The discovery of hydrothermal fields at ocean floor opens a new chapter for marine sciences. Fluids in hydrothermal fields are hot and acidic, where at least 400 different biological organisms have been detected, including shrimp, crab and bacteria. Such biological organisms are resistant to high temperature, acidic fluids, and high pressure, and they are dependent on energy and materials (hydrogen gas, methane, ethane and propane, and organic acids) provided by the interaction between basement rocks and seawater (i.e. serpentinization). Hydrothermal fields resemble the early history of Earth. Therefore, serpentinization potentially contributes to the origin and evolution of life.