Paleontology
The hydrothermal vent hypothesis proposes that life on Earth may have originated at hydrothermal vents on the ocean floor, where heated, mineral-rich water is expelled from the Earth's crust. This environment provides a unique set of conditions that could facilitate the formation of complex organic molecules, potentially leading to the emergence of the first living organisms. The hypothesis emphasizes the importance of chemical reactions driven by the vent's extreme conditions and suggests that these settings could be analogous to early Earth environments.
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