Titre du document / Document title
Amazon River enhances diazotrophy and carbon sequestration in the tropical North Atlantic Ocean
Auteur(s) / Author(s)SUBRAMANIAM A.
YAGER P. L.
CARPENTER E. J.
KUSTKA A. B.
MONTOYA J. P.
SANUDO-WILHELMY S. A.
CAPONE D. G.
Résumé / Abstract
The fresh water discharged by large rivers such as the Amazon is transported hundreds to thousands of kilometers away from the coast by surface plumes. The nutrients delivered by these river plumes contribute to enhanced primary production in the ocean, and the sinking flux of this new production results in carbon sequestration. Here, we report that the Amazon River plume supports N2
fixation far from the mouth and provides important pathways for sequestration of atmospheric CO2
in the western tropical North Atlantic (WTNA). We calculate that the sinking of carbon fixed by diazotrophs in the plume sequesters 1.7 Tmol of C annually, in addition to the sequestration of 0.6 Tmol of C yr-1
of the new production supported by NO3
delivered by the river. These processes revise our current understanding that the tropical North Atlantic is a source of 2.5 Tmol of C to the atmosphere [Mikaloff-Fletcher SE, et a/. (2007) Inverse estimates of the oceanic sources and sinks of natural CO2
and the implied oceanic carbon transport. Global Biogeochem Cycles 21, doi:10.1029/2006GB002751]. The enhancement of N2
fixation and consequent C sequestration by tropical rivers appears to be a global phenomenon that is likely to be influenced by anthropogenic activity and climate change.
Revue / Journal TitleProceedings of the National Academy of Sciences of the United States of America
Source / Source
2008, vol. 105, no
30, pp. 10460-10465 [6 page(s) (article)]
Langue / Language
Editeur / Publisher
National Academy of Sciences, Washington, DC, ETATS-UNIS
Localisation / Location
INIST-CNRS, Cote INIST : 574, 35400019644666.0350
Nº notice refdoc (ud4) : 20548900