Abstract
The age of organic material discharged by rivers provides information about its sources and carbon cycling processes within watersheds. Although elevated ages in fluvially transported organic matter are usually explained by erosion of soils and sedimentary deposits1,2, it is commonly assumed that mainly young organic material is discharged from flat tropical watersheds due to their extensive plant cover and rapid carbon turnover3,4,5,6,7. Here we present compound-specific radiocarbon data of terrigenous organic fractions from a sedimentary archive offshore the Congo River, in conjunction with molecular markers for methane-producing land cover reflecting wetland extent. We find that the Congo River has been discharging aged organic matter for several thousand years, with apparently increasing ages from the mid- to the Late Holocene. This suggests that aged organic matter in modern samples is concealed by radiocarbon from atmospheric nuclear weapons testing. By comparison to indicators for past rainfall changes we detect a systematic control of organic matter sequestration and release by continental hydrology, mediating temporary carbon storage in wetlands. As aridification also leads to exposure and rapid remineralization of large amounts of previously stored labile organic matter, we infer that this process may cause a profound direct climate feedback that is at present underestimated in carbon cycle assessments.
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Acknowledgements
We thank J. M. Hayes, G. Mollenhauer, T. Goldhammer, M. Zabel, T. Wagner and M. Schulz for discussions. M. Luttmann, H. Buschhoff, D. Montluçon, F. Sidgwick, P. Green and S. Sylva are thanked for analytical support. We thank the staff at all involved radiocarbon dating facilities for their invaluable efforts. This study was supported by the Deutsche Forschungsgemeinschaft (grants SCHN 621/3-3, RU 458/29-3, GR 1845/2-3, SCHE 903/1), the US National Science Foundation (grant OCE-0137005), a Starting Grant from the European Research Council (ERC) awarded to H.M.T. for project AMOPROX (no. 258734) and grants ICM-NC120066 and FONDECYT1140536 to R.D.P.-H. This work was supported by the DFG Research Center/Cluster of Excellence ‘The Ocean in the Earth System’ at MARUM—Center for Marine Environmental Sciences, University of Bremen.
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E.S., T.I.E., J.R., P.M.G. and R.R.S. designed the study; analytical work was performed by E.S., C.L.S.-J., H.M.T., J.R., P.M.G. and R.D.P.-H.; E.S. wrote the manuscript, which was approved by all co-authors.
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Schefuß, E., Eglinton, T., Spencer-Jones, C. et al. Hydrologic control of carbon cycling and aged carbon discharge in the Congo River basin. Nature Geosci 9, 687–690 (2016). https://doi.org/10.1038/ngeo2778
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DOI: https://doi.org/10.1038/ngeo2778
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