Marc K. Drezner

Evaluation of a Role for 1,25-Dihydroxyvitamin D3 in the Pathogenesis and Treatment of X-linked Hypophosphatemic Rickets and Osteomalacia

Although a defect in renal transport of phosphate seems well established as the primary abnormality underlying the pathogenesis of X-linked hypophosphatemic rickets and osteomalacia, several observations indicate that renal phosphate wasting and hypophosphatemia cannot solely account for the spectrum of abnormalities characteristic of this disease. Thus, in the present study, we investigated the potential role of abnormal vitamin D metabolism in the pathogenesis of this disorder and the effect of 1,25-dihydroxyvitamin D(3) therapy on both the biochemical abnormalities characteristic of this disease and the osteomalacia. Four untreated patients, ages 14-30 yr, had normocalcemia (9.22+/-0.06 mg/dl); hypophosphatemia (2.25+/-0.11 mg/dl); a decreased renal tubular maximum for the reabsorption of phosphate per liter of glomerular filtrate (2.12+/-0.09 mg/dl); normal serum immunoreactive parathyroid hormone concentration; negative phosphate balance; and bone biopsy evidence of osteomalacia. The serum 25-hydroxyvitamin D(3) concentration was 33.9+/-7.2 ng/ml and, despite hypophosphatemia, the serum level of 1,25-dihydroxyvitamin D(3) was not increased, but was normal at 30.3+/-2.8 pg/ml. These data suggested that abnormal homeostasis of vitamin D metabolism might be a second defect central to the phenotypic expression of X-linked hypophosphatemic rickets/osteomalacia. This hypothesis was supported by evaluation of the long-term response to pharmacological amounts of 1,25-dihydroxyvitamin D(3) therapy in three subjects. The treatment regimen resulted in elevation of the serum 1,25-dihydroxyvitamin D levels to values in the supraphysiological range. Moreover, the serum phosphate and renal tubular maximum for the reabsorption of phosphate per liter of glomerular filtrate increased towards normal whereas the phosphate balance became markedly positive. Most importantly, however, repeat bone biopsies revealed that therapy had positively affected the osteomalacic component of the disease, resulting in normalization of the mineralization front activity. Indeed, a central role for 1,25-dihydroxyvitamin D(3) in the mineralization of the osteomalacic bone is suggested by the linear relationship between the serum level of this active vitamin D metabolite and the mineralization front activity. We, therefore, suggest that a relative deficiency of 1,25-dihydroxyvitamin D(3) is a factor in the pathogenesis of X-linked hypophosphatemic rickets and osteomalacia and may modulate the phenotypic expression of this disease.

Osteomalacia After Parathyroidectomy in Patients with Uremia

Five patients on maintenance dialysis had symptoms of osteomalacia, proven by biopsy, after parathyroidectomy. In all five patients clinical and radiographic manifestations of secondary hyperparathyroidism were present before surgery, and in two patients preoperative biopsy of bone confirmed the existence of osteitis fibrosa. Like previously described patients with osteomalacia all five had multiple fractures and normal or high serum calcium concentrations that rose to abnormally high values on treatment with vitamin D or dihydrotachysterol. Quantitative histomorphometry of biopsy after parathyroidectomy showed no residual parathyroid hormone effect and nearly complete cessation of mineralization. Four patients had forearm autografts of parathyroid tissue that appeared to be functioning at very low rates according to paired venous sampling, and all five patients had relatively low circulating concentrations of parathyroid hormone. This and earlier experiences reported by others suggest that secondary hyperparathyroidism may have an important facilitative role in the mineralization of bone in uremic patients.

Calcification of Entheses Associated with X-Linked Hypophosphatemic Osteomalacia

We undertook a retrospective analysis of 26 patients with X-linked hypophosphatemic osteomalacia (or rickets), whose ages ranged from 1 to 62 years and who were from 11 different kindreds, to determine the prevalence and clinical characteristics of a unique disorder of the entheses (tendons, ligaments, and joint capsules). We found a generalized involvement of the entheses, with exuberant calcification of tendon and ligament insertions and of joint capsules, in 69 per cent of the subjects. The prevalence and extent of disease increased with age but were not correlated with sex. Commonly affected sites included the hand and sacroiliac joints. Histologic evaluation in a selected patient revealed intratendinous lamellar bone but no inflammatory cells. Our observations indicate that this disorder is an integral part of X-linked hypophosphatemic osteomalacia and exhibits clinical, radiographic, and histologic characteristics that differentiate it from degenerative disorders of these tissues and seronegative spondyloarthropathies.

Healing of bone disease in X-linked hypophosphatemic rickets/osteomalacia. Induction and maintenance with phosphorus and calcitriol.

