Biogeochemistry of Carbon in the Amazonian Floodplains over a 2000-km Reach: Insights from a Process-Based Model

Autor(es)

Bustillo, Vincent ^{[1, 2]} ; Victoria, Reynaldo Luiz ^{[1, 3]} ; Sousa de Moura, Jose Mauro ^[4] ; Victoria, Daniel de Castro ^[5] ; Andrade Toledo, Andre Marcondes ^[6] ; Colicchio, Erich ^[7]

Afiliação do(s) autor(es)

^[1] Ctr Energia Nucl Agr, Lab Geoprocessamento & Tratamento Imagens, Piracicaba - Brazil

^[2] Univ Orleans, Univ Tours, Inst Sci Terre Orleans, CNRS, INSU, UMR 6113, F-37200 Tours - France

^[3] USP ESALQ, NUPEGEL, Piracicaba - Brazil

^[4] Univ Fed Oeste Para, Santarem - Brazil

^[5] Embrapa Monitoramento Satelite, Campinas - Brazil

^[6] Univ Fed Mato Grosso, Rondonopolis - Brazil

^[7] Univ Fed Tocantins, AgroUnitins, Palmas - Barbados

• Tipo de documento: Artigo Científico
• Fonte: Earth Interactions; v. 15, JAN 2011.
• Citações Web of Science: 2

Resumo

The influence of Amazonian floodplains on the hydrological, sedimentary, and biogeochemical river budget was investigated over a 2000-km reach. A process-based model relying on the closure of chemical fluxes and isotopic signals was implemented. On average for the whole studied reach, the overall fluxes of carbon associated with mineralization and aquatic photosynthesis were estimated to 35.7 and 15.3 Tg C yr(-1), respectively. Almost 57% of the carbon sequestrated by photosynthesis comes from aerial sources (flooded forest); the remaining 43% resulted from aquatic sources (varzea grasses and phytoplankton). The process rates substantially fluctuate over the annual cycle, depending particularly on the extension of flooded area and on the river-floodplain connectivity. As the river level declines, the drastic decrease of turbidity and the lower supply of carbon substrates promote autotrophy to the detriment of heterotrophy, leading to substantial changes of pH and gaseous equilibria in the river water. The main consequences are (i) the side-chain oxidation of dissolved organic matter leading to the concomitant rises of the carbon to nitrogen atomic ratio and nitrate contents and (ii) the sorption of hydrophobic humic acids, which fractionate (13)C and thus lead to (13)C-depleted particulate organic matter (fine fraction) compared to remaining dissolved organic matter. As the river flow rises, the heterotrophy prevails over autotrophy and this tends to attenuate the chemical signature imprinted by the latter. The significant contribution of aerial autochthonous sources to the budget of carbon indicates that the fluxes of mineralization are sustained by the net primary production of river corridors. The variable extension of submerged areas defines the proportions of CO(2) exported by the river and released to the atmosphere. The rate of CO(2) outgassing on the studied reach (18.8 Tg C yr(-1)) represents about 50% of the incoming dissolved inorganic carbon flux. The rate of methane emission is estimated as 2.2 Tg C yr(-1) and that of denitrification is estimated as 0.87 Tg N yr(-1), representing 1.5 times the flux of dissolved inorganic nitrogen (DIN) exported by the Amazon River at the station of Obidos (0.64 Tg N yr(-1)). (AU)

• Processo FAPESP: 05/58884-5 - Um modelo sintético de larga escala aplicado à hidroclimatologia e à ecogeodinâmica da Bacia do Rio Amazonas
• Beneficiário: Vincent Bustillo
• Modalidade de apoio: Bolsas no Brasil - Pós-Doutorado