Nam Onyou, Suzuki Iwane, Shiraiwa Yoshihiro, Jin EonSeon
Department of Life Science, Research Institute for Natural Sciences, Hanyang University, Seoul 04763, Korea.
Faculty of Life and Environmental Sciences, University of Tsukuba, Tsukuba, Ibaraki 305-8572, Japan.
Microorganisms. 2020 Sep 10;8(9):1389. doi: 10.3390/microorganisms8091389.
Biomineralization by calcifying microalgae is a precisely controlled intracellular calcification process that produces delicate calcite scales (or coccoliths) in the coccolithophore (Haptophycea). Despite its importance in biogeochemical cycles and the marine environment globally, the underlying molecular mechanism of intracellular coccolith formation, which requires calcium, bicarbonate, and coccolith-polysaccharides, remains unclear. In CCMP 371, we demonstrated that reducing the calcium concentration from 10 (ambient seawater) to 0.1 mM strongly restricted coccolith production, which was then recovered by adding 10 mM calcium, irrespective of inorganic phosphate conditions, indicating that coccolith production could be finely controlled by the calcium supply. Using this strain, we investigated the expression of differentially expressed genes (DEGs) to observe the cellular events induced by changes in calcium concentrations. Intriguingly, DEG analysis revealed that the phosphatidylinositol-specific phospholipase C (PI-PLC) gene was upregulated and coccolith production by cells was blocked by the PI-PLC inhibitor U73122 under conditions closely associated with calcium-induced calcification. These findings imply that PI-PLC plays an important role in the biomineralization process of the coccolithophore .
钙化微藻的生物矿化是一个精确控制的细胞内钙化过程,在颗石藻(定鞭藻纲)中产生精致的方解石鳞片(或颗石)。尽管其在全球生物地球化学循环和海洋环境中具有重要意义,但细胞内颗石形成的潜在分子机制仍不清楚,这一过程需要钙、碳酸氢盐和颗石多糖。在CCMP 371中,我们证明将钙浓度从10 mM(环境海水)降至0.1 mM会强烈限制颗石的产生,然后通过添加10 mM钙使其恢复,无论无机磷酸盐条件如何,这表明颗石的产生可以通过钙供应精细控制。利用该菌株,我们研究了差异表达基因(DEG)的表达,以观察钙浓度变化诱导的细胞事件。有趣的是,DEG分析显示磷脂酰肌醇特异性磷脂酶C(PI-PLC)基因上调,并且在与钙诱导钙化密切相关的条件下,细胞的颗石产生被PI-PLC抑制剂U73122阻断。这些发现表明PI-PLC在颗石藻的生物矿化过程中起重要作用。