2+ Free |
Vehicle | PGE2 | GJ | ER Store |
|---|---|---|---|---|---|---|---|---|
| Oscillatory | 412 | 394 | 225 | 152 | 396 | 398 | 323 | 134 |
| Steady | 441 | 131 | 95 | 66 | 151 | 139 | 125 | 111 |
Data Analysis and Statistics
A cell was defined as responsive to the fluid flow stimulation if it released a calcium spike with a magnitude four times higher than its fluctuations during the period of baseline measurement [45]. Responsive percentage of cells in each group was defined as the number of responsive cells divided by the total number of analyzed cells in the group. To quantitatively analyze the spatial-temporal characteristics of the [Ca2+]i transients, a set of parameters were defined as shown in Fig. 1D. The number of [Ca2+]i peaks during the stimulation period, the magnitude of the 1st [Ca2+]i peak, and the time to reach the first peak after the onset of fluid flow were measured and compared between different groups. Student t-tests were used to determine significant difference of spatiotemporal parameters between oscillatory and steady flows. One-way analysis of variance (ANOVA) with Bonferroni’s post hoc analysis was performed to determine statistical differences between mean values of different pathway inhibited groups. L-NMMA, suramin and Ca2+ free medium treated groups were compared with the untreated group. Since NS398, 18α-GA and thapsigargin were originally dissolved in DMSO, the results from these three groups were compared with those of DMSO vehicle control group. All data reported are mean ± standard deviation of the values of all responsive cells. Statistical significance was defined as p < 0.05
Results
A set of typical [Ca2+]i transients of MLO-Y4 cells under oscillatory and steady fluid flow stimulation are shown in Fig. 3. Both flow patterns induced prominent [Ca2+]i oscillations in MLO-Y4 cells. Under oscillating flow stimulation, the cell released a [Ca2+]i peak at the onset of flow and a few weaker peaks afterwards with reduced magnitudes. Under steady flow stimulation, MLO-Y4 cells tended to release repetitive and spike-like [Ca2+]i peaks with no attenuation in magnitude. A single cell can release up to 17 [Ca2+]i peaks in 9 minutes under steady flow, but at most 6 [Ca2+]i peaks under oscillating flow.
Figure 3.
A set of typical [Ca2+]i responses of MLO-Y4 cells under steady and oscillatory fluid flow stimulations. The flow starts at the 60th second and lasts for 9 minutes in both tests.
The responsive percentages of MLO-Y4 cells under oscillating (96%) and steady (95%) fluid flow had no significant difference. Less than 5% of cells failed to respond to 20 dyne/cm2 shear stress stimulation (Fig. 4A). The number of multiple [Ca2+]i peaks was much higher under steady flow (4.3±2.8) than under oscillating flow (2.4±1.6) (Fig. 4B). 58% MLO-Y4 cells can release three or more [Ca2+]i peaks under 9-minute steady flow stimulation. The same percentage decreased to 21% under oscillatory flow stimulation. The average magnitude of the first [Ca2+]i peak under steady flow (3.3±2.6) was significantly higher than that under oscillating flow (2.5±1.5), and it took the cells significantly shorter time to reach the first peak under steady flow (21±11 seconds vs. 37±29 seconds under oscillatory flow).
Figure 4.
Comparison of spatiotemporal characteristics of the first [Ca2+]i peaks in MLO-Y4 cells under oscillatory and steady fluid flow: (A) percentage of responsive cells, (B) average number of [Ca2+]i peaks, (C) magnitude of the 1st [Ca2+]i peaks, and (D) time from onset of fluid flow to reach the 1st [Ca2+]i peak (*: p < 0.05).
The responsive percentages of all sixteen pharmacological treated groups were summarized in Fig. 5. Under both flow patterns, MLO-Y4 cells showed no [Ca2+]i responses when calcium free medium were used. Under steady flow stimulation, the responsive percentages are above 85% in all groups except the ER calcium store depleted group (57%). The ER depleted group (57%) and ATP pathway blocked group (87%) showed significantly lower responsive percentages than the corresponding control groups under steady flow. Under oscillatory flow stimulation, the ER depleted group (42%), NO (89%), and ATP (78%) interrupted groups showed significantly lower responsive percentages than corresponding controls, while the 18α-GA treatment increased the responsive percentage (97% vs 87% in vehicle control group). In the NO, ATP, PGE2, and ER calcium store inhibited groups, the responsive percentages of cells are significantly lower under the oscillating flow than the steady flow, while other pharmacological treatment groups showed no significant difference between two fluid flow patterns.
