ALTERATIONS IN THE LIPIDS OF BONE CAUSED BY HYPERVITAMINOSIS A AND D

1. The total lipid, phospholipid, total and free fatty acid, free and esterified cholesterol contents of the long bones of normal, hypervitaminotic A, D and A plus D rats were determined. 2. Toxic amounts of vitamin A decreased the total fatty content, whereas toxic amounts of vitamin D increased triglycerides, esterified cholesterol and in particular the phospholipids of bone. 3. An interaction occurred between toxic amounts of vitamins A and D, which prevented, to a large extent, the alterations in bone lipids that occur in hypervitaminosis D. 4. The studies suggest an involvement of vitamin D in lipid metabolism and tend to support the idea that lipids are involved in ossification.

FLUORIDE: ITS EFFECTS ON 2 PARAMETERS OF BONE GROWTH IN ORGAN CULTURE

Bones of the forepaws of young rats were subjected to varying concentrations of fluoride ions in organ culture. The formation of DNA and protein synthesis were evaluated by measurements of the uptake of tritiated thymidine and C(14)-labeled proline. Fluoride concentrations as high as 10 to 20 parts per million had no demonstrable effect in vitro on these basic parameters of skeletal growth

THE PROBLEM OF DEMINERALISATION IN THIN SECTIONS OF FULLY CALCIFIED BONE

Thin sections of embryonic avian bone decalcify during preparation for electron microscopy, creating a false impression of mineral distribution. The results of the experiments reported herein show that viscous embedding materials do not penetrate compact formed bone, and so, in thin sections, the calcium apatite crystals may be leeched out by water, both in the collecting trough and in aqueous solutions of stains used to enhance tissue electron opacity. To prevent decalcification, a simple technique is described in which the aqueous fluids that come in contact with thin sections are saturated with respect to calcium and phosphate ions, thereby preventing solution of the bone mineral. The theoretical basis of this technique is briefly discussed.

MEASUREMENT OF BONE MINERAL IN VIVO: AN IMPROVED METHOD

The mineral content of bone can be determined by measuring the absorption by bone of a monochromatic, low-energy photon beam which originates in a radioactive source (iodine-125 at 27.3 kev or americium 241 at 59.6 kev). The intensity of the beam transmitted by the bone is measured by counting with a scintillation detector. Since the photon source and detector are well collimated, errors resulting from scattered radiation are reduced. From measurements of the intensity of the transmitted beam, made at intervals across the bone, the total mineral content of the bone can be determined. The results are accurate and reproducible to within about 3 percent.