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Generation of long-chain fatty acids by hydrogen-driven bicarbonate reduction in ancient alkaline hydrothermal vents

Chemistry

Generation of long-chain fatty acids by hydrogen-driven bicarbonate reduction in ancient alkaline hydrothermal vents

G. Purvis, L. Šiller, et al.

This groundbreaking study reveals how dissolved hydrogen and bicarbonate react with magnetite to produce vital long-chain aliphatic compounds, essential for the formation of early cell membranes. Conducted by Graham Purvis and colleagues at Newcastle University, this research opens up new insights into the origins of life and the potential pathways for the emergence of membrane-forming amphiphilic organic molecules.

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Playback language: English
Abstract
The origin of life required membrane-bound compartments. Long-chain amphiphilic molecules, such as fatty acids, are strong candidates for the first cell membranes, but their generation remains unclear. This study shows that the reaction of dissolved hydrogen and bicarbonate with magnetite under conditions of continuous flow, alkaline pH, and relatively low temperatures (90 °C) generates a range of functionalised long-chain aliphatic compounds, including mixed fatty acids up to 18 carbon atoms in length. This suggests that similar chemistry in bicarbonate-rich water mixing with alkaline hydrogen-rich fluids from serpentinization could have driven the generation of readily available membrane-forming amphiphilic organic molecules in early cellular life.
Publisher
Communications Earth & Environment
Published On
Jan 10, 2024
Authors
Graham Purvis, Lidija Šiller, Archie Crosskey, Jupiter Vincent, Corinne Wills, Jake Sheriff, Cijo Xavier, Jon Telling
Tags
origin of life
long-chain amphiphilic molecules
membrane formation
bicarbonate
serpentinization
hydrogen
fatty acids
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