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Life's Possible Incubators: The Deep-Sea Hydrothermal Vent Hypothesis and the Freshwater Hot Spring Hypothesis

In recent years, research on the origin of life has increasingly converged with planetary science, prompting scientists to reassess whether different planetary bodies possess the necessary conditions for life to emerge. Life may not have arisen by chance in an obscure corner, but instead developed step by step under specific physicochemical conditions following fundamental processes. Therefore, understanding plausible scenarios for the origin of life is not only essential for reconstructing Earth's history, but also for improving the probability of detecting life on Mars, Europa, Enceladus, and even exoplanets.


Two leading hypotheses currently dominate discussions of life's origins, each focusing on fundamentally different environments: deep-sea hydrothermal vents and terrestrial freshwater hot springs. Although often portrayed as competing ideas, they actually address different stages of the origin process. The hydrothermal vent model emphasizes how chemical gradients and energy sources in deep oceans could generate the basic building blocks of life. In contrast, the hot spring model focuses on how these building blocks assemble into protocells capable of heredity and environmental selection.

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