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- Atribacteria from the Subseafloor Sedimentary Biosphere Disperse to the Hydrosphere through Submarine Mud Volcanoes. Frontiers in Microbiology. 8:1135.
- Biological CO2 conversion to acetate in subsurface coal-sand formation using a high-pressure reactor system. Frontiers in Microbiology. 4.
- Cultivable microbial community in 2-km-deep, 20-million-year-old subseafloor coalbeds through ~1000 days anaerobic bioreactor cultivation. Scientific Reports. 9.
- Deep-biosphere methane production stimulated by geofluids in the Nankai accretionary complex. Science Advances. 4:eaao4631.
- Exploring deep microbial life in coal-bearing sediment down to ~2.5 km below the ocean floor. Science. 349:420-424.
- Increase in acetate concentrations during sediment sample onboard storage: a caution for pore-water geochemical analyses. Geochemical Journal. 47:567-571.
- Low-Temperature Clay Mineral Dehydration Contributes to Porewater Dilution in Bering Sea Slope Subseafloor. Frontiers in Earth Science. 6:36.
- Methyl-compound use and slow growth characterize microbial life in 2-km-deep subseafloor coal and shale beds. Proceedings of the National Academy of Sciences. 114:E9206-E9215.
- Origins of lithium in submarine mud volcano fluid in the Nankai accretionary wedge. Earth and Planetary Science Letters. 414:144-155.