Abstract

A model of the healing phase of low phosphate, vitamin D deficiency was used to investigate the initial stages of mineralization. The matrix vesicle distribution between the zones of the growth plate was found to be bimodal with high volume densities in the resting and hypertrophic zones and low volume densities in the proliferative and calcifying zones. Healing of the rachitic lesion was associated with a decrease in matrix vesicle volume density in the calcifying zone, compared with the lower hypertrophic zone in florid rickets. The volume density differences were due to differences in the number of vesicles, as the variation in mean caliper diameter was rather small. The findings are compatible with the dynamic cell debris theory for matrix vesicle origin and distribution presented earlier, which favours the view that a major part of matrix vesicles are formed from cell debris. A role of matrix vesicles in the mineralization process is indicated by the finding of an association between mineralization and matrix vesicle degradation.

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