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定量原子力显微镜为基质小泡矿化提供新的见解。

Quantitative atomic force microscopy provides new insight into matrix vesicle mineralization.

机构信息

Cancer Early Detection Advanced Research Center, Knight Cancer Institute, Oregon Health & Science University, Portland, OR, 97201, USA; Department of Bioengineering, University of California San Diego, La Jolla, CA, 92093, USA.

Laboratory of Biochemistry of Lipids, Nencki Institute of Experimental Biology, Polish Academy of Sciences, 02-093, Warsaw, Poland.

出版信息

Arch Biochem Biophys. 2019 May 30;667:14-21. doi: 10.1016/j.abb.2019.04.003. Epub 2019 Apr 16.

Abstract

Matrix vesicles (MVs) are a class of extracellular vesicles that initiate mineralization in cartilage, bone, and other vertebrate tissues by accumulating calcium ions (Ca) and inorganic phosphate (P) within their lumen and forming a nucleation core (NC). After further sequestration of Ca and P, the NC transforms into crystalline complexes. Direct evidence of the existence of the NC and its maturation have been provided solely by analyses of dried samples. We isolated MVs from chicken embryo cartilage and used atomic force microscopy peak force quantitative nanomechanical property mapping (AFM-PFQNM) to measure the nanomechanical and morphological properties of individual MVs under both mineralizing (+Ca) and non-mineralizing (-Ca) fluid conditions. The elastic modulus of MVs significantly increased by 4-fold after incubation in mineralization buffer. From AFM mapping data, we inferred the morphological changes of MVs as mineralization progresses: prior to mineralization, a punctate feature, the NC, is present within MVs and this feature grows and stiffens during mineralization until it occupies most of the MV lumen. Dynamic light scattering showed a significant increase in hydrodynamic diameter and no change in the zeta potential of hydrated MVs after incubation with Ca. This validates that crystalline complexes, which are strongly negative relative to MVs, were forming within the lumen of MVs. These data were substantiated by transmission electron microscopy energy dispersive X-ray and Fourier transform infrared spectroscopic analyses of dried MVs, which provide evidence that the complexes increased in size, crystallinity, and Ca/P ratio within MVs during the mineralization process.

摘要

基质小泡 (MVs) 是一类细胞外囊泡,通过在其腔室内积累钙离子 (Ca) 和无机磷酸盐 (P) 并形成成核核心 (NC),从而启动软骨、骨骼和其他脊椎动物组织中的矿化过程。在进一步隔离 Ca 和 P 后,NC 转化为结晶复合物。NC 的存在及其成熟的直接证据仅通过对干燥样本的分析提供。我们从鸡胚软骨中分离出 MVs,并使用原子力显微镜峰值力定量纳米力学特性映射 (AFM-PFQNM) 来测量在矿化 (+Ca) 和非矿化 (-Ca) 流体条件下单个 MVs 的纳米力学和形态特性。在矿化缓冲液中孵育后,MVs 的弹性模量显著增加了 4 倍。从 AFM 映射数据中,我们推断出 MV 随着矿化过程的形态变化:在矿化之前,MV 内存在点状特征,即 NC,并且该特征在矿化过程中生长并变硬,直到占据 MV 腔室的大部分。动态光散射显示,在 Ca 孵育后,水合 MVs 的水动力直径显著增加,而 ζ 电位没有变化。这验证了在 MV 腔室内形成了相对于 MV 强烈负电性的结晶复合物。这些数据通过对干燥 MVs 的透射电子显微镜能量色散 X 射线和傅里叶变换红外光谱分析得到证实,这些分析提供了证据,证明在矿化过程中,复合物在 MV 内的大小、结晶度和 Ca/P 比增加。

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