The inorganic carbon carried in rivers of the Amazon basin seems to originate largely from the decomposition of young plant material — a finding that improves our understanding of the role of rivers in the carbon cycle.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Mayorga, E. et al. Nature 436, 538–541 (2005).
Houghton, R. A., Lawrence, K. T., Hackler, J. L. & Brown, S. Glob. Change Biol. 7, 731 (2001).
Richey, J. E., Melack, J. M., Aufdenkampe, A. K., Ballester, V. M. & Hess, L. L. Nature 416, 617–620 (2002).
Cole, J. J. & Caraco, N. F. Mar. Freshwat. Res. 52, 101–110 (2001).
Raymond, P. A. & Bauer, J. E. Org. Geochem. 32, 469–485 (2001).
Blair, N. E. et al. Geochim. Cosmochim. Acta 67, 63–73 (2003).
Kao, S. & Liu, K. Limnol. Oceanogr. 41, 1749–1757 (1996).
Masiello, C. A. & Druffel, E. R. M. Glob. Biogeochem. Cycles 15, 407–416 (2001).
Raymond, P. A. et al. Mar. Chem. 92, 353–366 (2004).
Blair, N. E. et al. Mar. Chem. 92, 141 (2004).
Druffel, E. R. M., Bauer, J. E. & Griffin, S. Geochem. Geophys. Geosyst. 6, Q03009 (2005).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Raymond, P. The age of the Amazon's breath. Nature 436, 469–470 (2005). https://doi.org/10.1038/436469a
Published:
Issue Date:
DOI: https://doi.org/10.1038/436469a