Department of Materials Science and Engineering, McMaster University, Hamilton L8S 4L7, Ontario, Canada.
Department of Biomaterials, Sahlgrenska Academy, University of Gothenburg, Göteborg 40530, Sweden.
ACS Nano. 2023 Dec 26;17(24):24710-24724. doi: 10.1021/acsnano.3c04633. Epub 2023 Oct 17.
Mineralized collagen fibrils are the building block units of bone at the nanoscale. While it is known that collagen fibrils are mineralized both inside their gap zones (intra-fibrillar mineralization) and on their outer surfaces (extra-fibrillar mineralization), a clear visualization of this architecture in three dimensions (3D), combining structural and compositional information over large volumes, but without compromising the resolution, remains challenging. In this study, we demonstrate the use of on-axis -contrast electron tomography (ET) with correlative energy-dispersive X-ray spectroscopy (EDX) tomography to examine rod-shaped samples with diameters up to 700 nm prepared from individual osteonal lamellae in the human femur. Our work mainly focuses on two aspects: (i) low-contrast nanosized circular spaces ("holes") observed in sections of bone oriented perpendicular to the long axis of a long bone, and (ii) extra-fibrillar mineral, especially in terms of morphology and spatial relationship with respect to intra-fibrillar mineral and collagen fibrils. From our analyses, it emerges quite clearly that most "holes" are cross-sectional views of collagen fibrils. While this had been postulated before, our 3D reconstructions and reslicing along meaningful two-dimensional (2D) cross-sections provide a direct visual confirmation. Extra-fibrillar mineral appears to be composed of thin plates that are interconnected and span over several collagen fibrils, confirming that mineralization is cross-fibrillar, at least for the extra-fibrillar phase. EDX tomography shows mineral signatures (Ca and P) within the gap zones, but the signal appears weaker than that associated with the extra-fibrillar mineral, pointing toward the existence of dissimilarities between the two types of mineralization.
矿化胶原纤维是纳米尺度骨的结构单元。虽然已知胶原纤维在其间隙区(纤维内矿化)和外表面(纤维外矿化)都有矿化,但在不影响分辨率的情况下,对大体积的三维(3D)结构和组成信息进行清晰的可视化仍然具有挑战性。在这项研究中,我们展示了使用轴向对比电子断层扫描(ET)与相关能量色散 X 射线光谱(EDX)断层扫描来检查来自人类股骨骨单位的单个骨板制备的直径达 700nm 的棒状样品。我们的工作主要集中在两个方面:(i)在垂直于长骨长轴的骨切片中观察到的低对比度纳米级圆形空间(“孔”),以及(ii)纤维外矿化,特别是在形态和与纤维内矿化和胶原纤维的空间关系方面。从我们的分析中可以清楚地看出,大多数“孔”是胶原纤维的横截面。虽然之前已经提出过这种假设,但我们的 3D 重建和沿有意义的二维(2D)横截面的重新切片提供了直接的可视化确认。纤维外矿化似乎由薄片状的矿物质组成,这些矿物质相互连接并跨越几个胶原纤维,证实矿化是交叉纤维的,至少对于纤维外矿化阶段是如此。EDX 断层扫描显示在间隙区存在矿物质特征(Ca 和 P),但信号比与纤维外矿化相关的信号弱,表明两种类型的矿化之间存在差异。