Sorbonne Université, CNRS, Laboratoire de Réactivité de Surface, LRS, F-75005 Paris, France.
Université de Technologie de Compiègne, CNRS, Laboratoire de Biomécanique & Bioingénierie, F-60205 Compiègne, France.
Int J Mol Sci. 2021 Nov 30;22(23):12957. doi: 10.3390/ijms222312957.
Biomineralization is the process by which organisms produce hard inorganic matter from soft tissues with outstanding control of mineral deposition in time and space. For this purpose, organisms deploy a sophisticated "toolkit" that has resulted in significant evolutionary innovations, for which calcium phosphate (CaP) is the biomineral selected for the skeleton of vertebrates. While CaP mineral formation in aqueous media can be investigated by studying thermodynamics and kinetics of phase transitions in supersaturated solutions, biogenic mineralization requires coping with the inherent complexity of biological systems. This mainly includes compartmentalization and homeostatic processes used by organisms to regulate key physiological factors, including temperature, pH and ion concentration. A detailed analysis of the literature shows the emergence of two main views describing the mechanism of CaP biomineralization. The first one, more dedicated to the study of in vivo systems and supported by researchers in physiology, often involves matrix vesicles (MVs). The second one, more investigated by the physicochemistry community, involves collagen intrafibrillar mineralization particularly through in vitro acellular models. Herein, we show that there is an obvious need in the biological systems to control both where and when the mineral forms through an in-depth survey of the mechanism of CaP mineralization. This necessity could gather both communities of physiologists and physicochemists under a common interest for an enzymatic approach to better describe CaP biomineralization. Both homogeneous and heterogeneous enzymatic catalyses are conceivable for these systems, and a few preliminary promising results on CaP mineralization for both types of enzymatic catalysis are reported in this work. Through them, we aim to describe the relevance of our point of view and the likely findings that could be obtained when adding an enzymatic approach to the already rich and creative research field dealing with CaP mineralization. This complementary approach could lead to a better understanding of the biomineralization mechanism and inspire the biomimetic design of new materials.
生物矿化是生物体从软组织中产生硬无机物质的过程,具有出色的时空控制矿物质沉积的能力。为此,生物体利用一种复杂的“工具包”,从而导致了重大的进化创新,其中钙磷酸盐(CaP)是脊椎动物骨骼选择的生物矿化物质。虽然可以通过研究过饱和度溶液中相转变的热力学和动力学来研究水介质中 CaP 矿物的形成,但生物矿化需要应对生物系统固有的复杂性。这主要包括生物体用于调节关键生理因素(包括温度、pH 值和离子浓度)的隔室化和动态平衡过程。对文献的详细分析表明,出现了两种主要观点来描述 CaP 生物矿化的机制。第一种观点更专注于体内系统的研究,并得到生理学家的支持,通常涉及基质囊泡(MVs)。第二种观点更多地被物理化学界研究,涉及胶原纤维内矿化,特别是通过体外无细胞模型。在这里,我们通过深入调查 CaP 矿化的机制,表明生物系统明显需要控制矿物质形成的位置和时间,这就需要将生理学家和物理化学家这两个群体聚集在一起,共同关注酶法来更好地描述 CaP 生物矿化。对于这些系统,可以设想均相和多相酶催化,并且在这项工作中报告了这两种类型的酶催化在 CaP 矿化方面的一些初步有希望的结果。通过这些结果,我们旨在描述我们观点的相关性以及在将酶法添加到已经丰富而富有创意的 CaP 矿化研究领域中时可能获得的发现。这种补充方法可以更好地理解生物矿化机制,并激发新材料的仿生设计。