Methane formation driven by light and heat prior to the origin of life
Methane is a potent greenhouse gas, which likely enabled the evolution of life by keeping the early Earth warm. Here, we demonstrate new routes towards abiotic methane formation under early-earth conditions from methylated sulfur and nitrogen compounds with prebiotic origin. These compounds are demethylated in Fenton reactions governed by ferrous iron and reactive oxygen species, produced by light and heat in aqueous environments. The reactions generate methyl radicals and ultimately release methane and ethane. Organic iron chelators enhance reaction rates and recycle ferric to ferrous complexes via ligand-to-metal charge transfer, establishing a light-driven iron redox cycle. This abiotic reaction facilitates methane and ethane formation across Earths humid realm, thereby shaping the chemical evolution of the atmosphere prior to the origin of life and beyond. One-Sentence SummaryUnder suboxic and anoxic conditions, iron and reactive oxygen species drive the global formation of methane in aqueous environments.