Abstract

ABSTRACTHistorically, rickets and osteomalacia have been synonymous with vitamin D deficiency dating back to the 17th century. The term osteomalacia, which literally means soft bone, was traditionally applied to characteristic radiologically or histologically documented skeletal disease and not just to clinical or biochemical abnormalities. Osteomalacia results from impaired mineralization of bone that can manifest in several types, which differ from one another by the relationships of osteoid (ie, unmineralized bone matrix) thickness both with osteoid surface and mineral apposition rate. Osteomalacia related to vitamin D deficiency evolves in three stages. The initial stage is characterized by normal serum levels of calcium and phosphate and elevated alkaline phosphatase, PTH, and 1,25‐dihydroxyvitamin D [1,25(OH)2D]—the latter a consequence of increased PTH. In the second stage, serum calcium and often phosphate levels usually decline, and both serum PTH and alkaline phosphatase values increase further. However, serum 1,25(OH)2D returns to normal or low values depending on the concentration of its substrate, 25‐hydroxyvitamin D (25OHD; the best available index of vitamin D nutrition) and the degree of PTH elevation. In the final stage, hypocalcemia and hypophosphatemia are invariably low with further exacerbation of secondary hyperparathyroidism. The exact,or even an approximate, prevalence of osteomalacia caused by vitamin D deficiency is difficult to estimate, most likely it is underrecognized or misdiagnosed as osteoporosis. Signs and symptoms include diffuse bone, muscle weakness, and characteristic fracture pattern, often referred to as pseudofractures, involving ribs, scapulae, pubic rami, proximal femurs, and codfish‐type vertebrae. The goal of therapy of vitamin D‐deficiency osteomalacia is to alleviate symptoms, promote fracture healing, restore bone strength, and improve quality of life while correcting biochemical abnormalities. There is a need for better understanding of the epidemiology of osteomalacia. Simplified tools validated by concurrent bone histology should be developed to help clinicians promptly diagnose osteomalacia. © 2020 The Authors. JBMR Plus published by Wiley Periodicals LLC. on behalf of American Society for Bone and Mineral Research.

Highlights

  • Rickets and osteomalacia have been synonymous with vitamin D deficiency dating back to the 17th century

  • From a biochemical point of view, osteomalacia caused by vitamin D deficiency evolves in three stages: an initial stage characterized by normal serum levels of calcium and phosphate and elevated levels of alkaline phosphatase, serum PTH, and 1,25-dihydroxyvitamin D [1,25(OH)2D]—the latter as a consequence of increased PTH

  • We exclusively address the osteomalacia that is directly related to vitamin D deficiency. (Other aspects of vitamin D are discussed in related articles in this special issue.)

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Summary

Introduction

Rickets and osteomalacia have been synonymous with vitamin D deficiency dating back to the 17th century. From a biochemical point of view, osteomalacia caused by vitamin D deficiency evolves in three stages: an initial stage characterized by normal serum levels of calcium and phosphate and elevated levels of alkaline phosphatase, serum PTH, and 1,25-dihydroxyvitamin D [1,25(OH)2D]—the latter as a consequence of increased PTH At this stage, bone histomorphometry reveals only the effects of excess PTH without a mineralization defect. It is a common finding to observe, at the beginning, an increase of serum alkaline phosphatase that gradually decreases; in patients with prolonged vitamin D deficiency, secondary hyperparathyroidism may persist for a long time, and in rare cases it may progress to hypercalcemic tertiary hyperparathyroidism. Treatment with vitamin D in the setting of renal failure should take into account the degree of suppression of PTH secretion, which may increase the risk of adynamic bone disease

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25. Kidney Disease
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