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绵羊椎间盘钙化:羟基磷灰石沉积病模型

Calcification in the ovine intervertebral disc: a model of hydroxyapatite deposition disease.

作者信息

Melrose James, Burkhardt D, Taylor T K F, Dillon C T, Read R, Cake M, Little C B

机构信息

Raymond Purves Research Laboratory, Institute of Bone and Joint Research, Kolling Institute of Medical Research, University of Sydney, Royal North Shore Hospital, St. Leonards, Sydney, NSW, Australia.

出版信息

Eur Spine J. 2009 Apr;18(4):479-89. doi: 10.1007/s00586-008-0871-y. Epub 2009 Jan 23.

Abstract

The study design included a multidisciplinary examination of the mineral phase of ovine intervertebral disc calcifications. The objective of the study was to investigate the mineral phase and its mechanisms of formation/association with degeneration in a naturally occurring animal model of disc calcification. The aetiology of dystrophic disc calcification in adult humans is unknown, but occurs as a well-described clinical disorder with hydroxyapatite as the single mineral phase. Comparable but age-related pathology in the sheep could serve as a model for the human disorder. Lumbar intervertebral discs (n = 134) of adult sheep of age 6 years (n = 4), 8 years (n = 12) and 11 years (n = 2) were evaluated using radiography, morphology, scanning and transmission electron microscopy, energy dispersive X-ray spectroscopy, X-ray powder diffraction, histology, immunohistology and proteoglycan analysis. Half of the 6-year, 84% of the 8-year and 86% of the 11-year-old discs had calcific deposits. These were not well delineated by plain radiography. They were either: (a) punctate deposits in the outer annulus, (b) diffuse deposits in the transitional zone or inner annulus fibrosus with occasional deposits in the nucleus, or (c) large deposits in the transitional zone extending variably into the nucleus. Their maximal incidence was in the lower lumbar discs (L4/5-L6/7) with no calcification seen in the lumbosacral or lower thoracic discs. All deposits were hydroxyapatite with large crystallite sizes (800-1,300 A) compared to cortical bone (300-600 A). No type X-collagen, osteopontin or osteonectin were detected in calcific deposits, although positive staining for bone sialoprotein was evident. Calcified discs had less proteoglycan of smaller hydrodynamic size than non-calcified discs. Disc calcification in ageing sheep is due to hydroxyapatite deposition. The variable, but large, crystal size and lack of protein markers indicate that this does not occur by an endochondral ossification-like process. The decrease in disc proteoglycan content and size suggests that calcification may precede or predispose to disc degeneration in ageing sheep.

摘要

该研究设计包括对绵羊椎间盘钙化矿化相的多学科检查。本研究的目的是在椎间盘钙化的自然发生动物模型中研究矿化相及其形成机制/与退变的关联。成人营养不良性椎间盘钙化的病因尚不清楚,但它作为一种已被充分描述的临床病症出现,其中羟基磷灰石是唯一的矿化相。绵羊中类似但与年龄相关的病理学情况可作为人类该病症的模型。对6岁(n = 4)、8岁(n = 12)和11岁(n = 2)成年绵羊的腰椎间盘(n = 134)进行了X线摄影、形态学、扫描和透射电子显微镜检查、能量色散X射线光谱分析、X射线粉末衍射、组织学、免疫组织学和蛋白聚糖分析。6岁绵羊的椎间盘中有一半、8岁绵羊的84%以及11岁绵羊的86%有钙化沉积物。这些钙化沉积物在普通X线摄影中显示不清晰。它们要么是:(a)外环中的点状沉积物,(b)过渡区或内环纤维环中的弥漫性沉积物,偶尔在髓核中也有沉积物,要么是(c)过渡区中的大沉积物,不同程度地延伸到髓核中。其最高发生率出现在下腰椎间盘(L4/5 - L6/7),腰骶部或下胸段椎间盘未见钙化。所有沉积物均为羟基磷灰石,与皮质骨(300 - 600 Å)相比,其微晶尺寸较大(800 - 1300 Å)。尽管骨唾液蛋白染色呈阳性,但在钙化沉积物中未检测到X型胶原蛋白、骨桥蛋白或骨连接蛋白。钙化椎间盘的蛋白聚糖比未钙化椎间盘的蛋白聚糖具有更小的流体动力学尺寸且含量更少。衰老绵羊的椎间盘钙化是由于羟基磷灰石沉积。晶体尺寸可变但较大且缺乏蛋白质标志物表明,这不是通过类似软骨内成骨的过程发生的。椎间盘蛋白聚糖含量和尺寸的减少表明,钙化可能先于或易导致衰老绵羊的椎间盘退变。

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