Introduction
Bone is constantly remodeled through the balanced activities of osteoblasts and osteoclasts. Whereas genetic defects of bone-forming osteoblasts typically result in delayed bone development and osteoporosis, mutational inactivation of bone-resorbing osteoclasts leads to osteopetrosis, a condition of high bone mass accompanied by immunologic defects due to bone marrow displacement1, 2. Through their ability to release calcium from the mineralized bone matrix, osteoclasts are also involved in calcium homeostasis, which is mediated mostly by the action of parathyroid hormone (PTH) triggering increased bone resorption3. Likewise, hypocalcemia and hyperparathyroidism have been observed in individuals with infantile malignant osteopetrosis, and there are a few case reports describing rachitic widening of the growth plate, a phenotype that has been termed osteopetrorickets4, 5, 6.
Because osteoclasts resorb bone through extracellular acidification, it is not surprising that most of the known human osteopetrosis mutations affect genes involved in acid production and secretion7. These include CA2, encoding the proton-generating cytoplasmic enzyme carbonic anhydrase 2; CLCN7, encoding the transmembrane chloride transporter CLC-7; and OSTM1, encoding a presumptive
-subunit of CLC-7 (refs. 8,9,10). Moreover, TCIRG1, the gene most commonly mutated in individuals with osteopetrosis, encodes a subunit of the vacuolar ATPase, a proton pump mediating acidification of intracellular organelles11. The physiological importance of the Tcirg1 protein (also termed ATP6i, ATP6v0a3 or OC116) for bone resorption was first demonstrated through the generation of a strain of mouse deficient in this gene that then developed osteopetrosis due to a cell-autonomous defect of osteoclast-mediated extracellular acidification12. A deletion within the Tcirg1 gene was subsequently found in oc/oc mice, a spontaneously occurring osteopetrotic mouse model13, 14. Moreover, genetic screening of humans with infantile malignant osteopetrosis revealed that inactivating TCIRG1 mutations account for approximately 50% of cases15, 16, 17, 18.
Notably, the initial characterization of Tcirg1-deficient oc/oc mice revealed an osteopetrorickets phenotype—again, high bone mass accompanied by rachitic widening of the growth plates and defects of skeletal mineralization19. However, the importance of Tcirg1 for cartilage and bone mineralization was not fully investigated thereafter, as histology was performed only after decalcification of the specimens. Moreover, to our knowledge there have been no systematic studies on the importance of functional osteoclasts for calcium homeostasis and skeletal mineralization, and the reported osteoclast-specific expression of Tcirg1 did not provide a sufficient explanation for the osteopetrorickets phenotype of the oc/oc mice12, 20.
Here we have analyzed non-decalcified bone biopsy specimens from individuals with osteopetrosis and found defects of skeletal mineralization in fewer than 50% of them, suggesting that osteopetrosis and osteopetrorickets are distinct phenotypes. This was confirmed by comparison of two mouse models, Src-/- and oc/oc, which show osteopetrosis and osteopetrorickets phenotypes, respectively19, 21. The defects of skeletal mineralization in oc/oc mice result from severe hypocalcemia and can be prevented by feeding the mice a high-calcium diet. To assess how Tcirg1 deficiency triggers hypocalcemia, we next analyzed the expression pattern of Tcirg1 and found specific expression not only in osteoclasts but also in parietal cells. Our subsequent finding that oc/oc mice display low gastric acid levels (hypochlorhydria) demonstrated that Tcirg1 is physiologically involved in gastric acidification. Finally, to determine whether this previously unknown function of Tcirg1 could explain the osteopetrorickets phenotype of oc/oc mice, we studied Cckbr-/- mice, which lack the cholecystokinin B–gastrin receptor22. We found that these mice, which are known to have a hypochlorhydria phenotype, also have mild hypocalcemia, secondary hyperparathyroidism and increased bone resorption; in addition, mice with deficiencies of both Cckbr and Src have osteopetrorickets. Moreover, Cckbr deficiency by itself triggers an osteoporotic phenotype, which is fully rescued by calcium gluconate supplementation. Together, these results suggest that gastric acid levels, rather than solely affecting osteoclast activity, help determine proper serum calcium levels, and that osteopetrorickets and osteopetrosis are distinct phenotypes.
