在预成形的阿拉贡石中,通过竞争性Sr2+替代产生的Ca1-x-Sr-x-CO3相的分析
Saja Nasser1, Gili Cohen-Taguri1, Tali Mass2
1Department of Chemistry and Institute of Nanotechnology and Advanced Materials, Bar-Ilan University, Ramat-Gan 5290002, Israel.
海洋生物矿物质中与的比率是关键的地化学标志物. 这项研究揭示了如何被纳入阿拉戈尼特晶体,模仿珊瑚生物矿物化,取决于环境中的度.
科学领域:
- 地质化学 地质化学
- 生物矿物化 生物矿物化
- 海洋科学 海洋科学
背景情况:
- 在海洋生物矿物中与 (Sr/Ca) 的比率对于重建过去的海洋条件至关重要.
- 控制珊瑚骨中Sr/Ca比率的确切机制,无论是环境还是有机,仍在争论中.
研究的目的:
- 为了研究在阿拉贡石晶体中体替代的实验室替代.
- 了解矿化溶液中的度与在阿拉戈尼特和斯特朗提亚尼特中的结合之间的关系.
主要方法:
- 阿拉戈尼特晶体的沉.
- 阿拉贡石晶体暴露在不同度的溶液中.
- 在得到的双相物质 (Sr-doped aragonite和Ca-doped strontianite) 中对阴离子替代的分析.
主要成果:
- 在矿化溶液中的含量和结合在阿拉戈尼特中的和结合在斯特朗提亚尼特之间建立了线性相关性.
- 晶体替代所需的离子溶液度大约是5倍,以匹配珊瑚中发现的水平.
- 确定了形成石酸阶段所需的特定水平.
结论:
- 该研究提供了关于海生物体中的生物矿化过程的见解.
- 环境中的度显著影响了的纳入阿拉戈尼特和斯特朗提亚尼特.
- 这些发现有助于改进使用Sr/Ca比率作为古海洋学代理的方法.
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