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Initial stages of calcium uptake and mineral deposition in sea urchin embryos

机译:海胆胚胎中钙摄取和矿物质沉积的初始阶段

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摘要

Sea urchin larvae have an endoskeleton consisting of two calcitic spicules. We reconstructed various stages of the formation pathway of calcium carbonate from calcium ions in sea water to mineral deposition and integration into the forming spicules. Monitoring calcium uptake with the fluorescent dye calcein shows that calcium ions first penetrate the embryo and later are deposited intracellularly. Surprisingly, calcium carbonate deposits are distributed widely all over the embryo, including in the primary mesenchyme cells and in the surface epithelial cells. Using cryo-SEM, we show that the intracellular calcium carbonate deposits are contained in vesicles of diameter 0.5–1.5 μm. Using the newly developed airSEM, which allows direct correlation between fluorescence and energy dispersive spectroscopy, we confirmed the presence of solid calcium carbonate in the vesicles. This mineral phase appears as aggregates of 20–30-nm nanospheres, consistent with amorphous calcium carbonate. The aggregates finally are introduced into the spicule compartment, where they integrate into the growing spicule.
机译:海胆幼虫的内骨骼由两个钙突针组成。我们重建了碳酸钙形成途径的各个阶段,从海水中的钙离子到矿物质沉积并整合到形成的针状物中。用荧光染料钙黄绿素监测钙的摄取表明钙离子首先穿透胚胎,然后沉积在细胞内。令人惊讶的是,碳酸钙沉积物广泛分布于整个胚胎,包括在原代间充质细胞和表面上皮细胞中。使用cryo-SEM,我们发现细胞内碳酸钙沉积物包含在直径0.5–1.5μm的囊泡中。使用新开发的airSEM,它可以使荧光光谱和能量色散光谱直接相关,我们证实了囊泡中存在固体碳酸钙。该矿物相以20–30 nm纳米球的聚集体形式出现,与无定形碳酸钙一致。最后,将聚集体引入到针刺隔室中,在那里它们整合到正在生长的针刺中。

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