Results
Osteopetrosis and osteopetrorickets are distinct phenotypes
To analyze whether osteoclast dysfunction is generally associated with defects of skeletal mineralization, we first performed histomorphometry on non-decalcified transiliac bone biopsy specimens from 21 individuals with diagnosed osteopetrosis who had not been previously genotyped. As expected, we observed pathologically high trabecular bone volume, as compared to control biopsy specimens, in all 21 cases (Fig. 1a). In contrast, we found pathologic enrichment of non-mineralized bone matrix (osteoid), indicative of osteopetrorickets, in only ten cases. That this mineralization defect was not caused by excessive bone formation was demonstrated by our observation of diffuse fluorescence, with only occasional discrete fluorochrome labels, following tetracycline administration in the biopsy specimens from these individuals (Fig. 1b). To underscore the differences between the two groups, we carried out histomorphometry, which suggested that osteopetrosis and osteopetrorickets are distinct phenotypes that can be distinguished by quantifying osteoid thickness and osteoid volume (Fig. 1c).
Figure 1: Osteopetrosis (OPT) and osteopetrorickets (OPR) are distinct phenotypes.
(a) Von Kossa/van Gieson staining of non-decalcified bone biopsy specimens. Normally mineralized bone matrix is stained black and non-mineralized osteoid is stained red. The Histomorphometric quantification of the trabecular bone volume per tissue volume (BV/TV) is shown below (here and throughout, values are given as mean
s.d.). **P < 0.005 versus the control group (n = 12). Scale bars, 400
m. (b) Fluorescence micrographs from the same specimens showing tetracycline-labeled bone surfaces. Scale bars, 200
m. (c) Histomorphometric quantification of osteoid thickness (O.Th.) and osteoid volume per bone volume (OV/BV). **P < 0.005 versus the control group. Here and throughout, box plots denote the mean and the 25th–75th percentile range. (d) Contact radiographs of whole skeletons (top) and vertebral bodies (middle), as well as von Kossa/van Gieson staining of non-decalcified vertebral sections (bottom), from wild-type (WT), Src-/- and oc/oc mice at 2 weeks of age. Scale bars, 2 cm, 2 mm and 0.5 mm. (e) Contact radiographs (top) and non-decalcified histology of tibias (middle and bottom). Scale bars, 2 mm, 1 mm and 200
m. (f) Contact radiographs (top) and non-decalcified histology of calvariae (bottom). Scale bars, 1 cm and 100
m. (g) Histomorphometric quantification of femoral length, growth-plate thickness (GpTh), BV/TV and OV/BV. **P < 0.005 versus WT (n = 5 mice per group).
We confirmed this phenotypic difference between these two conditions through analysis of two osteopetrotic mouse models, Src-deficient mice and Tcirg1-deficient oc/oc mice19, 21. Contact radiographs performed at 2 weeks of age revealed an osteopetrorickets phenotype specifically in oc/oc mice, whose high bone mass was accompanied by rachitic widening of the growth plates and by severe growth retardation—two characteristics not seen in Src-/- mice (Fig. 1d,e). Non-decalcified histology confirmed that only oc/oc mice had a mineralization defect of hypertrophic cartilage and bone matrix, whereas in Src-/- mice the increased bone matrix was normally mineralized (Fig. 1e). We also observed enrichment of osteoid in the absence of Tcirg1 in craniofacial bones, which is important because these bones develop without the formation of a cartilage intermediate (Fig. 1f). Finally, we quantified our observations by histomorphometry, which confirmed that Src-/- mice displayed osteopetrosis, whereas oc/oc mice displayed osteopetrorickets, demonstrating that osteoclast dysfunction does not necessarily cause a defect in skeletal mineralization (Fig. 1g).
