Aragonite is an important dimorph of calcium carbonate, industrially and biologically. However, aragonite is so thermodynamically unstable that it is difficult to understand its formation mechanism. A continuous microfluidic system was employed, in which crystallization was induced only by diffusion in a micron-scale channel. Calcium carbonate (CaCO 3 ) formed by liquid-liquid reaction and magnesium ions (Mg 2+ ) were used as additives. To assess the influence of Mg 2+ concentration, the Mg 2+ /Ca 2+ molar ratio was set to 1, 3, and 5. Laminar streams flowed in the detection channel with different concentration gradients. The initial crystallization time (t I.C ) increased exponentially and the density of crystals decreased as the Mg 2+ ion concentration increased. Following transformation of all particles into snowman or sphere shapes, they became spinose sphere-shaped crystals, which was the final form in this study.