Figure 5.
Percentage of responsive cells under fluid flow with different pathways blocked in MLO-Y4 cells. The blocked pathways are listed below the corresponding pharmacological chemicals employed. L-NMMA, Suramin and Ca2+ free medium treated groups were compared with the untreated group. NS398, 18α-GA and thapsigargin treated groups were compared with the DMSO vehicle control group. The cells treated with Ca2+ free medium had no responses to fluid flow stimulation. * means significant difference with corresponding untreated group, and + with vehicle control group. # represents significant difference between the two connected groups, p < 0.05.
Figure 6 shows the number of [Ca2+]i peaks in all groups. In the NO pathway and ER calcium store interrupted groups, steady flow stimulated cells showed significantly more peaks than corresponding groups under oscillatory flow. The number of [Ca2+]i peaks in the two ATP pathway inhibited groups decreased close to 1 and had no difference under two flow profiles. The ER calcium store depleted groups under both flow profiles showed the average number of [Ca2+]i peaks less than two, significantly lower than corresponding vehicle control groups. When the gap junctions were blocked by 18α-GA, the number of [Ca2+]i peaks under oscillatory flow is higher than the vehicle control group, which is opposite to the result under steady flow. Disruption of NO and PGE2 pathways had no significant influence on the number of [Ca2+]i peaks compared with corresponding control groups. MLO-Y4 cells took significantly longer time to reach the first [Ca2+]i peak under oscillating flow than under steady flow in all groups (Fig. 7). Interestingly, this timing gap is even broadened when the cells were treated with pathway inhibitors. In most groups under steady flow, except the calcium free medium group, chemical treatment showed no significant effect on the time to reach the first [Ca2+]i peaks. In contrast, when MLO-Y4 cells were stimulated with oscillatory flow, the time to reach the first peak was significantly increased in ER store depleted group, ATP, NO and PGE2 pathway blocked groups when compared to the untreated or vehicle groups. The time was lengthened three times in NO blocked group, and twice for ER store depleted groups. Interestingly, no significant difference was detected in the response speed between the vehicle control and 18α-GA treated groups under oscillatory flow.
Figure 6.
The average number of responsive [Ca2+]i peaks in MLO-Y4 cells treated with pharmacological inhibitors. The affected pathways are listed below the corresponding chemicals. * means significant difference with corresponding untreated group, and + with vehicle control group. # represents significant difference between the two connected groups, p < 0.05.
Figure 7.
The time to reach 1st [Ca2+]i peak in MLO-Y4 cells after the start of fluid flow stimulation. The inhibited pathways are listed below the chemicals employed. * means significant difference with corresponding untreated group, and + with vehicle control group. # represents significant difference between the oscillatory and steady flow groups, p < 0.05.
Discussion
In this study, the calcium signaling of osteocytic networks was investigated and compared under the stimulation of steady or oscillatory fluid flow. The results clearly demonstrated that the oscillatory flow is significantly less potent than the steady flow to osteocytes. Osteocytes tend to release more frequent [Ca2+]i peaks with higher magnitudes under the stimulation of steady fluid flow than under the oscillatory flow. Previous studies on monolayer osteoblastic cells also showed that in vitro oscillating flow is far less stimulatory than the unidirectional flow [7]. The responsive percentage, but not the response amplitude, of osteoblasts is dependent on the flow profiles. Thus an “all or nothing” [Ca2+]i response character was proposed for osteoblastic cells under fluid flow stimuli [7]. In the present study, however, the responsive percentages of osteocytes show no significant differences between the two flow patterns, but significant differences in the spatiotemporal characters were observed in the [Ca2+]i transients, i.e., more frequent and stronger [Ca2+]i peaks under steady flow than under oscillatory flow. In our previous studies on the calcium signaling of osteocytes under fluid shear stress ranging from 0.5 to 4 Pa, it was also found that the spatiotemporal parameters, but not responsive percentages of osteocytes, are correlated with the strength of fluid shear stress [11]. Therefore the information regarding the profiles of fluid flow is represented by the spatiotemporal characters of [Ca2+]i transients rather than by the responsive percentage of osteocytes. This finding is opposite to that revealed in osteoblasts [7], which further implies that the osteocytes and osteoblasts may incorporate different [Ca2+]i signaling mechanisms under similar mechanical stimuli. Our previous studies also confirmed that the osteocytic and osteoblastic networks had dramatically different [Ca2+]i responses under the same steady fluid flow stimulation. The [Ca2+]i transients of osteocytes are much more dynamic than those of osteoblasts. It has been shown that the expression of T-type voltage gated calcium channels in osteocytes may play an essential role in the spike-like [Ca2+]i responses of MLO-Y4 cells under mechanical stimulation [11, 46, 47].