Osteopetrorickets in oc/oc mice is caused by hypocalcemia
To assess whether the absence of Tcirg1 in oc/oc mice results in a cell-autonomous defect of skeletal mineralization, we first analyzed Tcirg1 expression in ex vivo cultures of bone cells. As expected, we found Tcirg1 expressed by osteoclasts but not by chondrocytes or osteoblasts. We observed the same pattern in vivo when we performed in situ hybridization on tibia sections from wild-type mice (Fig. 2a,b). Likewise, we did not observe any difference in extracellular matrix mineralization, alkaline phosphatase activity or osteocalcin production when primary osteoblasts from wild-type and oc/oc mice were differentiated ex vivo (Fig. 2c,d). An intrinsic osteoblast defect was further ruled out by the findings that bone mineralization was not affected in oc/oc mice at embryonic day 17.5 (E17.5) and that the osteopetrorickets phenotype developed postnatally (Fig. 2e,f). These observations can be explained by the fact that embryonic development of oc/oc mice occurs in oc/+ mothers, which were normocalcemic (Fig. 2g); after birth, however, oc/oc mice developed hypocalcemia and were not viable beyond the age of 3 weeks.
Figure 2: Osteoid enrichment in oc/oc mice is caused by hypocalcemia.
(a) Top, northern blot for Tcirg1 expression in cultured mouse osteoclasts (Ocl; differentiated for 0, 5 or 10 d as indicated), growth-plate chondrocytes (C; differentiated for 20 d) and osteoblasts (Obl; differentiated for 0, 5, 15 or 25 d) derived from wild-type (WT) mice. Bottom, ethidium bromide staining of RNA. (b) In situ hybridization for Tcirg1 expression in tibias from 3-day-old WT mice at low (left) and at high magnification (right). GP, growth plate; PS, primary spongiosa; Ocl, osteoclasts; Obl, osteoblasts; Ocy, osteocytes. Scale bars, 200
m (left) and 50
m (right). Unless otherwise indicated, arrows indicate osteoclasts. (c) Von Kossa staining for mineralized matrix in primary osteoblasts from wild-type and oc/oc mice after differentiation for 10 or 20 d. Scale bars, 1 cm. (d) Alkaline phosphatase activity (AP) and osteocalcin level (OC) after 20 d of differentiation. (e) Von Kossa/van Gieson staining of non-decalcified vertebral sections from WT and oc/oc mice before (E17.5, left) and after birth (postnatal day 2 (P2), right). Scale bars, 100
m. (f) Quantification of BV/TV and OV/BV. *P < 0.05 versus WT (n = 4 mice per group). (g) Serum calcium and PTH in 2-week-old WT, Src-/-, oc/+ and oc/oc mice. **P < 0.005 versus WT (n = 5 mice per group). (h) Contact radiographs (scale bars, 2 mm) from vertebral bodies (top left) and tibias (bottom left), and von Kossa/van Gieson staining of non-decalcified sections from vertebral bodies (middle left, scale bars, 500
m), tibias (top right, scale bars, 200
m) and calvariae (bottom right, scale bars, 100
m) from 6-week-old WT and oc/oc mice kept on a high-calcium liquid diet. Quantification of OV/BV is also shown.
We next analyzed whether calcium homeostasis would be affected by inactivation of Tcirg1. We found that oc/oc mice were characterized by severe hypocalcemia and hyperparathyroidism, conditions not seen in oc/+ mice or in Src-/- mice (Fig. 2g). To demonstrate that the osteopetrorickets phenotype of oc/oc mice is caused by hypocalcemia, we fed the mice a high-calcium liquid diet, which resulted in normalization of serum calcium levels (10.4
0.2 mg dl-1 in wild-type mice given the same diet versus 9.5 + 3.1 mg dl-1 in oc/oc mice). As the majority of the oc/oc mice receiving this diet survived beyond 3 weeks of age, we performed our histologic analysis at 6 weeks and found that treated oc/oc mice had elevated trabecular bone volume (89.0
6.9% versus 21.6
2.2% in wild-type mice, P < 0.005) but no enrichment of osteoid (Fig. 2h). Taken together, these results demonstrated that the rachitic aspects of osteopetrorickets are caused by hypocalcemia and that the disturbance of calcium homeostasis in the absence of Tcirg1 is not solely explained by osteoclast dysfunction.
