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The lethal, autosomal recessive osteopetrotic mutation in the rabbit, osteosclerosis (os/os), has recently been made available for experimental investigation. We have examined the cytology and ultrastructure of skeletal cells in mutants and report abnormalities in osteoblasts, osteocytes, and osteoclasts. Mutant osteoclasts lack a well-defined ruffled border and show few morphological signs of bone resorption. Osteoblasts in mutants form bone in neonatal life but show signs of degeneration by 2 weeks after birth. Mutant osteoblasts and osteocytes contain large, electron-dense cytoplasmic inclusions. External surfaces of mutant long bones show no evidence of bone resorption by scanning electron microscopy, and fibrosis of intertrabecular spaces is a prominent feature in mutants. These data, considered with recent evidence that the functions of osteoblasts and osteoclasts are interrelated, suggest that reduced bone resorption, a characteristic feature of osteopetrosis, may be related to osteoblast incompetence in this mutation.

The toothless (tl) rat is a nonlethal osteopetrotic mutation characterized by the presence of few osteoclasts and the failure to be cured by bone-marrow transplantation. We examined the skeletal biology of tl rats and normal littermates up to 6 weeks after birth. Osteoclasts in tl rats were small, reduced 25-fold in number, and had greatly reduced concentrations of acid hydrolases. Bone shape internally and externally reflected reduced bone resorption, and tl rats were hypophosphatemic and mildly hypocalcemic at 2 weeks. These data indicate that the basic defect in tl rats is one of differentiation of osteoclasts and, coupled with the observation that normal bone-marrow cells cannot develop into osteoclasts in the tl skeleton, suggest that the defect lies in the skeletal micro-environment.

Osteopetrosis, a metabolic bone disease characterized by a generalized sclerosis of the skeleton, is inherited as an autosomal recessive in a number of mammalian species. The pathogenesis of congenital osteopetrosis is mediated by a reduction in bone resorption as a result of decreased osteoclast function. This hypothesis is based on both functional and structural evidence of reduced bone resorption in all mutations examined to date. The present study examined the histology of cartilage and bone, the ultrastructure of osteoclasts, and the morphology of mineralized bone surfaces in a lethal osteopetrotic mutation, the osteosclerotic (oc) mouse. Histologically, epiphyseal cartilage growth plates, especially the hypertrophic zone, are markedly thickened in oc mice and metaphyses contain excessive osteoid, features characteristic of rickets. Transmission electron microscopy revealed that less than one-quarter of osteoclasts in oc mice demonstrated evidence of ruffled border formation compared with three-quarters of the osteoclasts in normal littermates. In mutants, ruffled borders were less elaborate and cytoplasmic processes penetrated into bone surfaces, suggesting that bone may be removed by mechanical rather than by enzymatic means. There was little morphological evidence of cartilage degradation and broad laminae limitantes persisted in mutants. Mineralized surfaces that undergo resorption in normal mice showed no evidence of bone resorption by scanning EM in mutants. The presence of a rachitic condition, the observations of reduced bone resorption, and the possible contribution of undermineralized matrices to decreased bone resorption are characteristics of the osteosclerotic mutation which suggest that it is a unique osteopetrotic mutant in which to study both the development and regulation of skeletal metabolism.