在碳酸形成过程中组装骨内珊瑚有机基质
Silvia Milita1, Tal Zaquin2, Simona Fermani3,4
1CNR-Institute for Microelectronic and Microsystems, via Gobetti 101, Bologna 40129, Italy.
Crystal growth & design
|August 7, 2023
概括
珊瑚的可溶性有机基质 (SOM) 分子影响碳酸的形成. SOM自组装成分层结构,将石的生长指向基板和溶液中的无形碳酸.
科学领域:
- 生物矿物化 生物矿物化
- 材料科学 材料科学 材料科学
- 海洋生物学 海洋生物学
背景情况:
- 斯克莱拉克提尼亚珊瑚骨架的形成涉及阿拉贡石沉.
- 溶性有机基质 (SOM) 分子对于珊瑚生物矿化至关重要,影响碳酸的形状和多态性.
- 在SOM中介的阿拉贡石生长的结构方面还不太清楚.
研究的目的:
- 研究珊瑚SOM对碳酸沉积的结构影响.
- 为了比较不同珊瑚物种SOM对矿物形成的影响.
- 阐明在碳酸核和生长过程中SOM的自我组装和结构行为.
主要方法:
- 牧场发生率X射线衍射 (GIXRD)
- 拉曼光谱法 拉曼光谱法
- 电子和光学显微镜的使用.
- 碳酸沉积在基板上,在提取的珊瑚SOM的存在下.
主要成果:
- 吸附的SOM自组装成分层结构,诱导导导向酸盐的生长,并抑制酸盐.
- 在溶液中分散的SOM诱导无形碳酸 (ACC) 沉积,保持了分层结构.
- 观察到的效应取决于物种,与之前的研究一致.
- 珊瑚SOM表现出一个2D状结构,保留了ACC,但与石丢失了.
结论:
- 珊瑚SOM在指导碳酸多态和结构方面发挥着重要作用.
- SOM的二维状结构是其与碳酸相互作用的关键特征.
- 这些发现为珊瑚生物矿物化提供了新的见解,并对研究其他生物体中的生物矿物化有更广泛的影响.
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