The role of external ionic strength in diatom biosilica formation was assessed by monitoring the nanostructural changes in the biosilica of the two marine diatom species Thalassiosira punctigera and Thalassiosira weissflogii that was obtained from cultures grown at two distinct salinities. Using physicochemical methods, we found that at lower salinity the specific surface area, the fractal dimensions, and the size of mesopores present in the biosilica decreased. Diatom biosilica appears to be denser at the lower salinity that was applied. This phenomenon can be explained by assuming aggregation of smaller coalescing silica particles inside the silica deposition vesicle, which would be in line with principles in silica chemistry. Apparently, external ionic strength has an important effect on diatom biosilica formation, making it tempting to propose that uptake of silicic acid and other external ions may take place simultaneously. Uptake and transport of reactants in the proximity of the expanding silica deposition vesicle, by (macro)pinocytosis, are more likely than intracellular stabilization and transport of silica precursors at the high concentrations that are necessary for the formation of the siliceous frustule components.biosilica ͉ silica nanostructure ͉ silicification ͉ silica chemistry D iatoms are known for the intriguing species-specific morphology of their siliceous exoskeletons, the frustules (1, 2), which consist of two silica valves (the epi-and hypovalve), siliceous girdle bands, and a protective organic casing that prevents dissolution of the siliceous parts in the aquatic environment. During cell division, a parental diatom cell undergoes cytokinesis, and each of the next two daughter cells produces a new hypovalve, a hypocingulum, and girdle band(s); the sequence of their formation differs among species (1, 2). After valve and girdle band completion, the daughter cells finally separate, and cell division continues. The silica of every new valve is formed in the silica deposition vesicle (SDV) that is located inside each daughter cell and is closely appressed to the plasma membrane along the cleavage furrow. The SDV rapidly expands two-dimensionally and subsequently thickens more slowly in the three-dimensional direction during formation of the new hypovalve (3, 4). In the course of this fast two-dimensional expansion process, the essential reactants for silica polymerization have to be transported efficiently to the SDV. Silicon transporters have been identified (5, 6), but there is no clear evidence that they transport sufficient amounts of silicic acid across the plasma membrane and/or SDV membrane to enable silica polymerization.In diatoms, both organic and inorganic compounds foster silica biomineralization and possibly control silica precipitation and direct the structures formed (7-9). Relevant organic compounds are silica-precipitating peptides such as silaffins and long-chain polyamines (8-10). They all have an intracellular origin and require specific targeting or intracellular transpo...