Appearance of electron-dense segments: indication of possible conformational changes of pre-mineralizing collagen fibrils in the osteoid of rat bones

To elucidate precise mechanisms of appositional mineralization of bone, structural features of mineralizing collagen fibrils of the osteoid in normal and hypocalcaemic rats were examined in detail by transmission electron microscopy. Ultrathin sections of the osteoid of various types of bones of the rats fed with regular or normal calcium diet often displayed electrondense segments in the specific regions of the collagen fibrils located immediately adjacent to the mineralization front or to the mineralization nodules. Such dense segments appeared only after Ur-Pb staining and were more distinct in undecalcified specimens. Dense segments were undetectable in ultrathin sections picked up on ethylene glycol instead of water in the trough, even after Ur-Pb staining. Collagen fibrils in the widened osteoid of hypocalcaemic rats fed with calcium-free diet failed to show electron-dense segments. A careful comparison between the hydrously or anhydrously processed adjacent sections of a normal rat bone indicated a drastic dissolution of electron-dense material from the bone matrix near the mineralization front in hydrously processed sections and, thus, implicated the presence of labile mineral–matrix complexes in the recently mineralized bone matrix. Such labile sediments were readily dissociated within the ultrathin sections while the sections were floating on water and immediately adsorbed onto the pre-mineralizing collagen fibrils, where some conformational changes might have occurred. These data indicate that highly electron-dense segments appearing in the osteoidal collagen fibrils are a type of process-induced product, which indirectly represent possible structural alterations in the segmental portions of pre-mineralizing collagen fibrils in the osteoid of rat bones.