This audiobook is narrated by a digital voice.

Understanding the origins of life on Earth provides the foundational framework for the search for life elsewhere in the universe. Scientists believe that life began approximately 3.5 to 4 billion years ago, during a time when the planet was vastly different from today. The early Earth was a volatile environment, with high temperatures, volcanic activity, and a primitive atmosphere composed mainly of water vapor, carbon dioxide, nitrogen, and trace gases. These harsh conditions may have actually set the stage for the chemical reactions that led to life.

At the heart of this inquiry lies the study of the basic building blocks of life: organic molecules such as amino acids, nucleotides, and lipids. These compounds can form under a variety of conditions and have been created in laboratory experiments simulating early Earth's environment, such as the famous Miller-Urey experiment in 1953. This experiment demonstrated that, with the right energy input, simple chemicals can produce more complex organic molecules. These early compounds may have accumulated in Earth's primordial oceans, creating a "soup" of chemicals from which life gradually emerged.

The next step in this process was the development of self-replicating molecules, most likely RNA, which is capable of both storing genetic information and catalyzing chemical reactions. This stage marked the beginning of biological evolution, where natural selection began to favor more efficient and stable forms of molecular organization. Over time, these molecules may have become enclosed within lipid membranes, forming primitive cells known as protocells. These protocells were likely the ancestors of all modern life.