LEUKEMIA INHIBITORY FACTOR AND ONCOSTATIN-M INFLUENCE THE MINERAL PHASES FORMED IN A MURINE HETEROTOPIC CALCIFICATION MODEL - A FOURIER-TRANSFORM INFRARED MICROSPECTROSCOPIC STUDY
S. Bohic et al., LEUKEMIA INHIBITORY FACTOR AND ONCOSTATIN-M INFLUENCE THE MINERAL PHASES FORMED IN A MURINE HETEROTOPIC CALCIFICATION MODEL - A FOURIER-TRANSFORM INFRARED MICROSPECTROSCOPIC STUDY, Journal of bone and mineral research, 13(10), 1998, pp. 1619-1632
The study of bone mineralization processes is of considerable interest
in understanding bone diseases and developing new therapies for skele
tal disorders, particularly since bone homeostasis requires numerous c
ell types and a large cytokine network Cell culture models of minerali
zation have often been used to study the cellular mechanisms of minera
lization, but few data have been reported concerning the influence of
extracellular matrix components and cytokines on the physicochemical p
roperties of mineral. The purpose of this study was to analyze the eff
ects of two cytokines, leukemia inhibitory factor (LIF) and oncostatin
M (OSM), involved in bone metabolism on the physicochemical propertie
s of bone mineral formed in a murine in vivo mineralization model. Mur
ine bone marrow cells implanted under the kidney capsule in the presen
ce or absence of cytokines led to heterotopic ossicle formation. A sca
nning electron microscopic microprobe revealed that heterotopic calcif
ication had a lower (similar to 20%) Ca/P ratio after cytokine treatme
nt as compared with the control without cytokine, Transmission electro
n microscopic analysis of cytokine-treated ossicles showed numerous ar
eas with low mineral density, whereas electron diffraction pattern rev
ealed an apatitic phase. These areas were not observed in the absence
of cytokine, Moreover, Fourier transform-infrared microspectroscopy sh
owed at the molecular level that the presence of either cytokine induc
ed many microscopic areas in which short-range order organization, suc
h as incorporation of carbonate and crystallinity/maturity of ossicle
mineral, were modified. LIF and OSM influenced mineral phase formation
in the present model and may thus be key protagonists in bone mineral
development and skeletal diseases.