Tcirg1 is involved in gastric acidification
To assess how Tcirg1 deficiency triggers hypocalcemia, we first determined urinary calcium levels and found that they were significantly lower in oc/oc mice than in their wild-type littermates (Fig. 3a). Because this finding ruled out a defect of renal calcium reabsorption, it seemed possible that intestinal calcium uptake might be affected in oc/oc mice, and we therefore analyzed Tcirg1 expression in the gastrointestinal tract by RT-PCR. We detected specific expression of Tcirg1 in the fundus, a region of the stomach involved in gastric acid production (Fig. 3b). This finding led us to determine the gastric pH in wild-type, oc/oc and Cckbr-/- mice—the latter serving as a control, as they are known to display hypochlorhydria due to their lower numbers of acid-producing parietal cells22. Whereas all the wild-type mice had gastric pH below 2.5, we observed higher gastric pH not only in Cckbr-/- mice but also in oc/oc mice, thereby demonstrating, for what we believe is the first time, that hypochlorhydria is associated with Tcirg1 deficiency (Fig. 3c).
Figure 3: Tcirg1 is expressed by parietal cells and involved in gastric acidification.
(a) Urinary calcium concentrations in wild-type (WT), oc/+ and oc/oc mice. *P < 0.05 versus WT (n = 4 mice per group). (b) RT-PCR analysis for Tcirg1 expression in the gastrointestinal tract. Expression of the gastric-specific Atp4b gene and the housekeeping gene Gapdh were monitored as controls. (c) Gastric pH in WT, oc/oc and Cckbr-/- mice. *P < 0.05 versus WT (n = 5 mice per group). (d) Immunohistochemistry on a human tissue microarray at low (left) and high magnification (right) using a TCIRG1-specific antibody. Scale bars, 2 mm and 100
m. (e) Non-decalcified histology of a transiliac bone biopsy specimen from an 18-month-old child carrying a homozygous point mutation (R56W) in TCIRG1 and from an age-matched control subject (scale bars, 100
m). Quantification of BV/TV and OV/BV is shown at right. (f) Retrospective analysis of serum parameters from 12 individuals with TCIRG1-dependent autosomal recessive osteopetrosis (OPT). Shown are values for calcium, phosphorus, PTH, 1,25-(OH)2-vitamin D3 and gastrin. *P < 0.05 versus the control group (n = 12).
To evaluate whether this deduced function of Tcirg1 in gastric acidification is also relevant in humans, we used a monoclonal antibody directed against the human TCIRG1 protein to perform immunohistochemistry on tissue microarrays. TCIRG1 was detectable only in the parietal cells of the stomach but not in sections from other organs (Fig. 3d). To determine whether TCIRG1 deficiency in humans results in the same phenotypic abnormalities as are seen in oc/oc mice, we next analyzed bone mineralization and gastric acidification in an individual with TCIRG1-dependent osteopetrosis (Fig. 3e). Although this individual's serum calcium was in the low normal range (2.3 mM), non-decalcified histology revealed high bone mass and a pathologic enrichment of osteoid, indicative of osteopetrorickets. Moreover, the individual's gastric pH was pathologically elevated, remaining between 2.7 and 4.1 and never reaching a normal value (below 2.2) in the course of 24 h of monitoring. We further performed a retrospective analysis of serum parameters from 12 individuals with TCIRG1-dependent osteopetrosis, in which we observed significantly lower serum calcium levels compared to age-matched controls. We also found elevated serum concentrations of PTH, 1,25-vitamin D3 and gastrin, indicative of disturbed calcium homeostasis and hypochlorhydria (Fig. 3f).