Although conventional therapy (pharmacologic doses of vitamin D and phosphorus supplementation) is usually successful in healing the rachitic bone lesion in patients with X-linked hypophosphatemic rickets, it does not heal the coexistent osteomalacia. Because serum 1,25-dihydroxyvitamin D levels are inappropriately low in these patients and high calcitriol concentrations may be required to heal the osteomalacia, we chose to treat five affected subjects with high doses of calcitriol (68.2 +/- 10.0 ng/kg total body weight/d) and supplemental phosphorus (1-2 g/d) performing metabolic studies and bone biopsies before and after 5-8 mo of this therapy in each individual. Of these five patients, three (aged 13, 13, and 19 yr) were receiving conventional treatment at the inception of the study and therefore showed base-line serum phosphorus concentrations within the normal range. The remaining two untreated patients (aged 2 and 37 yr) displayed characteristic hypophosphatemia before calcitriol therapy. All five patients demonstrated serum calcitriol levels in the low normal range (22.5 +/- 3.2 pg/ml), impaired renal phosphorus conservation (tubular maximum for the reabsorption of phosphate per deciliter of glomerular filtrate, 2.13 +/- 0.20 mg/dl), and osteomalacia on bone biopsy (relative osteoid volume, 14.4 +/- 1.7%; mean osteoid seam width, 27.7 +/- 3.7 micron; mineral apposition rate, 0.46 +/- 0.12 micron/d). On high doses of calcitriol, serum 1,25-dihydroxyvitamin D levels rose into the supraphysiologic range (74.1 +/- 3.8 pg/ml) with an associated increment in the serum phosphorus concentration (2.82 +/- 0.19 to 3.78 +/- 0.32 mg/dl) and improvement of the renal tubular maximum for phosphate reabsorption (3.17 +/- 0.22 mg/dl). The serum calcium rose in each patient while the immunoactive parathyroid hormone concentration measured by three different assays remained within the normal range. Most importantly, repeat bone biopsies showed that high doses of calcitriol and phosphorus supplements had reversed the mineralization defect in all patients (mineral apposition rate, 0.88 +/- 0.04 micron/d) and consequently reduced parameters of bone osteoid content to normal (relative osteoid volume, 4.1 +/- 0.7%; mean osteoid seam width, 11.0 +/- 1.0 micron). Complications (hypercalcemia and hypercalciuria) ensued in four of these five patients within 1-17 mo of documented bone healing, necessitating reduction of calcitriol doses to a mean of 1.6 +/- 0.2 micrograms/d (28 +/- 4 ng/kg ideal body weight per day). At follow-up bone biopsy, these four subjects continued to manifest normal bone mineralization dynamics (mineral apposition rate, 0.88 +/-0.10 micrometer/d) on reduced doses of 1.25-dihydroxyvitamin D with phosphorus supplements (2 g/d) for a mean of 21.3 +/- 1.3 mo after bone healing was first documented. Static histomorphometric parameters also remained normal (relative osteoid volume, 1.5 +/- 0.4%; mean osteoid seam width, 13.5 +/- 0.8 micrometer). These data indicate that administration of supraphysiologic amounts of calcitriol, in conjunction with oral phosphorus, results in complete healing of vitamin D resistant osteomalacia in patients with X-linked hypophosphatemic rickets. Although complications predictably require calcitriol dose reductions once healing is achieved, continued bone healing can be maintained for up to 1 yr with lower doses of 1,25-dihydroxyvitamin D and continued phosphorus supplementation.

Tumor-Induced Osteomalacia

Tumor-induced osteomalacia is a sporadic condition characterized by defective bone and cartilage mineralization in children and bone mineralization in adults, which resolves after resection of a co-existing tumor. The abnormal calci®cation of cartilage occurs at epiphyseal growth plates and contributes to an associated delayed maturation of the cartilage cellular sequence and disorganization of cell arrangement [1]. The resultant profusion of disorganized, nonmineralized, degenerating cartilage leads to widening of the epiphyseal plates with ̄aring or cupping, irregularity of the epiphysealmetaphyseal junctions, attendant skeletal abnormalities and possibly growth retardation. Abnormal calci®cation of bone is limited to the newly formed organic matrix deposited at the bone-osteoid interfaces of remodeling tissue. This defect results in an increase in the bone forming surface covered by incompletely mineralized osteoid, an enhanced osteoid volume and thickness, a decrease in the mineralizing surface, and likely a heightened susceptibility to fractures and/or bone deformities [2].

Aluminum deposition at the osteoid-bone interface. An epiphenomenon of the osteomalacic state in vitamin D-deficient dogs.

