1. Ancient Life: Millions of years ago, microscopic organisms lived in the ocean. When they died, their bodies settled to the seafloor and were buried under layers of sediment.
2. Heat and Pressure: Over time, these sediment layers became thicker and heavier, creating enormous pressure. At the same time, Earth's internal heat increased the temperature.
3. Transformation: Under this intense heat and pressure, the organic matter in the dead organisms underwent a series of chemical transformations. This process, called diagenesis, breaks down the complex molecules of the organisms into simpler hydrocarbons, which are the main components of oil and natural gas.
4. Migration and Trapping: The hydrocarbons, lighter than the surrounding rock, migrated upwards. They were eventually trapped underground in porous rock formations, often capped by impermeable rock layers that prevent them from escaping.
In essence, oil is the fossilized remains of ancient life, transformed by geological processes over millions of years.