球霰石
核苷酸
无定形碳酸钙
化学
碳酸钙
核酸
方解石
无水的
结晶学
晶体结构
Crystal(编程语言)
碳酸盐
生物矿化
无定形固体
矿物学
化学工程
有机化学
生物化学
程序设计语言
计算机科学
文石
工程类
基因
作者
Arad Lang,Iryna Polishchuk,Alexander Katsman,Boaz Pokroy
标识
DOI:10.1021/acs.cgd.3c00367
摘要
The interactions of organic hereditary materials (i.e., DNA and RNA) with inorganic minerals are of key importance in many fields of research, from archeology and paleontology to medicine. It was previously shown that the building blocks of the main structural biomacromolecules, amino acids and monosaccharides, can be incorporated into the crystal lattice of calcium carbonate (CaCO3), the most abundant biomineral. Here, we continue this reductionist approach and study how the mineral host is affected when grown in the presence of mono- or triphosphate nucleotides─the building blocks of nucleic acids. We show that the nucleotides facilitate the stabilization of the amorphous polymorph of CaCO3, as well as promote the formation of vaterite, its least thermodynamically stable anhydrous crystalline phase. We use high-resolution powder X-ray diffraction, and a variety of chemical analysis tools, to demonstrate the mechanism by which nucleotides become incorporated within the vaterite lattice.
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