Although aluminum excess is an apparent pathogenetic factor underlying osteomalacia in dialysis-treated patients with chronic renal failure, the mechanism by which aluminum impairs bone mineralization is unclear. However, the observation that aluminum is present at osteoid-bone interfaces in bone biopsies of affected patients suggests that its presence at calcification fronts disturbs the cellular and/or physiochemical processes underlying normal mineralization. Alternatively, aluminum at osteoid-bone interfaces may reflect deposition in preexistent osteomalacic bone without direct effects on the mineralization process. We investigated whether aluminum accumulates preferentially in osteomalacic bone and, if so, whether deposition of aluminum occurs at calcification fronts and specifically inhibits mineralization. Aluminum chloride (1 mg/kg) was administered intravenously three times per week for 3 wk to five normal and five vitamin D-deficient osteomalacic dogs. Before administration of aluminum the vitamin D-deficient dogs had biochemical and bone biopsy evidence of osteomalacia. Bone aluminum content in the osteomalacic dogs (15.1 +/- 2.2 micrograms/g) and the plasma aluminum concentration (10.4 +/- 2.1 micrograms/liter) were no different than those of normal dogs (10.5 +/- 3.5 micrograms/g and 11.9 +/- 1.2 microgram/liter, respectively). After the 3 wk of aluminum administration the plasma phosphorus, parathyroid hormone, and 25-hydroxyvitamin D concentrations were unchanged in normal and vitamin D-deficient dogs. Similarly, no alteration in bone histology occurred in either group. In contrast, bone aluminum content increased to a greater extent in the vitamin D-deficient dogs (390.3 +/- 24.3 micrograms/g) than in the normal dogs (73.6 +/- 10.6 micrograms/g). Moreover, aluminum localized at the osteoid-bone interfaces of the osteomalacic bone in the vitamin D-deficient dogs, covering 42.9 +/- 9.2% of the osteoid-bone surface. Further, in spite of continued aluminum chloride administration (1 mg/kg two times per week), vitamin D repletion of the vitamin D-deficient dogs for 11 wk resulted in normalization of their biochemistries. In addition, while normal dogs maintained normal bone histology during the period of continued aluminum administration, vitamin D repletion of the vitamin D-deficient dogs induced healing of their bones. Indeed, the appearance of aluminum in the cement lines of the healed bones indicated that mineralization had occurred at sites of prior aluminum deposition. These observations illustrate that aluminum deposition in osteomalacic bone may be a secondary event that does not influence bone mineralization. Thus, although aluminum may cause osteomalacia in chronic renal failure, its presence at mineralization fronts may not be the mechanism underlying this derangement.

X-Linked hypophosphatemic rickets: a disease often unknown to affected patients

X-Linked hypophosphatemic rickets (XLH) is an X-linked dominant disorder that is secondary to renal phosphate wasting. Affected individuals frequently present the following characteristics: short stature, lower-extremity deformity, bone pain, dental abscesses, enthesopathy, rickets, and osteomalacia. Since the disorder is characterized by evident phenotypic abnormalities, we hypothesized that there would be a high degree of knowledge about the disease in affected kindreds. Thus, we constructed a six-page, self-administered questionnaire to determine whether family members are, in fact, aware of their disease and properly diagnosed and treated. We also designed the survey to determine rates of symptoms thought to be associated with rickets/osteomalacia in a population with a lower referral bias than is usually seen in tertiary care centers. We administered the questionnaire to 234 study subjects (57 affected) who were members of one of three large kindreds. Although 62% of affected individuals knew they had some problem with their bones, only 22.6% were told by a physician that they had rickets or osteomalacia. This apparent lack of awareness occurred in spite of 61.1% of affected subjects complaining of bone or joint problems to their personal physician. Indeed, of those patients who had persistent complaints, only 34.5% were told they had rickets or osteomalacia. Only one patient was taking phosphate and vitamin D.(ABSTRACT TRUNCATED AT 250 WORDS)

Newer knowledge of vitamin D and its metabolites in health and disease.

Renewed interest in vitamin D, over the past several years, has resulted in increased knowledge of (1) the metabolic pathways which result in production of an active metabolite, (2) the role of its various metabolities at target tissues, and (3) its interaction with other control systems in the maintenance of calcium/phosphorus homeostasis. Presently, a role for 1, 25-(OH)2 D3 can be identified in the regulation of (1) calcium and phosphorus absorption from the intestine, (2) PTH production, and (3) calcium mobilization from bone (in conjunction with PTH). Several other actions at the kidney, muscle and other organs have been suggested but not proven. In contrast, the actual process of bone mineralization may be dependent, in part, on 25-(OH) D3. Despite these major advances in our knowledge, many gaps remain and controversial data continues unresolved. However, application of this new information to analysis of a wide variety of disease states has resulted in remarkable progress in appreciation of the pathogenesis and appropriate treatment for these diseases. Nonetheless, continued research promises further advances and more precise definition of disease states as well as delineation of the therapeutic role of Vitamin D metabolites in their treatment.