Millennial-aged peat carbon outgassed by large humic lakes in the Congo Basin

Drake, Travis W.;Hemingway, Jordon D.;Barthel, Matti;de Clippele, Antoine;Six, Johan;et.al.
(2026) Nature Geoscience — p. 10 (2026)

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Authors
  • Drake, Travis W.orcid-logoDepartment of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
    Author
  • Hemingway, Jordon D.orcid-logoGeological Institute, Department of Earth and Planetary Sciences, ETH Zurich, Zurich, Switzerland
    Author
  • Barthel, Mattiorcid-logoDepartment of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
    Author
  • de Clippele, Antoineorcid-logoDepartment of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
    Author
  • Author
  • Six, Johanorcid-logoDepartment of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
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Abstract
Congo Basin lakes Mai Ndombe and Tumba are major CO2 sources. Here we show that their dissolved inorganic carbon is some 2,170–3,515 14C years old and partially (39–40%) originates from the surrounding peatlands. This implies a loss pathway for peat carbon, in which microbes respire old carbon within the peat and the resulting CO2 is transported to the lakes and outgassed, linking these immense ancient stores to the modern carbon cycle.
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Citations

Drake, T. W., Hemingway, J. D., Barthel, M., de Clippele, A., Haghipour, N., Wabakanghanzi, J. N., Van Oost, K., & Six, J. (2026). Millennial-aged peat carbon outgassed by large humic lakes in the Congo Basin. Nature Geoscience, 10. https://doi.org/10.1038/s41561-026-01924-3 (Original work published 2026)