Articles | Volume 23, issue 5
https://doi.org/10.5194/bg-23-1755-2026
https://doi.org/10.5194/bg-23-1755-2026
Research article
 | 
04 Mar 2026
Research article |  | 04 Mar 2026

Tropical wet season runoff mobilises younger carbon in rainforest streams but older carbon in agricultural streams

Clément Duvert, Vanessa Solano, Dioni I. Cendón, Francesco Ulloa-Cedamanos, Liza K. McDonough, Robert G. M. Spencer, Niels C. Munksgaard, Lindsay B. Hutley, Jean-Sébastien Moquet, and David E. Butman

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Cited articles

Aiken, G. R., Spencer, R. G. M., Striegl, R. G., Schuster, P. F., and Raymond, P. A.: Influences of glacier melt and permafrost thaw on the age of dissolved organic carbon in the Yukon River basin, Global Biogeochem. Cy., 28, 525–537, https://doi.org/10.1002/2013GB004764, 2014. 
Barnes, R. T., Butman, D. E., Wilson, H., and Raymond, P. A.: Riverine export of aged carbon driven by flow path depth and residence time, Environ. Sci. Technol., 52, 1028–1035, https://doi.org/10.1021/acs.est.7b04717, 2018. 
Battin, T. J., Lauerwald, R., Bernhardt, E. S., Bertuzzo, E., Gener, L. G., Hall, R. O., Hotchkiss, E. R., Maavara, T., Pavelsky, T. M., Ran, L., Raymond, P., Rosentreter, J. A., and Regnier, P.: River ecosystem metabolism and carbon biogeochemistry in a changing world, Nature, 613, 449–459, https://doi.org/10.1038/s41586-022-05500-8, 2023. 
Beck, H. E., McVicar, T. R., Vergopolan, N., Berg, A., Lutsko, N. J., Dufour, A., Zeng, Z., Jiang, X., van Dijk, A. I. J. M., and Miralles, D. G.: High-resolution (1 km) Köppen-Geiger maps for 1901–2099 based on constrained CMIP6 projections, Sci. Data, 10, 724, https://doi.org/10.1038/s41597-023-02549-6, 2023. 
Behnke, M. I., Fellman, J. B., D'Amore, D. V., Gomez, S. M., and Spencer, R. G. M.: From canopy to consumer: what makes and modifies terrestrial DOM in a temperate forest, Biogeochemistry, 164, 185–205, https://doi.org/10.1007/s10533-022-00906-y, 2023. 
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Short summary
This study examines the age and composition of carbon in tropical streams. We find that dissolved organic carbon (DOC) is centuries to millennia old, while dissolved inorganic carbon (DIC) is consistently younger, indicating a decoupling between the two. DOC age varies seasonally, with rainforest streams exporting younger DOC during high flow, while agricultural streams mobilise older DOC. Our results suggest land conversion alters carbon export, potentially worsening with climate change.
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