Bone cell calcium stores: their size, location and kinetics of exchange

The ultrastructure of slam-frozen bone mineral

Bone salt may be altered by preparative procedures. 'Slam' freezing can usefully be applied to bone mineral because it minimizes preparation and preserves the tissue chemistry. The structure and composition of the mineral in 'slam'-frozen neonatal mouse calvaria (which require neither previous slicing nor manipulation) was examined by transmission electron microscopy and X-ray microanalysis in unstained sections, 0.25 micron thick (i.e. unusually thick). Comparison was made with fresh intact calvaria and with 'snap'-frozen histological sections of mature rat femora. Under the optical microscope, calcified microspheres, up to 1 micron in diameter, were evident within 'young' osteocytes and within the extracellular matrix of both immature and mature, unstained and von Kossa-stained bone. In the electron microscope, microspheres of similar dimension and distribution were observed after 'slam' freezing and were divided into two groups. One group, found inside and outside cells, had a substructure of closely packed, electron-dense, rounded bodies 30-40 nm in diameter; despite their unusual stability in EDTA, X-ray microanalysis indicated high levels of both calcium and phosphorus. The other group was found at the calcification front and, although similar to the first group in size and chemical composition, these microspheres had a substructure of clusters of 5-nm-thick electron-dense filaments containing mineral that was characteristically EDTA labile. The 30- to 40-nm dense bodies did not appear to be mitochondrial and were absent from customary fixed and resin-embedded, ultrathin, stained preparations. They were not observed singly and their aggregation into arrangements of microspheres, sometimes linked by bridges, may be an important preliminary step in the development of the filamentous clusters. Needle-shaped and plate-like crystals of bone mineral were absent. It was concluded that 'slam' freezing preserves both intracellular and extracellular bone salt in the form of microspheres within which the mineral may modulate from dense bodies into filamentous arrays of variable density with maturity.

Significance of early increase in stable and radioactive plasma calcium after parathyroidectomy in primary hyperparathyroidism

Early effects of parathyroid hormone (PTH) deficiency were studied in 12 patients with primary hyperparathyroidism due to single parathyroid adenoma by following the precise time course of changes in plasma calcium (Ca) and immunoreactive parathyroid hormone (IPTH) after parathyroid surgery and by prelabeling 2 patients with radiocalcium (Ca*). Surgical removal of the adenoma was immediately followed by a sudden increase in plasma Ca which preceded the usual fall. The increase in plasma Ca commenced simultaneously with the fall in iPTH and was accompanied by a parallel increase in specific activity (sp. act.) of plasma Ca*. Specific activity continued to rise for 2 h in both prelabeled patients, whereas blood calcium was already falling thereafter reaching a markedly low removal rate constant as long as plasma Ca decreased. When plasma Ca began to rise, sp. act. resumed a descending course. Our findings indicate that the initial hypercalemia depends on PTH withdrawal and results from a rapid flux into general extracellular fluid (ECF) of calcium coming from a compartment with higher sp. act., contained within the miscible pool, immediately followed by a reduction in calcium transfer from bone. These results suggest that acute PTH deficiency determines an outflow of calcium from bone cells and support the theory that PTH initiates its action by modifying their intracellular calcium content.

The actions of parathyroid hormone on bone: relation to bone remodeling and turnover, calcium homeostasis, and metabolic bone disease. Part I of IV parts: mechanisms of calcium transfer between blood and bone and their cellular basis: morphological and kinetic approaches to bone turnover

The supracellular organization of living bone enables the study of isolated cellular and subcellular systems to be related to the study of the whole organism. Bone is formed by osteoblasts in successive stages, separated in both time and space, of matrix formation and primary mineralization. Osteoblasts are joined by tight junctions and largely cover the osteoid seam which separates them from mineralized bone. Secondary mineralization is not completed for several months and is not regulated by the osteoblast. Bone is resorbed by osteoclasts which simultaneously accomplish mineral dissolution and matrix digestion. Active osteoblasts occupy about 5% of the free bone surface, osteoid seams with less active osteoblasts about 10%, active osteoclasts about 0.5%, and Howship's lacunae at which bone remodeling is either quiescent or arrested about 5%. The remaining 80% of the free bone surface is covered by a leaky envelope of thin flattened cells, termed surface osteocytes. Some osteoblasts become permanently buried in the bone as deep osteocytes, around which a specialized and metabolically active perilacunar bone is formed. This bone is less highly mineralized and can temporarily lose or gain calcium in accordance with homeostatic needs. Deep osteocytes maintain contact with each other and with the surface osteocytes, their cell processes within canaliculi being joined by gap junctions. Remodeling of cortical bone proceeds with the excavation by osteoclasts of a longitudinal tunnel which is refilled by osteoblasts to form a new osteon. The anatomically discrete longitudinally oriented structure consisting of a cutting cone of osteoclasts in front and a closing cone of osteoblasts behind is termed a cortical remodeling unit. The events of centrifugal resorption and centripetal formation which occur in a single cross section is termed a cortical remodeling cycle. Normally each new cycle is slightly out of phase with its predecessor. The quantities which characterize cortical remodeling are the birth rate of new remodeling cycles or activation frequency (mu), and the durations of the resorptive period (sigma r), the quiescent interval (sigma q) and the formation period (sigma f). The average distances traveled by the osteoclast and osteoblast are indicated respectively by the mean cement line diameter and mean wall thickness of completed osteons. These quantities show little interindividual variation. Because of this constancy the magnitude of bone turnover (the bone formation rate) is almost entirely a function of mu, the activation frequency of new remodeling cycles. Variations in the velocity of advance of osteoclasts (the linear resorption rate) or of osteoblasts (the appositional rate) alter inversely both the extent of surface engaged in resorption or formation and the time taken to replace a particular moiety of bone, but in a steady state do not influence the rate of turnover of the skeleton as a whole...

Mitochondrial granules in human osteoblasts with a reference to one case of osteogenesis imperfecta

Electron-dense granules in mitochondria from prenatal human osteoblasts, postnatal human osteoblasts, and from osteoblasts derived from a child with osteogenesis imperfecta congenita are described. The mitochondrial granules were of about 600 A in diameter and were attached to the mitochondrial cristae. Sections of mitochondria from prenatal osteoblasts showed an average number of 10 granuales per mitochondrial section, whereas sections of mitochondria of postnatal osteoblasts showed only occasionally 1-2 granules per mitochondrial section. Mitochondria from osteoblasts derived from the child with an untreated osteogenesis imperfecta congenita showed an average number of 10 granules per mitochondrial section.