Osteopetrorickets due to impaired gastric acidification
By analyzing the bone phenotype of Cckbr-/- mice, we next addressed the question of whether hypochlorhydria results in impaired calcium homeostasis and bone mineralization. In Cckbr-/- mice at 2 weeks of age, although osteoid volume was no larger, we did observe greater growth-plate thickness and significantly lower serum calcium levels compared to those of wild-type littermates (Fig. 4a). Moreover, the Cckbr-/- mice had higher PTH levels and osteoclast numbers, suggesting that a more severe hypocalcemia is prevented by calcium mobilization from the bone matrix. This observation raised the possibility that the combination of hypochlorhydria and osteoclast dysfunction could explain the osteopetrorickets phenotype of oc/oc mice. To confirm this hypothesis, we generated mice deficient in both Cckbr and Src, thereby combining hypochlorhydria and osteoclast dysfunction caused by two independent genetic defects. As expected, when we analyzed the Cckbr-/-Src-/- mice at 2 weeks of age, we found a rachitic widening of the growth plates, a pathologic increase of the osteoid volume and early lethality, three phenotypes that are observed neither in Cckbr-/- nor in Src-/- mice (Fig. 4b). The lethality caused by the combined deficiency of Cckbr and Src is comparable to that of the oc/oc mice, and both the hypocalcemia (7.2
0.7 mg calcium per dl serum) and the hyperparathyroidism (214
82 mg PTH per ml serum) were more pronounced than in mice lacking Cckbr alone.
Figure 4: Osteopetrorickets caused by a combined defect of bone resorption and gastric acidification.
(a) Top, toluidine blue–stained sections from tibias of 2-week-old WT and Cckbr-/- mice. The white bar in each panel indicates the growth plate (scale bar, 100
m). Bottom, TRAP activity staining of osteoclasts (stained in red; scale bar, 50
m). Quantification of GpTh, serum calcium, PTH and osteoclast number per bone surface (OcN/BS) is given on the right. *P < 0.05 versus WT (n = 5 mice per group). (b) Von Kossa/van Gieson staining of non-decalcified sections from tibias of 2-week-old Cckbr-/- and Cckbr-/-Src-/- mice. Scale bars, 500
m and 200
m. Quantification of BV/TV, GpTh, OV/BV and survival curves of three mutant strains are given at right. *P < 0.05 versus Cckbr-/- littermates (n = 5 mice per group). (c) Immunohistochemistry on decalcified human bone biopsy specimens demonstrating osteoclast-specific presence of TCIRG1, CLC-7 and SLC4a2, but no expression of ATP4b. Arrows indicate multinucleated osteoclasts. Scale bars, 100
m. (d) Contact radiographs (scale bar, 2 mm) and von Kossa/van Gieson staining of non-decalcified sections from vertebral bodies (lower left) and tibias (middle top) from 2-week-old WT and Slc4a2-/- mice. Scale bars, 500
m (vertebrae) and 200
m (tibias). Quantification of serum calcium, PTH, BV/TV and OV/BV is also shown. **P < 0.005 versus WT (n = 6 mice per group).
We next investigated whether mice lacking the anion exchanger Slc4a2 would have a similar phenotype, given that Slc4a2-/- mice display not only achlorhydria but also failure of tooth eruption, a typical feature of osteopetrosis23. To address a possible function of Slc4a2 in bone resorption, we first performed immunohistochemistry on sections from decalcified human bone biopsy specimens and found that Slc4a2 was present on osteoclasts (Fig. 4c). Consistent with this finding, Slc4a2-/- mice, which do not survive beyond the age of 3 weeks, had high bone mass, impaired calcium homeostasis and osteoid enrichment—all hallmarks of osteopetrorickets (Fig. 4d). Taken together, these data demonstrate that impaired gastric acidification negatively affects calcium homeostasis and that the combination of this condition with an osteoclast defect causes more severe hypocalcemia and osteopetrorickets.
