Fourier transform infrared imaging as a tool to chemically and spatially characterize matrix-mineral deposition in osteoblasts.

Mineralizing osteoblasts are regularly used to study osteogenesis and model in vivo bone formation. Thus, it is important to verify that the mineral and matrix being formed in situ are comparable to those found in vivo. However, it has been shown that histochemical techniques alone are not sufficient for identifying calcium phosphate-containing mineral. The goal of the present study was to demonstrate the use of Fourier transform infrared imaging (FTIRI) as a tool for characterizing the spatial distribution and colocalization of the collagen matrix and the mineral phase during the mineralization process of osteoblasts in situ. MC3T3-E1 mouse osteoblasts were mineralized in culture for 28 days and FTIRI was used to evaluate the collagen content, collagen cross-linking, mineralization level and speciation, and mineral crystallinity in a spatially resolved fashion as a function of time. To test whether FTIRI could detect subtle changes in the mineralization process, cells were treated with risedronate (RIS). Results showed that collagen deposition and mineralization progressed over time and that the apatite mineral was associated with a collagenous matrix rather than ectopic mineral. The process was temporarily slowed by RIS, where the inhibition of osteoblast function caused slowed collagen production and cross-linking, leading to decreased mineralization. This study demonstrates that FTIRI is a complementary tool to histochemistry for spatially correlating the collagen matrix distribution and the nature of the resultant mineral during the process of osteoblast mineralization. It can further be used to detect small perturbations in the osteoid and mineral deposition process.