Carbonic anhydrase was localized in osteoclasts by light and electron microscopy using a preembedding peroxidase-antiperoxidase staining method. Osteoclasts on the endosteal surface of the metatarsi of calcitonin-treated and untreated (control) chicks were studied. A positive staining reaction was seen in the cytosol, in the Golgi apparatus, in and on vesicles, on the plasma membrane of the ruffled border, and on the bone surface beneath control osteoclasts. After calcitonin treatment, positive staining reactions were seen at the same sites except that staining was absent on the plasma membrane and endosteal bone surface. The morphology of osteoclasts from calcitonin-treated chicks was indicative of cell inactivity. The carbonic anhydrase which was bound to the plasma membrane of the ruffled border is appropriately arrayed for hydrogen ion secretion and subsequent mineral dissolution. The presence of the enzyme within lysosomelike vesicles and on the endosteal surface beneath active cells suggests that it may be released into the resorbing zone along with the lysosomal hydrolases. The function of the extracellular enzyme is also unknown.
Quantitative electron probe analysis was performed on chick epiphyseal growth cartilage prepared by two anhydrous methods, ultrathin cryosections and freeze-dried epoxy-embedded tissue. Levels of Na, Mg, P, S, Cl, K, and Ca were determined in cytoplasm, mitochondria, extracellular matrix, matrix vesicles, and mineral nodules in four zones of the cartilage--proliferative, prehypertrophic, early hypertrophic, and early calcification. The exceptionally high levels of Na and K (up to 550 and 200 mmol/kg wet wt, respectively) found in the matrix are believed to be largely bound to fixed anions. Within cells, Na was higher than K (140 versus 20-34 mmol/kg wet wt), a condition that may reflect hypoxia. Ca and P were low in cells and unmineralized matrix. Ca and P were high in mitochondrial granules of the early hypertrophic zone and diminished in amount in the calcifying zone; the converse occurred in matrix vesicles. Mg was low to undetectable except in heavily mineralized structures (i.e., mitochondrial granules, matrix vesicles, and mineral nodules). S levels were high in matrix (approximately 400 mmol/kg wet wt) and increased slightly with maturation. The amount of S present greatly exceeds Ca levels and implies that sulfate, the predominant form of sulfur in proteoglycans, may serve as an ion-exchange mechanism for the passage of Ca through the matrix to sites where Ca and phosphate are precipitated.
The endosteal reaction, the initial step in the formation of medullary bone, was investigated in femurs of estrogen-treated male Japanese quail. Morphologically, the endosteal cells were in an undifferentiated state until 30 h after estrogen treatment and showed characteristics resembling those of resting cells. Many preosteoblasts were seen on the endosteum at 33 h, whereas mitotic figures and fully differentiated osteoblasts were recognized at 36 h after estrogen. The mitotic figures were observed among the preosteoblasts on the endosteum. Autoradiographs showed that the number of endosteal cells labeled by [3H]thymidine injected 1 h before sacrifice was maximal 27 h after the estrogen administration and decreased markedly by 30 h. When a single injection of [3H]thymidine was given at 26 h after estrogen, the highest percent of labeled endosteal cells was observed 1 h later (27 h after estrogen). Labeled preosteoblasts and osteoblasts were observed at 7 h (33 h after estrogen) and 10 h (36 h after estrogen), respectively. Our results show that under the influence of estrogen, endosteal cells are induced to maximally synthesize DNA about 27 h after estrogen. These cells appear to modulate into preosteoblasts in about 6 h and then divide via mitosis to become osteoblasts within an additional 3 h. The development of medullary bone induced by estrogen occurs in a sequential and predictable manner, which makes it a useful system for studying basic problems on bone cell differentiation.
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