The exact mechanism of fluid shear stress induced [Ca2+]i signaling in bone cells remains elusive, but several essential pathways in bone remodeling process have been proven to interact with [Ca2+]i responses in osteoblasts [15, 20, 31, 32, 48]. In this study, we found that the fluid flow induced [Ca2+]i responses in osteocytes involve the gap junction, PGE2, NO and ATP related pathways. Purinergic receptors on cell membrane are especially critical for the release of multiple [Ca2+]i peaks in MLO-Y4 cells under both steady and oscillatory flows. The results also proved that the [Ca2+]i responses of osteocytes rely on two major calcium sources, the extracellular calcium in medium and intracellular calcium stored in ER, while the release of ER store has to be initiated by the influx of extracellular calcium. Osteocytic networks stopped responding to fluid flow in calcium-free medium, and the depletion of calcium in ER store significantly reduced the number of [Ca2+]i peaks. Blocking these pathways showed similar effects on the number of [Ca2+]i peaks under both oscillating and unidirectional flow patterns. However, the time to reach the first peak was significantly increased in most chemical-treated groups under oscillating flow stimulation, but not under steady flow. This indicates that the [Ca2+]i transients in osteocytes are more readily affected by pharmacological treatment under oscillating fluid flow, the assumed “normal” stimulation on osteocytes.
Compared with the interruption of ATP pathway, intra- and extracellular calcium sources, the blocking of NO and PGE2 release showed less significant effects on the flow induced [Ca2+]i signaling in MLO-Y4 cells. Since the upregulation of NO release is another early response of osteocytes under fluid flow stimulation, which occurs in a few minutes [49, 50], it is highly possible that NO release and [Ca2+]i signaling can interfere with each other. The production of NO in human bone cells is mainly regulated by the endothelial nitric oxide synthase [51]. According to the time reaching the 1st [Ca2+]i peaks demonstrated in the present study (20 seconds in the control group), the flow induced [Ca2+]i signaling in osteocytes is even faster than the NO release. Therefore it is unlikely the [Ca2+]i signaling is a downstream activity of NO release in flow-stimulated osteocytes. Our previous studies on osteoblasts also showed that activation of NO release has no essential influence on the flow induced [Ca2+]i signaling. The PGE2 release under fluid flow starts even later than NO [49], and the treatment of L-NMMA prevented both NO and PGE2 release in chicken osteocytes, suggesting that the upregulation of PGE2 is dependent on the NO pathway. Thus it is not a surprise that the inhibition of PGE2 release did not reduce the calcium responsive percentage in the present study.
Most pharmacological treatments in this study had negative effects on the [Ca2+]i responses of MLO-Y4 cells. Interestingly, the treatment with 18α-GA increased the responsive percentage and number of peaks in cells under oscillating flow, but not under steady flow, and the speed of calcium response has no significant difference with the vehicle control group. The 18α-GA has been widely used in bone cell research to block the intercellular gap junctions. A number of studies from our group and other groups have proven the effectiveness of this chemical in blocking gap junction and its effect on calcium signaling [11, 12, 14, 15, 19, 24, 36, 43, 52, 53]. Our previous studies using a bone explant model also showed that 18α-GA treatment attenuated the effects of mechanical loading in new bone formation while having minimal toxic effects on osteocyte health in a 4-week long culture [53]. It is interesting that the treatment of 18α-GA on MLO-Y4 cells boosts the calcium responses under oscillatory fluid flow. Identifying the exact mechanisms responsible for this unexpected result may require extensive studies, which is beyond the scope of this present work. However, this result from 18α-GA treatment revealed a critical difference between the stimulative effects of steady and oscillatory flow in osteocyte mechanotransduction. Finally, it is important to note the limitations of the usage of chemical inhibitors. Each pharmacological chemical may have complex effects on the cells besides its major functions. Therefore, a thorough understanding of the mechanisms of these pathways in calcium signaling may require comprehensive studies using a combination of various techniques.
