Osteophyte Formation in the Lumber Spine and Relevance to Low Back Pain

Abstract

Vertebral osteophyte formation is a well-documented phenomenon that is associated with degeneration and altered mechanics of the spine, both of which have been considered to be the result of aging, a purely physiologic response to load bearing, or intrinsic spinal disease as etiologic factors. (Lane et al., 1993, O’Neill et al., 1999) They are recognized radiologically as hyperostosis at the region of the attachment of the annular fibers to the vertebral body and localized increases in bone mineral density. (Nathan et al., 1994) As the etiologic factors, the compressive forces on the vertebral endplates (Nathan et al., 1962), bone mineral density (Kinoshita et al., 1998), obesity (O’Neill et al., 1999) and genetic factors (Sambrook et al., 1999) have been reported as causes, although the absence of a single definitive factor causing spinal degeneration has led to a suggestion that several factors including both genetic and nongenetic ones contribute to the development of osteophyte formation. (Harada et al., 1998, Liu et al., 1997)