Cckbr-/- mice develop an osteoporotic phenotype
Because the analysis of 2-week-old Cckbr-/- mice revealed secondary hyperparathyroidism, we next addressed the question of whether hypochlorhydria, in the absence of an osteoclast defect, would trigger osteoporosis. We therefore analyzed the skeletal phenotype of wild-type and Cckbr-/- mice at 12 and 52 weeks of age. Using histomorphometry following non-decalcified sectioning of vertebral bodies, we found that trabecular bone volume was significantly lower in the Cckbr-/- mice at both ages (Fig. 5a,b). We found the same in sections from the tibia, where we also observed severe cortical porosity in 52-week-old Cckbr-/- mice, which we did not see in wild-type controls. To understand the underlying cause of the observed phenotype, we first performed dynamic histomorphometry following dual injection of calcein. Although we did not observe any defect of bone matrix mineralization in the Cckbr-/- mice, their rates of bone formation were significantly lower than those of wild-type controls (Fig. 5c). Yet neither osteocalcin level nor alkaline phosphatase activity were significantly lower in the serum of Cckbr-/- mice versus wild-type controls, suggesting that their osteoporotic phenotype is caused primarily by higher levels of bone resorption (Fig. 5d).
Figure 5: Osteoporotic phenotype of Cckbr-/- mice.
(a) Non-decalcified histology of vertebral bodies (top) and tibias (bottom) from 12- and 52-week-old WT and Cckbr-/- mice. Arrow indicates cortical porosity in the 52-week-old Cckbr-/- mice. Scale bars, 1 mm. (b) Histomorphometric quantification of BV/TV (top, vertebral bodies; bottom, tibia) and trabecular thickness (TbTh). *P < 0.05 versus WT (n = 6 mice per group). (c) Fluorescence micrographs showing calcein-labeled bone surfaces (left) and the deduced bone formation rate per bone surface (BFR/BS) (right) in 52-week-old WT and Cckbr-/- mice. Scale bars, 20
m. *P < 0.05 versus WT (n = 6 mice per group). (d) Serum osteocalcin levels (OC) and alkaline phosphatase activity (AP) of 52-week-old WT and Cckbr-/- mice. (e) Contact radiographs (top; scale bars, 5 mm and 500
m), non-decalcified histology (middle; scale bars, 500
m) and TRAP activity staining (bottom; scale bars, 500
m). Arrows indicate the severe cortical porosity caused by increased bone resorption in the Cckbr-/- mice. (f) Histomorphometric quantification of fibrous tissue per bone surface (FT/BS) and osteoclast surface per bone surface (OcS/BS). **P < 0.005 versus WT (n = 6 mice per group). (g) Urinary abundance of Dpd cross-links in WT and Cckbr-/- mice. Values were normalized to creatinine to control for differences in urine water content. *P < 0.05 versus WT (n = 6 mice per group). (h) Three-point bending assays of the femurs of WT and Cckbr-/- mice. Fmax, required force in newtons (N) until bone failure. *P < 0.05 versus WT (n = 6 mice per group).
In fact, although contact radiography and histologic analysis confirmed the presence of cortical lesions in the femurs of Cckbr-/- mice as well, activity staining for the osteoclast marker TRAP (tartrate-resistant acid phosphatase) revealed that this was due to higher levels of bone resorption (Fig. 5e). To quantify these observations, we performed histomorphometry, which showed that fibrotic tissue and osteoclast number, both indicative of secondary hyperparathyroidism, were pathologically elevated in the cortical bone of the Cckbr-/- mice (Fig. 5f). Higher levels of systemic bone resorption in the Cckbr-/- mice was further confirmed by the elevated concentrations of bone-specific collagen degradation products (Dpd cross-links) in the urine (Fig. 5g). Finally, to demonstrate that these abnormalities negatively affected biomechanical bone stability, we performed three-point bending assays of the femurs and observed that the required force until bone fracture was significantly lower in the absence of Cckbr (Fig. 5h).
