Interuniversity Institute for Marine Sciences, Eilat 88103, Israel Israel.
Sci Rep. 2013;3:1700. doi: 10.1038/srep01700.
The main source of calcium carbonate (CaCO₃) in the ocean comes from the shells of calcifying planktonic organisms, but substantial amounts of CaCO₃ are also produced in fish intestines. The precipitation of CaCO₃ assists fish in intestinal water absorption and aids in whole body Ca²⁺ homeostasis. Here we report that the product formed in the intestinal lumen of the gilt-head seabream, Sparus aurata, is an amorphous calcium carbonate (ACC) phase. With FTIR spectroscopy and SEM imaging, our study shows that the fish-derived carbonates from S. aurata are maintained as a stable amorphous phase throughout the intestinal tract. Moreover, intestinal deposits contained up to 54 mol% Mg²⁺, the highest concentration yet reported in biogenic ACC. Mg is most likely responsible for stabilizing this inherently unstable mineral. The fish carbonates also displayed initial rapid dissolution when exposed to seawater, exhibiting a significant increase in carbonate concentration.
海洋中碳酸钙(CaCO₃)的主要来源来自于钙化浮游生物的外壳,但鱼类肠道中也会产生大量的 CaCO₃。CaCO₃的沉淀有助于鱼类在肠道中吸收水分,并有助于全身 Ca²⁺的动态平衡。在这里,我们报告说,在真鲷(Sparus aurata)的肠道腔中形成的产物是无定形碳酸钙(ACC)相。通过傅里叶变换红外光谱(FTIR)和扫描电子显微镜(SEM)成像,我们的研究表明,来自 S. aurata 的鱼类衍生碳酸盐在整个肠道中保持稳定的无定形相。此外,肠道沉积物中含有高达 54 mol%的 Mg²⁺,这是迄今为止在生物成因 ACC 中报道的最高浓度。Mg 很可能是稳定这种固有不稳定矿物的原因。当暴露于海水中时,这些鱼源碳酸盐也表现出快速初始溶解,碳酸盐浓度显著增加。