d13C tracing of dissolved inorganic carbon sources in Patagonian rivers (Argentina)

• Published in: Hydrological Processes
• Main Authors: Brunet, Frédéric, Gaiero, Diego M., Probst, Jean-Luc, Depetris, Pedro J., Gauthier-Lafaye, François, Stille, Peter
• Other Authors: Universidad Nacional de Cordoba - UNC (ARGENTINA), Institut National Polytechnique de Toulouse - INPT (FRANCE), Institut de Recherche pour le Développement - IRD (FRANCE), Université Toulouse III - Paul Sabatier - UPS (FRANCE), Centre National de la Recherche Scientifique - CNRS (FRANCE), Université Louis Pasteur-Strasbourg I - ULP (FRANCE)
• Format: Article in Journal/Newspaper
• Language: English
• Published: John Wiley & Sons 2005
• Subjects: Géochimie; Dissolved inorganic carbon; Flux; Patagonia; River; Isotopic signature; Tracing; Dissolved organic carbon; Strontium isotopes; Rock weathering; Atmospheric CO2; Biospheric CO2; Argentina; Chubut; Gallegos; South Atlantic Ocean
• Online Access: http://oatao.univ-toulouse.fr/3408/; http://oatao.univ-toulouse.fr/3408/1/Brunet_3408.pdf; https://doi.org/10.1002/hyp.5973

The main Patagonian rivers (Colorado, Negro, Chubut, Deseado, Coyle, Chico, Santa Cruz and Gallegos) were sampled between September 1995 and November 1998 to determine their chemical and isotopic compositions, the origins of the suspended and dissolved river loads and their inputs to the South Atlantic Ocean. This paper focuses on the dissolved inorganic carbon (DIC) transport and its υ13C isotopic signature. The υ13CDIC values vary between 12Ð8 and 1Ð8‰ and allow one to distinguish two river groups: (i) the Colorado, Negro, Chubut and Santa Cruz, which display the highest values and the lowest seasonal variations; (ii) the Deseado, Coyle, Chico and Gallegos, which show the lowest values and the highest seasonal variations. For the first group, υ13CDIC is mainly controlled by important exchanges between the river waters and atmospheric CO2, due to the presence of lakes and dams. For the second group, υ13CDIC also appears to be controlled by the oxidation of organic carbon, showing a negative relationship between υ13CDIC and the dissolved organic carbon. These biogeochemical processes interfere with the contribution of carbonate and silicate weathering to the riverine DIC and do not allow use of υ13CDIC alone to distinguish these contributions. The annual DIC flux exported by Patagonian Rivers to the South Atlantic Ocean averages 621 ð 109 g. of C, i.e. a specific yield of 2Ð7 g m2 year1. The mean υ13CDIC can be estimated to 4Ð9‰, which is high compared with other rivers of the world.