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Dark-field transmission electron microscopy of cortical bone reveals details of extrafibrillar crystals

机译:皮质骨的暗场透射电子显微镜揭示了原纤维外晶体的细节

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摘要

In a previous study we showed that most of the mineral in bone is present in the form of "mineral structures", 5-6 nm-thick, elongated plates which surround and are oriented parallel to collagen fibrils. Using dark-field transmission electron microscopy, we viewed mineral structures in ion-milled sections of cortical human bone cut parallel to the collagen fibrils. Within the mineral structures we observe single crystals of apatite averaging 5.8 +/- 2.7 nm in width and 28 +/- 19 nm in length, their long axes oriented parallel to the fibril axis. Some appear to be composite, co-aligned crystals as thin as 2 nm. From their similarity to TEM images of crystals liberated from deproteinated bone we infer that we are viewing sections through platy crystals of apatite that are assembled together to form the mineral structures. (C) 2014 Elsevier Inc. All rights reserved.
机译:在先前的研究中,我们表明,骨骼中的大多数矿物质以“矿物结构”的形式存在,厚度为5-6 nm的细长板,围绕并平行于胶原原纤维定向。使用暗场透射电子显微镜,我们观察了平行于胶原纤维切割的皮质人类骨骼的离子铣削部分的矿物结构。在矿物结构中,我们观察到磷灰石单晶体的平均宽度为5.8 +/- 2.7 nm,长度为28 +/- 19 nm,其长轴平行于原纤维轴。有些似乎是复合的,共取向的晶体,厚度仅为2 nm。从它们与从脱蛋白的骨骼中释放出来的晶体的TEM图像的相似性,我们可以推断出我们正在观察的是磷灰石板状晶体的切片,这些晶体组装在一起形成了矿物结构。 (C)2014 Elsevier Inc.保留所有权利。

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