Converging evidence from new top-down and bottom-up estimates of fossil “radiocarbon-free” methane emissions indicates that natural geologic sources account for a substantial component of the atmospheric methane budget. Comparing emission estimates based on atmospheric ¹⁴CH₄ (“radiomethane”) with geologic emissions from seepage, including terrestrial macroseeps, microseepage, marine seeps, and geothermal/volcanic emissions from the Earth's crust, shows that such “geo-CH₄” sources can be conservatively estimated at 53 ± 11 Tg yr⁻¹ globally. This makes geo-CH₄ second in importance to wetlands as a natural methane source. Such a new appraisal can easily be accommodated within the uncertainty of the global methane budget as recently compiled, and recognizes the importance of geophysical out-gassing of methane generated within the lithosphere. We propose a new coherent contemporary budget in which 30 ± 5% (based on atmospheric radiomethane measurements) of the global source of 582 ± 87 Tg yr⁻¹ has fossil origin, both natural and anthropogenic.