Abstract
Thermophiles are microorganisms that can grow at temperatures higher than 50 or 60°C. There are thermophilic eubacteria and thermophilic archaebacteria. Thermophilic microorganisms can be found geothermally and hydrothermally active area. The water penetrates into deep subsurface around thermal area and reacts with hot basalt. Some of the compounds in the water are reduced by the reaction. The water returned to the surface and reacts with seawater or air, depending on the location of the thermal area. Many types of autotrophes and heterotrophes were found near thermally active area. The microorganisms form the ecosystem based on the redox chemical reactions. All of the structural elements in thermophilic microorganisms are thermophilic or thermostable. Proteins found in microorganisms are thermostable. Though several common characteristics can be found in thermostable proteins, it is not easy to attribute the stability to specific amino acid residues. DNA in thermophiles is stabilized by increasing the G+C content or by histone-like DNA binding proteins. There are several molecular biological and geological evidences to support the relation between ancient life forms and thermal activity on the Earth. Thermophiles of different life forms may be found in thermally active area, in such as those that may be present in satellites of Jupiter.
