Radiolytic H2 in continental crust: Nuclear power for deep subsurface microbial communities

Li Hung Lin, James Hall, Johanna Lippmann-Pipke, Julie A. Ward, Barbara Sherwood Lollar, Mary DeFlaun, Randi Rothmel, Duane Moser, Thomas M. Gihring, Bianca Mislowack, T. C. Onstott

Research output: Contribution to journalArticlepeer-review

171 Scopus citations


H2 is probably the most important substrate for terrestrial subsurface lithoautotrophic microbial communities. Abiotic H2 generation is an essential component of subsurface ecosystems truly independent of surface photosynthesis. Here we report that H2 concentrations in fracture water collected from deep siliclastic and volcanic rock units in the Witwatersrand Basin, South Africa, ranged up to two molar, a value far greater than observed in shallow aquifers or marine sediments. The high H2 concentrations are consistent with that predicted by radiolytic dissociation of H2O during radioactive decay of U, Th, and K in the host rock and the observed He concentrations. None of the other known H2-generating mechanisms can account for such high H2 abundance either because of the positive free energy imposed by the high H2 concentration or pH or because of the absence of required mineral phases. The radiolytic H 2 is consumed by methanogens and abiotic hydrocarbon synthesis. Our calculations indicate that radiolytic H2 production is a ubiquitous and virtually limitless source of energy for deep crustal chemolithoautotrophic ecosystems.

Original languageEnglish (US)
Article numberQ07003
JournalGeochemistry, Geophysics, Geosystems
Issue number7
StatePublished - Jul 2005

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology


  • Continental crust
  • Hydrogen
  • Radiolysis
  • Subsurface ecosystems


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