Confocal imaging and timing of secretion of matrix proteins by osteoblasts derived from avian long bone

Primary osteoblasts derived from avian long bone have been evaluated in terms of spatial and temporal expression of known osteoblastic marker proteins during the early phases of cell culture. Confocal imaging of matrix proteins revealed that osteocalcin, bone sialoprotein, osteopontin, and osteonectin were restricted to the cell interior at day 4 of culture; secretion and deposition into the extra-cellular matrix of bone sialoprotein and osteopontin was evident at 8 and 12 days of culture. Osteocalcin and osteonectin were not deposited in the matrix within the timeframe of the study. Total collagen levels produced and alkaline phosphatase activity were substantial by day 4 of culture, and increased from that point 4.0- and 5.5-fold, respectively, by culture day 12. The expression of type I collagen, PTHrP receptor, osteopontin, bone sialoprotein and osteocalcin was followed by Northern blot analysis. Type I collagen and osteopontin mRNA were expressed at constant levels throughout the culture period. Over the 12 days of culture both PTH/PTHrP receptor and bone sialoprotein mRNA expression were found to increase by 2.3- and 2.5-fold, respectively. In contrast, the expression of osteocalcin message decreased by 2.5-fold by day 8 of culture.

Carbonic anhydrase activity in a calcium-mobilizing epithelium of the crustacean Orchestia cavimana during molting

We investigated the involvement of the enzyme, carbonic anhydrase, in the calcification-decalcification processes occurring in the posterior caeca of the midgut of the terrestrial crustacean, Orchestia cavimana, before and after exuviation. This enzyme was ultrahistochemically localized throughout the membranes of the caecal epithelium as well as extracellularly, i.e., within pre-exuvial calcareous concretions and postexuvial calcified spherules. During the molt cycle, the pattern of carbonic anhydrase activity in the posterior caeca was correlated with the calcium content at this level. Acetazolamide treatment in vivo inhibited about 50% of the calcium uptake during both pre-exuvial secretion and postexuvial reabsorption. The role of carbonic anhydrase in this mineralizing-demineralizing epithelium is discussed and compared with that of other mechanisms involved in this calcium turnover.

Recent studies of the mineral phase in bone and its possible linkage to the organic matrix by protein-bound phosphate bonds

The most widely accepted hypothesis to account for maturational changes in the X-ray diffraction characteristics of bone mineral has been the 'amorphous calcium phosphate theory', which postulates that an initial amorphous calcium phosphate solid phase is deposited that gradually converts to poorly crystalline hydroxyapatite. Our studies of bone mineral of different ages by X-ray radial distribution function analysis and 31P n.m.r. have conclusively demonstrated that a solid phase of amorphous calcium phosphate does not exist in bone in any significant amount. 31P n.m.r. studies have detected the presence of acid phosphate groups in a brushite-like configuration. Phosphoproteins containing O-phosphoserine and O-phosphothreonine have been isolated from bone matrix and characterized. Tissue and cell culture have established that they are synthesized in bone, most likely by the osteoblasts. Physiochemical and pathophysiological studies support the thesis that the mineral and organic phases of bone and other vertebrate mineralized tissues are linked by the phosphomonester bonds of O-phosphoserine and O-phosphothreonine, which are constituents of both the structural organic matrix and the inorganic calcium phosphate crystals.

Effect of phosphate deficiency on pulp alkaline phosphatase and Ca2+-, Mg2+-ATPase activity in rats

Phosphate deficiency imposed on weanling rats for two wk resulted in a 40% increase in alkaline phosphatase activity of incisor pulp, without a significant change in Ca2+-, Mg2+-ATPase activity. The results are consistent with a separate identity for the two enzymes, but their physiological roles remain obscure.

The role of synthetic and bone extracted Ca-phospholipid-PO4 complexes in hydroxyapatite formation

The calcium-phospholipid-phosphate (Ca-PL-PO4) complex isolated from young bone has been shown to initiate hydroxyapatite formation from a metastable calcium phosphate solution. The action of the complex was compared to that of the acidic phospholipids: phosphatidyl serine, phosphatidyl inositol and phosphatidic acid. These phospholipids first remove calcium, and a small amount of phosphate from the metastable solution forming a material similar to the complex isolated from bone, and then form hydroxyapatite. The rate of hydroxyapatite proliferation, once phosphatidyl serine and phosphatidyl inositol are converted to Ca-PL-PO4 complexes, is the same as the rate observed for comparable weights of the complex isolated from bone. It is suggested that the complex isolated from bone was formed in a manner similar to the complexes in our in vitro experiments. Finally, our evidence supports the possibility that a similar complex is responsible for the initial mineralization in matrix vesicles.

Extraction of a calcium-phospholipid-phosphate complex from bone

A calcium-phospholipid-phosphate complex with a constant 1:1 calcium to total phosphate molar ratio is shown to exist in rabbit and calf bone. This complex, which may be involved in the transport and deposition of bone mineral, appears to constitute a significantly greater proportion of the lipids of younger bone than of more mature bone. The comples was isolated by a modified Folch extraction employing ultrasonic disruption of cellular material. Evidence is presented to show that the complex is a natural constituent of bone rather than one created artifactually during extraction.