Miller and Urey conducted an experiment in 1953 to test the Oparin-Haldane theory that organic molecules could have formed on the early Earth. They placed water, methane, ammonia and hydrogen gases in an apparatus and provided electrical sparks as an energy source to simulate lightning. After one week, they detected amino acids such as glycine and alanine in the solution, supporting the idea that simple organic compounds could have been produced by chemical reactions in the early Earth's atmosphere.