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Outgassing from Amazonian rivers and wetlands as a large tropical source of atmospheric CO2

Nature volume 416, pages 617–620 (2002)Cite this article

Abstract

Terrestrial ecosystems in the humid tropics play a potentially important but presently ambiguous role in the global carbon cycle. Whereas global estimates of atmospheric CO2 exchange indicate that the tropics are near equilibrium or are a source with respect to carbon1,2, ground-based estimates indicate that the amount of carbon that is being absorbed by mature rainforests is similar to or greater than that being released by tropical deforestation3,4 (about 1.6 Gt C yr-1). Estimates of the magnitude of carbon sequestration are uncertain, however, depending on whether they are derived from measurements of gas fluxes above forests5,6 or of biomass accumulation in vegetation and soils3,7. It is also possible that methodological errors may overestimate rates of carbon uptake or that other loss processes have yet to be identified3. Here we demonstrate that outgassing (evasion) of CO2 from rivers and wetlands of the central Amazon basin constitutes an important carbon loss process, equal to 1.2 ± 0.3 Mg C ha-1 yr-1. This carbon probably originates from organic matter transported from upland and flooded forests, which is then respired and outgassed downstream. Extrapolated across the entire basin, this flux—at 0.5 Gt C yr-1—is an order of magnitude greater than fluvial export of organic carbon to the ocean8. From these findings, we suggest that the overall carbon budget of rainforests, summed across terrestrial and aquatic environments, appears closer to being in balance than would be inferred from studies of uplands alone3,5,6.

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Figure 1: Flooded area of the central Amazon basin at high water, as mapped from the Japanese Earth Resources Satellite radar data (May–June 1996).
Figure 2: Spatially integrated annual sequences of surface water area for hydrographic environments as determined from JERS-1 radar data and multi-year hydrographic records.
Figure 3: Seasonal distributions of carbon dioxide dissolved in rivers of the central Amazon basin.
Figure 4: Spatially integrated sequences of monthly carbon dioxide evasion for the respective hydrographic environments (identified in Fig. 2).

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Acknowledgements

We thank E. Mayorga, S. Denning, M. Gastil, D. Montgomery, R. Victoria, A. Krusche, A. Devol, P. Quay and J. Hedges for technical assistance and discussions, B. Forsberg and T. Pimental for fieldwork, and the Global Rain Forest Mapping Project of the National Space Development Agency of Japan for providing the JERS-1 radar data. This work was supported by the US NSF and NASA EOS and LBA projects, and by the Brazilian FAPESP programme.

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Authors and Affiliations

  1. School of Oceanography, University of Washington, Seattle, 98195, Washington, USA

    Jeffrey E. Richey & Anthony K. Aufdenkampe

  2. Institute for Computational Earth System Science, University of California, Santa Barbara, 93106, California, USA

    John M. Melack & Laura L. Hess

  3. Centro de Energia Nuclear na Agricultura, Caixa Postal 96, Piracicaba SP, Brazil

    Victoria M. Ballester

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  1. Jeffrey E. Richey
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Correspondence to Jeffrey E. Richey.

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Richey, J., Melack, J., Aufdenkampe, A. et al. Outgassing from Amazonian rivers and wetlands as a large tropical source of atmospheric CO2. Nature 416, 617–620 (2002). https://doi.org/10.1038/416617a

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