The effects of silicic acid on the growth of Thermus thermophilus TMY, an extreme thermophile isolated from a siliceous deposit formed from geothermal water at a geothermal power plant in Japan, were examined at 75°C. At concentrations higher than the solubility of amorphous silica (400 to 700 ppm SiO 2 ), a silica-induced protein (Sip) was isolated from the cell envelope fraction of log-phase TMY cells grown in the presence of supersaturated silicic acid. Two-dimensional sodium dodecyl sulfate-polyacrylamide gel electrophoresis revealed the molecular mass and pI of Sip to be about 35 kDa and 9.5, respectively. Induction of Sip expression occurred within 1 h after the addition of a supersaturating concentration of silicic acid to TM broth. Expression of Sip-like proteins was also observed in other thermophiles, including T. thermophilus HB8 and Thermus aquaticus YT-1. The amino acid sequence of Sip was similar to that of the predicted solute-binding protein of the Fe 3؉ ABC transporter in T. thermophilus HB8 (locus tag, TTHA1628; GenBank accession no. NC_006461; GeneID, 3169376). The sip gene (987-bp) product showed 87% identity with the TTHA1628 product and the presumed Fe 3؉ -binding protein of T. thermophilus HB27 (locus tag TTC1264; GenBank accession no. NC_005835; GeneID, 2774619). Within the genome, sip is situated as a component of the Fbp-type ABC transporter operon, which contains a palindromic structure immediately downstream of sip. This structure is conserved in other T. thermophilus genomes and may function as a terminator that causes definitive Sip expression in response to silica stress.Occurring mainly in the form of silica (SiO 2 ), silicon (Si) is the second-most abundant element in the earth's crust, accounting for 28.8% of the earth's mass (34). SiO 2 exists as monosilicic acid (Si(OH) 4 ) in aqueous solution, as represented in the following equation: SiO 2 ϩ 2H 2 O · (Si(OH) 4 ). The solubility of silica greatly depends on temperature, pH (17), and salt concentration, among other parameters (27). As the temperature of a silicic acid solution declines, its concentration can exceed the solubility of amorphous silica. Under those conditions, silicic acid polymerizes to form polysilisic acid, which is relatively stable in aqueous solution because the repulsion between the negative charges on its surface keeps it from readily aggregating and precipitating. In a geothermal reservoir, at high temperature and pressure, the silicic acid concentration at equilibrium shows the solubility of quartz. However, when that geothermal water is discharged to the surface, the silicic acid concentration becomes supersaturated as the water boils, frequently leading to the formation of siliceous deposits called "silica sinter" (11). Microscopic observation of such siliceous deposits reveals many microbe-like structures (20), and it has been suggested that these fossils represent archean microorganisms that grew in the hot, supersaturated fluids (26). There have been a number of experimental studies carried out wit...