Tibiae of young rats were examined by scanning electron microscopy (SEM) and transmission electron microscopy (TEM) in order to study the origin and structure of matrix vesicles in periosteal bone. SEM studies have shown that periosteal osteoblasts have elongated processes with globular structures of 0.1 µm in diameter attached to the cell surface and processes. Similar structures were found to cover the inner surface of osteoblastic lacunae. The SEM studies have further shown that in the periosteal surface (forming bone) the above-described globules once mineralized, aggregated to form larger, nonhomogeneous mineralized spherules in which, by proper treatment with NaOCl, hydroxyapatite crystals could be exposed. Endosteal osteoblasts had fewer processes, devoid of the globular structures. Similarly, osteocytic and osteoclastic processes, although elongated and numerous, were not covered by the globular structures. In the matrix, collagen fibers of forming bone were randomly orientated, while in the deeper areas of bone they formed bundles with a longitudinal orientation. TEM studies have shown that the structures found on the osteoblastic surface and in the matrix are membrane-bound matrix vesicles which seem to be formed by budding from cell processes.Preformed membrane-bound vesicles were also observed by TEM inside sections of osteoblastic processes. These vesicles resembled the extracellular matrix vesicles in size and shape, thus giving the impression that at least some of the matrix vesicles are preformed cellular structures. While comparing SEM with TEM, it can be concluded that in bone, as in cartilage, matrix vesicles which probably serve as the initial locus of calcification, are formed directly by osteoblasts.

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III rages. This approach will recommend itself to the senior medical student, pre-registration houseman, general practitioner and general physician, whose needs are practical; but those specially interested in the brain sciences may find it too simple, and will want to use it merely as an introduction to the subject. For this reason, a more comprehensive suggested reading list would have been valuable.

In an attempt to further define the nature of the active metabolite in bone formation, a series of experiments were conducted whereby vitamin D metabolites were administered locally in vivo into the proximal epiphyseal growth plate of the tibiae of rachitic chicks. Local administration of 3 micrograms of 24,25(OH)2D3 in vivo to D-deficient chicks resulted in disappearance of the rachitic lesions in the same leg. Administration of 1 microgram 1,25(OH)2D3 in a similar manner failed to show any sign of healing. Injection of 5 micrograms 25(OH)D3 was followed by recovery from rickets in both the injected right leg and in the vehicle-injected left tibia, although the recovery was more pronounced in the injected leg. Lower doses of 0.3 or 1 microgram 24,25(OH)2D3 failed to reverse the rachitic lesions and induced only minimal recovery. These findings suggest that 24,25(OH)2D3 at the higher doses has a direct local effect on cartilage and bone, while 1,25(OH)2D3 has no such effect in chicks. 25(OH)D3 is probably absorbed from the epiphyses into the blood stream and converted into the active metabolites, which were indeed detected in the blood to exert its systemic effects.