We investigated the biomineralization process of calcium carbonate deposition in the spicules of the calcareous sponge Heteropia glomerosa (Porifera, Calcarea). The finely polished spicules, composed of Mg-calcite, present a pattern of concentric lines spaced 400 nm apart when observed by scanning electron microscopy. We showed by electron backscattered diffraction that the whole spicule length has the same crystallographic orientation. Still, misorientation of up to 1.8 ? (~ 2 µm) and a continuous increase in the misalignment of up to 4.5 ? in adjacent regions (~ 2 µm) and a continuous increase in the misalignment of up to in regions separated by 300 µm were present. The sponge cells (mainly sclerocytes and pinacocytes) near the mineralization zone contain a high number of vesicles rich in calcium, which could be involved in the spicule biomineralization. We showed by electron and ion microscopies that the spicule growth occurs through the addition calcium carbonate granules, which form near the membrane of the sclerocyte, the cell responsible for biomineralization. The granules were deposited layer by layer on the surface of the spicule, increasing the biomineral thickness. Domains of 1–3 µm containing facets partially connected and surrounded by organic material were observed in an intermediate stage of the spicule growth. Misorientation between these domains was approximately 2 ? , similar to the misorientation obtained by electron backscattered diffraction, indicating that the spicule is formed by the addition of granules fusing in a predominant orientation.