Sponges (phylum Porifera) of the class of Demospongiae are stabilized by a siliceous skeleton. It is composed of silica needles (spicules), which provide the morphogenetic scaffold of these metazoans. In the center of the spicules there is an axial filament that consists predominantly of silicatein, an enzyme that catalyzes the synthesis of biosilica. By differential display of transcripts we identified additional proteins involved in silica formation. Two genes were isolated from the marine demosponge Suberites domuncula; one codes for a galectin and the other for a fibrillar collagen. The galectin forms aggregates to which silicatein molecules bind. The extent of the silicatein-mediated silica formation strongly increased if associated with the galectin. By applying a new and mild extraction procedure that avoids hydrogen fluoride treatment, native axial filaments were extracted from spicules of S. domuncula. These filaments contained, in addition to silicatein, the galectin and a few other proteins. Immunogold electron microscopic studies underscored the role of these additional proteins, in particular that of galectin, in spiculogenesis. Galectin, in addition to silicatein, presumably forms in the axial canal as well as on the surface of the spicules an organized net-like matrix. In the extraspicular space most of these complexes are arranged concentrically around the spicules. Taken together, these additional proteins, working together with silicatein, may also be relevant for potential (nano)-biotechnological applications of silicatein in the formation of surface coatings. Finally, we propose a scheme that outlines the matrix (galectin/silicatein)-guided appositional growth of spicules through centripetal and centrifugal synthesis and deposition of biosilica.The members of the phylum Porifera (sponges) are grouped according to their mineral skeleton into three classes: Hexactinellida and Demospongiae, which comprise a siliceous skeleton, and Calcarea, with calcareous skeletal materials (1). The elements constituting these skeletons are termed spicules; they are used as systematic characters for a given sponge species (2). Given the comprehensive studies of Bütschli (3) and Minchin (4), a descriptive view of the formation of the siliceous spicules has been well established. In demosponges, where most studies have been performed with Suberites domuncula, spicules are initially formed within specialized cells called sclerocytes (5). S. domuncula has the advantage of containing only macroscleres (tylostyles/oxeas), whereas most other sponges, e.g. Tethya aurantium, contain macroscleres (oxeas) as well as microscleres (spherasters) (6). Spicules have in their center a 1-2-m-wide axial canal (7), which contains the axial filament. In demosponges first siliceous deposits are arranged around this axial filament. When spicules reach lengths of about 10 m they are extruded from the cells. The spicules are completed extracellularly in the mesohyl (8), where they reach final sizes of 10 m (microscleres) and 200 m (mac...