4.8 Article

Hybrid organic-inorganic structures trigger the formation of primitive cell-like compartments

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NATL ACAD SCIENCES
DOI: 10.1073/pnas.2300491120

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origin of life; vesicles; inorganic mineral surfaces; surface chemistry; alkaline hydrothermal vents

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This paper investigates the features of alkaline hydrothermal vents and their significance in the origins of life. By integrating fatty alcohol decanol into inorganic minerals, novel three-dimensional structures were produced, and it has been demonstrated that the interaction between fatty alcohols and inorganic mineral structures may have played a crucial role in the formation of protocells.
Alkaline hydrothermal vents have become a candidate setting for the origins of life on Earth and beyond. This is due to several key features including the presence of gradients of temperature, redox potential, pH, the availability of inorganic minerals, and the existence of a network of inorganic pore spaces that could have served as primitive compartments. Chemical gardens have long been used as experimental proxies for hydrothermal vents. This paper investigates a set of prebiotic interactions between such inorganic structures and fatty alcohols. The integration of a medium-chain fatty alcohol, decanol, within these inorganic minerals, produced a range of emergent 3 dimensions structures at both macroscopic and microscopic scales. Fatty alcohols can be considered plausible prebiotic amphiphiles that might have assisted the formation of protocellular structures such as vesicles. The experiments presented herein show that neither chemical gardens nor decanol alone promote vesicle formation, but chemical gardens grown in the presence of decanol, which is then integrated into inorganic mineral structures, support vesicle formation. These observations suggest that the interaction of fatty alcohols and inorganic mineral structures could have played an important role in the emergence of protocells, yielding support for the evolution of living cells.

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