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Abstract
The siliceous skeletal elements of the sponges, the spicules, represent one of the very few examples from where the molecule toolkit required for the formation of an extracellular mineral-based skeleton, has been elucidated. The distinguished feature of the inorganic matrix, the bio-silica, is its enzymatic synthesis mediated by silicatein. Ortho-silicate undergoes in the presence of silicatein a polycondensation reaction and forms bio-silica under release of reaction water. The protein silicatein aggregates non-covalently to larger filaments, a process that is stabilized by the silicatein-associated protein, silintaphin-1. These structured clusters form the axial filament that is located in the center of the spicules, the axial canal. Surprisingly it has now been found that the initial axial orientation, in which the spicules grow, is guided by cell processes through evagination. The approximately two µm wide cell extensions release silicatein that forms the first organic axial filament, which then synthesizes the inner core of the siliceous spicule rods. In parallel, the radial growth of the spicules is controlled by a telescopic arrangement of organic layers, into which bio-silica and ortho-silicate are deposited. Hence, the formation of a mature siliceous spicule is completed by a centrifugal accretion of bio-silica mediated by the silicatein in the axial filament, and a centripetal bio-silica deposition catalyzed by the extra-spicular silicatein. Finally this contribution highlights that for the ultimate determination of the spicule shapes, their species-specific morphologies, bio-silica hardens during a process which removes reaction water. The data presented can also provide new blueprints for the fabrication of novel biomaterials for biomedical applications.