Osteocytic networks are regarded as the major mechanical sensor in bone modeling and remodeling processes. A number of studies showed that the bone is more sensitive to the change of mechanical environments rather than the magnitude or duration of loading [54]. Partitioning exercise into multiple sessions is much more effective for “training” bone to be stronger [55]. Five jumps per day can significantly increase the bone volume and fracture stiffness in rats [56]. However, little information is available about the correlation between the loading profiles and osteocyte behaviors. During cyclic movement of the human body, such as walking and running, a normal oscillatory fluid flow is expected in the LCS in bone. However, a posture change, such as from sitting to standing, may induce a constant, nonhomogeneous strain field in the bone. Due to the low permeability of LCS and the dense glycocalyx surrounding the osteocyte processes, this pressure gradient in the LCS may generate a minutes-long, steady fluid flow on osteocytes. Our recent study demonstrated a high viscoelasticity in osteocyte cytoskeletal networks under fluid flow loading [57]. The cell deformation slowly “creeps” to the equilibrium state under the constant push from a unidirectional flow. This process could take minutes under 1 Pa shear stress. Therefore the stress and strain developed in the cell body and processes under steady flow could be significantly higher than those under oscillatory flow. The difference in deformation amplitudes of the cell membrane and cell body may contribute to the differences in [Ca2+]i signaling revealed in the present study. Previous research using MC3T3-E1 cells also found that the stretch-activated membrane channel, blocked using gadolinium chloride, is not important for cell response to oscillatory fluid flow [32], but calcium responses were inhibited by blocking this channel under steady flow [13, 22]. Furthermore, mechanotransduction responses in MC3T3-E1 cells were shown to be induced by a mechanism that involves the reorganization of the actin cytoskeleton under unidirectional steady fluid flow [58], while exposure to oscillatory fluid flow failed to result in the development of F-actin stress fibers in osteoblastic cells [34]. Combining all of these factors with the results in this study, it is clear that the different stimulation effects of steady and oscillatory flows are related to the distinct strain fields developed in the cytoskeleton under two flow patterns. Another significant difference between steady and oscillatory flows is the effective volume of medium which the cells are exposed to. The cells are exposed to much more medium under the steady flow than the oscillatory flow. Therefore, essential biochemical factors for [Ca2+]i signaling within the medium would be depleted more rapidly under steady flow, and the messengers secreted from cells, such as ATP, would accumulate faster and higher within the small volume of oscillating medium. Identifying the existence and mechanisms of these factors could be a challenging yet important direction for future studies on this topic.
Conclusion
In summary, this study proved that fluid flow can induce robust intracellular calcium responses in osteocytic networks. The responsive percentage of osteocytes is not dependent on the flow patterns, but the spatiotemporal characteristics of calcium transients varies significantly under steady and oscillatory flows. Osteocytes can release more intracellular calcium peaks with higher magnitudes under steady flow than under oscillatory flow, i.e., steady flow is more stimulative to osteocytes than oscillatory flow. Experiments using pharmacological inhibitors demonstrated that extracellular calcium source in medium, intracellular calcium store in ER, and purinergic receptors on cell membrane are essential for calcium signaling of osteocytes under fluid flow stimulation.
Highlights.
► Intracellular calcium signaling of osteocytes is dependent on the profiles of mechanical stimulation. ► Osteocytic networks are more responsive to steady fluid flow than to oscillatory fluid flow. ► Responsive percentages of osteocytes have no significant difference under steady and oscillatory flows. ► Spatiotemporal characters of the calcium signaling transients in osteocytes vary significantly under different flow profiles. ► Endoplasmic reticulum calcium store, extracellular calcium source, and ATP pathways are critical for osteocytes to release multiple calcium peaks under the stimulation of fluid flow.
Acknowledgments
We thank Dr. L. Bonewald for her generous gift of MLO-Y4 cells.
Funding sources
NIH grant R21 AR052417, R01 AR052461, and RC1 AR058453 (XEG).
Footnotes
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Disclosures/conflicts of interest
The authors have nothing to disclose, and have no conflicts of interest.
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