Life on Earth began through a process known as abiogenesis, which refers to the natural origin of life from nonliving simple molecules. This theory posits that life emerged in Earth's oceans approximately 3.8 billion years ago. The foundational elements for this process were prebiotic molecules, which were abundant on early Earth, including hydrogen gas, water, ammonia, carbon dioxide, and methane.
The transition from these non-biological molecules to the first biomolecules is explained by several theories. One prominent theory is the atmospheric conversion theory, which suggests that energy from the sun and lightning facilitated the transformation of prebiotics into simple biomolecules. Alternatively, the hydrothermal vents theory proposes that biomolecules formed in the depths of the ocean, where sunlight and lightning could not reach, with hydrothermal vents providing the necessary energy for this conversion.
To illustrate this process, consider the formation of biomolecule monomers, such as amino acids. In the first theory, solar radiation and lightning act as catalysts to convert prebiotic materials into these monomers. In contrast, the second theory emphasizes the role of hydrothermal vents in generating the energy required for this transformation in environments shielded from sunlight.
While both theories have substantial experimental support, the exact mechanism of how the first biomolecule monomers were formed remains uncertain. However, it is clear that these monomers were crucial in the development of more complex biomolecules, setting the stage for the evolution of life. Future discussions will delve into how these initial biomolecule monomers combined to form the first biomolecule polymers.