Bone loss without the loss of bone mineral material? A new perspective on anorexia nervosa

Since the advent on non-invasive in vivo clinical bone densitometry, investigators have reported that regional bone mineral material loss accompanies the onset and continuance of anorexia nervosa (AN). Initial single-energy photon absorptiometric (SPA) studies were followed by a succession of dual-energy X-ray absorptiometric (DXA) investigations, and a few single-energy quantitative computer assisted tomographic (SEQCT) bone densitometry vertebral measurements. Although most all DXA studies found a relatively small diminution (∼ 3%) of bone mineral material at lumbar vertebral and proximal femoral bone-sites of AN-afflicted adolescent girls and young women, these findings have been consensually interpreted and near-universally accepted as losses of actual bone mineral material accompanying AN. It has also been claimed by some that about 50% of those beset by AN while still young adolescents were osteoporotic. Nonetheless, over the last intervening 2 decades of these studies, no specific underlying direct bone-biological causal link between AN and trabecular bone material loss has yet been uncovered. The present exposition shows that in vivo SPA, DXA, and SEQCT measurements of bone mineral material losses do not constitute evidence of actual loss of bone material, and that the attribution of osteopenia and osteoporosis to AN-afflicted younger adolescent girls is not sustainable. Rather, the full gamut of these reported bone material “losses” can be accounted for by the already well-documented AN-induced changes in the anthropometrics and compositional mixes of extra-osseous soft tissues (primarily in a very noticeable reduction of extra-skeletal fat) and intra-osseous bone marrow yellowing (marrow hypoplasia and marrow cell necrosis). These changes in soft tissue compositions and anthropometrics alone have been shown to be sufficient to cause in vivo SPA, DXA, and SEQCT to systematically mis-estimate true bone material density and erroneously register changes in bone mineral content, even when no actual changes in bone mineral material have occurred. As a result, it is seen that in vivo bone densitometry methodologies have not demonstrated that AN induces actual loss of bone mineral material. It is also demonstrated that DXA and SEQCT bone density measurements of predominantly trabecular bone-sites cannot be relied upon as gauges of heightened propensity for early (or late) osteoporotic development.