Silica is deposited in and around the spore coat layer of Bacillus cereus, and enhances the spore's acid resistance. Several peptides and proteins, including diatom silaffin and silacidin peptides, are involved in eukaryotic silica biomineralization (biosilicification). Homologous sequence search revealed a silacidin-like sequence in the C-terminal region of CotB1, a spore coat protein of B. cereus. The negatively charged silacidin-like sequence is followed by a positively charged arginine-rich sequence of 14 amino acids, which is remarkably similar to the silaffins. These sequences impart a zwitterionic character to the C terminus of CotB1. Interestingly, the cotB1 gene appears to form a bicistronic operon with its paralog, cotB2, the product of which, however, lacks the C-terminal zwitterionic sequence. A ⌬cotB1B2 mutant strain grew as fast and formed spores at the same rate as wild-type bacteria but did not show biosilicification. Complementation analysis showed that CotB1, but neither CotB2 nor C-terminally truncated mutants of CotB1, could restore the biosilicification activity in the ⌬cotB1B2 mutant, suggesting that the C-terminal zwitterionic sequence of CotB1 is essential for the process. We found that the kinetics of CotB1 expression, as well as its localization, correlated well with the time course of biosilicification and the location of the deposited silica. To our knowledge, this is the first report of a protein directly involved in prokaryotic biosilicification.
IMPORTANCEBiosilicification is the process by which organisms incorporate soluble silicate in the form of insoluble silica. Although the mechanisms underlying eukaryotic biosilicification have been intensively investigated, prokaryotic biosilicification was not studied until recently. We previously demonstrated that biosilicification occurs in Bacillus cereus and its close relatives, and that silica is deposited in and around a spore coat layer as a protective coating against acid. The present study reveals that a B. cereus spore coat protein, CotB1, which carried a C-terminal zwitterionic sequence, is essential for biosilicification. Our results provide the first insight into mechanisms required for biosilicification in prokaryotes.
Silicon (Si), the second most abundant element in the Earth's crust, is an important mineral for living organisms. It acts as the main component of structural skeletons of diatoms, radiolarians, and siliceous sponges (1). Si is also utilized by some plants (e.g., rice and cucumber) to protect against biotic and abiotic stresses (2). The presence of Si in bacterial spores was first noted several decades ago (3, 4). Until recently, however, there have been no reports on the precise localization of Si and its biological function in prokaryotes. In a recent study, we demonstrated that the Bacillus cereus group, a very homogenous cluster of six species, and its close relatives accumulate Si in and around their spore coat layer and that the Si-containing layer enhances acid resistance of the spores (5). In Si...