STUDIES ON BONE MATRIX IN NORMAL AND OSTEOPOROTIC BONE

Fossil proteins in vertebrate calcified tissues

Selected fossil vertebrates and the enclosing sediments dating from 1300 years B.C. to approximately 400 million years ago were subjected to amino acid assay. The amino acid analyses revealed little evidence of intact collagen in fossils of Tertiary, Mesozoic or Palaeozoic age. There was, however, evidence of contemporary proteinaceous material which may have been derived from bacteria. In Palaeozoic material the analyses detected a general background of amino acids common to both fossils and sediments. The degree of racemization was routinely determined as a means of measuring modern contamination of geologically older samples. An electron microscope study of Quaternary (Pleistocene) collagen revealed a significant reduction of the 64 nm banding to about 50 nm. The same Pleistocene material gave amino acid compositional profiles typical of collagen. However, when this material was subjected to digestion by the proteolytic enzymes collagenase, pronase and subtilisin, the resulting peptide fingerprints showed small but significant differences from those obtained from modern collagen digests, indicating the possibility of changes having occurred during fossilization affecting susceptible cleavage sites in the molecule.

Modified tetrachrome method for osteoid and defectively mineralized bone in paraffin sections

A new modification of the tetrachrome method for bone osteoid in paraffin sections has been designed. The modified tetrachrome method suitable for routine use in any histology laboratory retains the simplicity of the original method and gives good results on the freshly fixed, decalcified, paraffin embedded material. Osteoid tissue is stained deep blue and normally mineralized bone is stained red. Defectively mineralized bone stains pale blue or pink and the cellular population is clearly identifiable. The ability to distinguish the osteoid tissue from mineralized bone and connective tissue and cartilage makes diagnosis of osteomalacia or osteoid producing tumors or assessment of ossification process straightforward, without the need for undecalcified sections. By displaying simultaneously irregularities in the mineralized matrix and morphology of bone cells, the method also permits the diagnosis of conditions recently described in patients with osteoporotic fractures, such as osteocytic degeneration and bone tissue defects.

The role of calcium in the mechanical behaviour of bone

Plugs of fresh post mortem human patellar subchondral bone were soaked for three weeks in an organic solvent (ethanol) which contained a chelating agent (EDTA). This technique selectively removes the calcified inorganic component without disrupting the structure of the remaining bone matrix. These plugs, together with untreated plugs as controls, were treated in unconfined compression at a fixed strain rate and allowed to relax to evaluate the contribution made by the calcium component to the physical and time-dependent properties of subchondral bone.