The Cckbr-/- phenotype is prevented by calcium supplementation
We next assessed whether normalization of calcium homeostasis through dietary manipulation could prevent the osteoporotic phenotype of Cckbr-/- mice. Our reference diet included 0.8% calcium carbonate and 500 IU kg-1 vitamin D3, and we also used the same diet with 2% calcium carbonate and 2,000 IU kg-1 vitamin D3. In addition, because calcium carbonate is known to be poorly absorbed at elevated gastric pH, we also tested the effect of replacing calcium carbonate with calcium gluconate, which has greater solubility at neutral pH. To compare the efficiency of calcium carbonate and calcium gluconate in preventing hypochlorhydria-induced bone loss, we fed Cckbr-/- mice one of the four diets (0.8% calcium carbonate or calcium gluconate, 2% calcium carbonate or calcium gluconate) and studied their skeletal phenotypes at the age of 52 weeks.
We first analyzed vertebral bodies by contact radiography, which revealed higher bone density in the groups receiving either calcium gluconate or 2% calcium carbonate, results subsequently confirmed by non-decalcified histology and histomorphometry (Fig. 6a,b). Quantification of serum PTH and osteoclast numbers on the trabecular bone surfaces provided an explanation for this observation. Although Cckbr-/- mice receiving the control diet (0.8% calcium carbonate) had secondary hyperparathyroidism and pathologically elevated numbers of osteoclasts, both parameters were significantly improved by the other diets, but only the 2% calcium gluconate diet resulted in complete normalization (Fig. 6c). We observed the same pattern when we determined the biomechanical stability of the vertebral bodies by microcompression testing (Fig. 6d).
Figure 6: Hypochlorhydria-induced bone loss is prevented by calcium gluconate supplementation.
(a) Contact radiographs (top) and von Kossa/van Gieson staining (bottom) of non-decalcified sections from vertebral bodies of Cckbr-/- mice receiving diets containing 0.8% or 2% of either calcium carbonate or calcium gluconate. Scale bars, 2 mm and 1 mm. (b–d) Quantification of BV/TV (b), serum PTH and OcN/BS (c) and microcompression testing of the vertebrae (d). *P < 0.05 for calcium gluconate versus calcium carbonate (n = 6 mice per group). (e) Cross-sectional
CT scanning (top) and von Kossa/van Gieson staining (bottom) of non-decalcified sections from femurs. Scale bars, 500
m and 100
m. (f) Quantification of the cortical porosity and data from three-point bending assays of the femora. *P < 0.05 for calcium gluconate versus calcium carbonate (n = 6 mice per group). (g) Proposed model for the impact of hypochlorhydria on calcium homeostasis and bone mass. In healthy individuals (top), intact gastric acidification is a prerequisite for efficient intestinal uptake of calcium (blue circles). In hypochlorhydria (middle), intestinal calcium uptake (blue arrow) is lower, thereby leading to secondary hyperparathyroidism, osteoclast activation and osteoporosis. In the case of a combined acidification defect of gastric parietal cells and osteoclasts (bottom), PTH-dependent activation of bone resorption is blocked, resulting in severe hypocalcemia and osteopetrorickets.
We next analyzed the femurs of hypochlorhydric Cckbr-/- mice, quantifying their cortical porosity by cross-sectional micro-computed tomography (
CT) scanning and by histology and their biomechanical stability through three-point bending assays. Although mice receiving either 2% calcium carbonate or 0.8% calcium gluconate had reduced cortical porosity, only the diet containing 2% calcium gluconate fully prevented the osteoporotic phenotype (Fig. 6e,f). Likewise, at both concentrations (0.8% and 2%), calcium gluconate was more efficient than calcium carbonate both in reducing cortical porosity and in increasing biomechanical stability of the mouse femurs. Taken together, these results not only demonstrate that hypochlorhydria-induced bone loss is a consequence of secondary hyperparathyroidism but also reveal that calcium gluconate is the most effective calcium formulation for preventing this phenotype, at least in mice.
