Nanotechnology and Integrated Bioengineering Centre, University of Ulster, Northern Ireland.
Analyst. 2011 Jun 21;136(12):2471-81. doi: 10.1039/c1an15167c. Epub 2011 May 4.
The differentiation of stem cells into multi-lineages is essential to aid the development of tissue engineered materials that replicate the functionality of their tissue of origin. For this study, Raman spectroscopy was used to monitor the formation of a bone-like apatite mineral during the differentiation of human mesenchymal stem cells (hMSCs) towards an osteogenic lineage. Raman spectroscopy observed dramatic changes in the region dominated by the stretching of phosphate groups (950-970 cm(-1)) during the period of 7-28 days. Changes were also seen at 1030 cm(-1) and 1070 cm(-1), which are associated with the P-O symmetric stretch of PO(4)(3-) and the C-O vibration in the plane stretch of CO(3)(2-). Multivariate factor analysis revealed the presence of various mineral species throughout the 28 day culture period. Bone mineral formation was observed first at day 14 and was identified as a crystalline, non-substituted apatite. During the later stages of culture, different mineral species were observed, namely an amorphous apatite and a carbonate, substituted apatite, all of which are known to be Raman markers for a bone-like material. Band area ratios revealed that both the carbonate-to-phosphate and mineral-to-matrix ratios increased with age. When taken together, these findings suggest that the osteogenic differentiation of hMSCs at early stages resembles endochondral ossification. Due to the various mineral species observed, namely a disordered amorphous apatite, a B-type carbonate-substituted apatite and a crystalline non-substituted hydroxyapatite, it is suggested that the bone-like mineral observed here can be compared to native bone. This work demonstrates the successful application of Raman spectroscopy combined with biological and multivariate analyses for monitoring the various mineral species, degree of mineralisation and the crystallinity of hMSCs as they differentiate into osteoblasts.
干细胞向多谱系分化对于帮助开发组织工程材料至关重要,这些材料能够复制其原始组织的功能。在这项研究中,拉曼光谱被用于监测人骨髓间充质干细胞(hMSCs)向成骨谱系分化过程中形成类骨质磷灰石矿的过程。在 7-28 天的时间内,拉曼光谱观察到磷酸基团拉伸区域(950-970 cm(-1))发生了剧烈变化。在 1030 cm(-1)和 1070 cm(-1)处也观察到了变化,这与 PO(4)(3-)的 P-O 对称拉伸和 CO(3)(2-)平面拉伸中的 C-O 振动有关。多变量因子分析显示,在整个 28 天的培养过程中存在各种矿物物种。在第 14 天观察到骨矿物质的形成,被鉴定为结晶、无取代的磷灰石。在培养的后期,观察到不同的矿物物种,即无定形磷灰石和碳酸根取代的磷灰石,所有这些都是骨样材料的拉曼标志物。带面积比表明,碳酸根与磷酸根的比值和矿物与基质的比值都随着时间的增加而增加。总的来说,这些发现表明 hMSCs 的成骨分化在早期阶段类似于软骨内骨化。由于观察到的各种矿物物种,即无序的无定形磷灰石、B 型碳酸根取代的磷灰石和结晶的非取代羟磷灰石,因此可以认为这里观察到的类骨质矿物可以与天然骨相媲美。这项工作展示了拉曼光谱结合生物学和多变量分析在监测 hMSCs 向成骨细胞分化过程中各种矿物物种、矿化程度和结晶度的成功应用。