Abstract
Introduction: The aetiology of dystrophic disc calcification in adult humans is unknown but a well-described clinical disorder with hydroxyapatite as the single mineral phase. Comparable but age-related pathology in the sheep could serve as a model for the human disorder. The objective of this study was to investigate the mineral phase, its mechanisms of formation/association with degeneration in a naturally-occurring animal model of disc calcification.
Methods: Adult sheep lumbar intervertebral discs (n=134) from animals aged 6 (n=4), 8 (n=12) and 11 years (n=2) were evaluated using radiography, morphology, scanning and transmission electron microscopy, energy dispersive X-ray spectroscopy, X-ray powder diffraction, histology, immunohistology and proteoglycan analysis.
Results: Half of the 6 yr, 84% of the 8 yr and 86% of the 11 yr old discs had calcific deposits. These were not well delineated by plain radiography. They were either:
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punctate deposits in the outer annulus,
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diffuse deposits in the transitional zone or inner annulus fibrosus with occasional deposits in the nucleus, or
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large deposits in the transitional zone extending variably into the nucleus.
Their maximal incidence was in the lower lumbar discs (L4/5-L6/7) with no calcification seen in the lumbosacral or lower thoracic discs. All deposits were hydroxyapatite with large crystallite sizes (800–1300 angstrom) compared to cortical bone (300–600 angstrom). No type X-collagen, osteopontin or osteonectin, were detected in calcific deposits although positive staining for bone sialoprotein was evident. Calcified discs had less proteoglycan of smaller hydrodynamic size than non-calcified discs.
Discussion: Disc calcification in ageing sheep is due to hydroxyapatite deposition. The variable but large crystal size, lack of protein markers indicate that this does not occur by an ordered endochondral ossification-like process. The decrease in disc proteoglycan content and size suggests an association between calcification and disc degeneration in ageing sheep. There are notable dissimilarities between hydroxyapatite deposition disorder in humans and sheep. No mechanistic explanation can be offered for the different spinal distributions, thoracic and upper lumbar in the former and lumbar in the latter; hydroxyapatite deposition disorder has occasionally been seen in the lumbar spines of four year old sheep during the course of other studies but not at an earlier age. Diffferences in spinal biomechanics may be implicated but hydroxyapatite deposition does not primarily affect the most or least mobile discs in either species. Neither can an explanation be offered for the apparent immunity of the ovine lumbosacral disc to calcification. However, it is known that proteoglycan turnover is faster at this spinal level than at more proximal lumbar discs. While we have been unable to elucidate the mechanism of hydroxyapatite deposition disorder in sheep, clearly it is different from that in normal osteogenesis. We contend this animal provides a useful, naturally-occurring model for investigation of the aetiology and pathogenesis of human hydroxyapatite deposition disorder, notwithstanding obvious differences between sheep and man.
Correspondence should be addressed to Dr Owen Williamson, Editorial Secretary, Spine Society of Australia, 25 Erin Street, Richmond, Victoria 3121, Australia.