Discussion
Our results demonstrate that impaired gastric acidification negatively affects calcium homeostasis, thereby triggering either hyperparathyroidism-induced bone loss or, when combined with an osteoclast defect, impaired skeletal mineralization and early lethality due to severe hypocalcemia (Fig. 6g). Given that both pathologies can be normalized by calcium supplementation in mouse models, we believe that our data are also of clinical relevance, not only for osteopetrotic patients but also for many individuals suffering from hypochlorhydria or receiving proton-pump inhibitors.
Osteopetrosis is a severe genetic disorder of impaired bone resorption, which can be treated by bone marrow transplantation because osteoclasts are of hematopoietic origin24, 25. This is especially true for individuals carrying TCIRG1 mutations, as they do not display additional defects of the central nervous system such as are observed with CLC-7 or OSTM1 deficiency26, 27, 28. Moreover, because Tcirg1, unlike Clcn7 and Ostm1, is specifically expressed by osteoclasts, it appeared that the only physiologically relevant function of Tcirg1 is in bone resorption9, 12, 20, 29. However, as stomach expression of Tcirg1 has not, at least to our knowledge, been analyzed before, and as non-decalcified histology of Tcirg1-deficient bones was performed only for the initial characterization of oc/oc mice, we believe that an important aspect of Tcirg1-dependent osteopetrosis has been previously overlooked. In fact, our evidence here suggests that hypochlorhydria is an additional pathology in Tcirg1-dependent osteopetrosis that not only contributes to the severe impairment of calcium homeostasis but most likely remains uncorrected after bone marrow transplantation. Thus, although we do not want to speculate too far about the possible direct impact of our findings on clinical practice, we suspect that it might be useful to monitor gastric acidification, calcium homeostasis and bone mineral density in osteopetrotic patients, even after the initial normalization of bone mass following bone marrow transplantation. In addition, it will be important to implement the use of non-decalcified bone histology in clinical osteopetrosis treatment protocols to evaluate whether other genetic defects of osteoclast function also cause osteopetrorickets or whether this phenotype is specifically associated with the TCIRG1 inactivation.
Although autosomal recessive osteopetrosis is a rare disorder, with an incidence of 1:250,000, hypochlorhydria is common in individuals older than 60 years, with an estimated prevalence in the range of 30%7, 30, 31. In addition, many individuals have elevated gastric pH due to the use of proton-pump inhibitors, which antagonize H+/K+-ATPase, the enzyme principally responsible for gastric acid production32. That impaired gastric acidification can lead to calcium malabsorption has been suggested previously, as calcium carbonate, the calcium supplement most commonly prescribed for osteoporosis therapy, is poorly absorbed in individuals who have achlorhydria or are receiving proton-pump inhibitors33, 34. Most importantly, however, a recently published clinical study has demonstrated that long-term proton-pump inhibitor therapy is associated with an increased risk of hip fracture, suggesting that hypochlorhydria is a risk factor for osteoporosis35.
Therefore, we believe that our data demonstrating hyperparathyroidism-induced bone loss in a mouse model of hypochlorhydria are also relevant to the treatment of osteoporotic fractures, a major public health problem associated with increased mortality and morbidity36. In fact, our demonstration that calcium gluconate supplementation fully alleviates the osteoporotic phenotype of Cckbr-/- mice might have a direct impact on the current treatment for osteoporosis, which involves not only an osteoanabolic agent but also calcium and vitamin D supplementation. In this regard, we believe that it will be important to treat osteoporotic patients who have hypochlorhydria or receive proton-pump inhibitors with calcium supplements that are soluble at neutral pH, such as calcium citrate or calcium gluconate37. Moreover, because these calcium formulations are already available, we hope that our findings will initiate clinical studies analyzing their potential for improving bone health in a large subgroup of osteoporotic patients.

