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Quantitative atomic force microscopy provides new insight into matrix vesicle mineralization
- Plaut, Justin S., Strzelecka-Kiliszek, Agnieszka, Bozycki, Lukasz, Pikula, Slawomir, Buchet, René, Mebarek, Saida, Chadli, Meriem, Bolean, Maytê, Simao, Ana M.S., Ciancaglini, Pietro, Magrini, Andrea, Rosato, Nicola, Magne, David, Girard-Egrot, Agnès, Farquharson, Colin, Esener, Sadik C., Millan, José L., Bottini, Massimo
- Archives of biochemistry and biophysics 2019 v.667 pp. 14-21
- Fourier transform infrared spectroscopy, atomic force microscopy, calcium, cartilage, chick embryos, crystal structure, energy-dispersive X-ray analysis, hydrodynamics, ions, light scattering, mineralization, modulus of elasticity, phosphates, spectral analysis, transmission electron microscopy, vertebrates, zeta potential
- Matrix vesicles (MVs) are a class of extracellular vesicles that initiate mineralization in cartilage, bone, and other vertebrate tissues by accumulating calcium ions (Ca2+) and inorganic phosphate (Pi) within their lumen and forming a nucleation core (NC). After further sequestration of Ca2+ and Pi, 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 (+Ca2+) and non-mineralizing (–Ca2+) 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 Ca2+. 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.