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人骨关节炎软骨基质小泡在体外可生成二水焦磷酸钙和磷灰石。

Human osteoarthritic cartilage matrix vesicles generate both calcium pyrophosphate dihydrate and apatite in vitro.

作者信息

Derfus B, Kranendonk S, Camacho N, Mandel N, Kushnaryov V, Lynch K, Ryan L

机构信息

The Medical College of Wisconsin, Division of Rheumatology, 9200 W. Wisconsin Avenue, Milwaukee, Wisconsin 53226, USA.

出版信息

Calcif Tissue Int. 1998 Sep;63(3):258-62. doi: 10.1007/s002239900523.

Abstract

Calcium crystals in osteoarthritic (OA) joints promote enzymatic degradation of articular tissues. Matrix vesicles provide a nidus for calcium crystal formation in chick epiphyseal and mature porcine articular cartilage. In order to examine a potential role for matrix vesicles from OA cartilage in generating pathologic crystals, we sought to determine whether vesicles derived from human OA cartilage (OAMV) could mineralize; and we characterized the resultant mineral species. OAMV were isolated and examined for alkaline phosphatase (AP) and nucleoside triphosphate pyrophosphohydrolase (NTPPPH) activity. OAMV ATP-dependent and independent mineralization were measured in a radiometric biomineralization assay, and newly formed OAMV crystals were examined using Fourier transform infrared spectroscopy (FTIR) and compensated polarized light microscopy. The mean specific activity of OAMV AP was approximately 6 times higher and NTPPPH activity 11 times lower than that of previously characterized, mature, porcine, articular cartilage vesicles. OAMV progressively precipitated 45Ca over time both in the presence and absence of ATP. The FTIR spectra of mineral formed in ATP-dependent assays most closely resembled the standard spectrum for calcium pyrophosphate dihydrate (CPPD). The FTIR spectra of OAMV mineral formed in the absence of ATP closely resembled apatite. These data support the hypothesis that OAMV may form mineral phases of two key crystals found in degenerating cartilage and provide further evidence for the role of matrix vesicles in pathologic articular cartilage biomineralization.

摘要

骨关节炎(OA)关节中的钙晶体可促进关节组织的酶促降解。基质小泡为雏鸡骨骺和成熟猪关节软骨中的钙晶体形成提供了核心。为了研究来自OA软骨的基质小泡在生成病理性晶体中的潜在作用,我们试图确定源自人OA软骨的小泡(OAMV)是否能够矿化;并且我们对生成的矿物质种类进行了表征。分离出OAMV并检测其碱性磷酸酶(AP)和核苷三磷酸焦磷酸水解酶(NTPPPH)活性。在放射性生物矿化试验中测量OAMV的ATP依赖性和非依赖性矿化,并使用傅里叶变换红外光谱(FTIR)和补偿偏振光显微镜检查新形成的OAMV晶体。OAMV的AP平均比活性比先前表征的成熟猪关节软骨小泡高约6倍,而NTPPPH活性低11倍。无论有无ATP,OAMV都会随着时间的推移逐渐沉淀45Ca。在ATP依赖性试验中形成的矿物质的FTIR光谱与二水合焦磷酸钙(CPPD)的标准光谱最为相似。在没有ATP的情况下形成的OAMV矿物质的FTIR光谱与磷灰石非常相似。这些数据支持这样的假设:OAMV可能形成退变软骨中发现的两种关键晶体的矿相,并为基质小泡在病理性关节软骨生物矿化中的作用提供了进一步的证据。

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