在模拟生物条件下沉淀的文石硬度提高的来源。

IF 2.7 2区 地球科学 Q2 BIOLOGY
Geobiology Pub Date : 2026-09-10 DOI:10.1111/gbi.70060
Boontharee Chomhom, Gabriela A. Farfan, Samantha Greeves, Kirsty Penkman, Adrian A. Finch, Susan Fitzer, Roland Kröger, Alex Brasier, John Still, Matthieu Clog, Nicola Allison
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引用次数: 0

摘要

生物文石是一种矿物和生物分子的复合物,与无机类似物相比,它具有优越的材料性能。这一优势为支持珊瑚礁和贝壳渔业的生物文石结构的成功奠定了基础,但提高生物文石物理弹性的机制尚不清楚。在这项研究中,文石是在模拟海洋生物钙化部位的化学条件下合成的。将溶液中的天冬氨酸、谷氨酸和甘氨酸以通常在海洋生物矿物中观察到的浓度掺入文石中,并观察到显著提高文石维氏硬度。天冬氨酸的掺入比谷氨酸或甘氨酸更有效,但对于相当数量的氨基酸掺入,甘氨酸比天冬氨酸或谷氨酸更显著地改善文石硬度。甘氨酸和谷氨酸的掺入减小了文石晶粒尺寸,从而通过晶界的能量耗散提高了文石对压痕的弹性。相比之下,天冬氨酸也可以在较小的范围内提高硬度,可能是由于晶体结构扭曲。这些结果表明,氨基酸掺入通过多种机制影响文石硬度,并为探索更复杂的生物矿物蛋白的影响提供了一个原型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Origins of Improved Hardness in Bioinspired Aragonite Precipitated Under Simulated Biologic Conditions

Biogenic aragonite is a composite of mineral and biomolecules that exhibits superior material properties compared to its inorganic analog. This superiority underpins the success of the bioaragonite structures which support coral reefs and shell fisheries, yet the mechanisms improving the physical resilience of bioaragonite are not well understood. In this study, aragonite is synthesised under chemical conditions which simulate those of calcification sites in marine organisms. Aspartic acid, glutamic acid, and glycine in solution are incorporated into the aragonite at concentrations typically observed in marine biominerals and are observed to significantly improve aragonite Vickers hardness. Aspartic acid is incorporated more efficiently than glutamic acid or glycine, but for comparable amounts of amino acid incorporation, glycine improves aragonite hardness significantly more than either aspartic or glutamic acid. Glycine and glutamic acid incorporation reduce the aragonite grain size, thereby improving resilience to indentation via energy dissipation along grain boundaries. In contrast, aspartic acid also improves hardness on a smaller scale, possibly due to crystal structure distortions. These results suggest that amino acid incorporation influences biogenic aragonite hardness via multiple mechanisms and provide a prototype for exploring the influence of more complicated biomineral proteins.

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来源期刊
Geobiology
Geobiology 生物-地球科学综合
CiteScore
6.80
自引率
5.40%
发文量
56
审稿时长
3 months
期刊介绍: The field of geobiology explores the relationship between life and the Earth''s physical and chemical environment. Geobiology, launched in 2003, aims to provide a natural home for geobiological research, allowing the cross-fertilization of critical ideas, and promoting cooperation and advancement in this emerging field. We also aim to provide you with a forum for the rapid publication of your results in an international journal of high standing. We are particularly interested in papers crossing disciplines and containing both geological and biological elements, emphasizing the co-evolutionary interactions between life and its physical environment over geological time. Geobiology invites submission of high-quality articles in the following areas: Origins and evolution of life Co-evolution of the atmosphere, hydrosphere and biosphere The sedimentary rock record and geobiology of critical intervals Paleobiology and evolutionary ecology Biogeochemistry and global elemental cycles Microbe-mineral interactions Biomarkers Molecular ecology and phylogenetics.
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