Natural radioactive environments as sources of local disequilibrium for the emergence of life
Thiago Altair, Larissa M. Sartori, Fabio Rodrigues, Marcio G. B. de, Avellar, Douglas Galante

TL;DR
This paper explores how natural radioactive environments on early Earth could have generated chemical disequilibrium through water radiolysis, potentially providing energy sources and conditions conducive to the emergence of life, similar to alkaline hydrothermal systems.
Contribution
It introduces a kinetic model analyzing water radiolysis effects in natural radioactive environments, linking them to conditions favorable for life's emergence on early Earth.
Findings
Water radiolysis can produce chemical disequilibrium similar to alkaline hydrothermal vents.
The model shows a steady increase in pH, promoting mineral precipitation and catalytic activity.
Natural electrochemical gradients could have supported proto-metabolic processes.
Abstract
Certain subterranean environments of Earth have naturally accumulated long-lived radionuclides, such as 238U, 232Th and 40K, near the presence of liquid water. In these natural radioactive environments (NRE), water radiolysis can produce chemical species of biological importance, such as H2. Although the proposal of radioactive decay as an alternative source of energy for living systems has existed for more than thirty years, this hypothesis gained strength after the recent discovery of a peculiar ecosystem in a gold mine in South Africa, whose existence is dependent on chemical species produced by water radiolysis. In this work, we calculate the chemical disequilibrium generated locally by water radiolysis due gamma radiation and analyse the possible contribution of this disequilibrium for the emergence of life, considering conditions of early Earth and having as reference the alkaline…
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