δ13C tracing of dissolved inorganic carbon sources in Patagonian rivers (Argentina)

Authors

  • F. Brunet,

    1. Laboratoire des Mécanismes de Transfert en Géologie (LMTG), UMR no. 5563 CNRS–IRD–Université Paul Sabatier, 14 avenue Edouard Belin, Toulouse 31400, France
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  • D. Gaiero,

    1. Centro de Investigaciones Geoquímicas y de Procesos de la Superficie (CIGeS), FCEFyN, Universidad Nacional de Córdoba, Avenida Vélez Sarsfield 1611, X5016GCA Córdoba, Argentina
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  • J. L. Probst,

    Corresponding author
    1. Laboratoire des Mécanismes de Transfert en Géologie (LMTG), UMR no. 5563 CNRS–IRD–Université Paul Sabatier, 14 avenue Edouard Belin, Toulouse 31400, France
    • INPT, ENSAT–Agronomie Environnement Ecotoxicologie, EA no. 3715, av. de l'Agrobiopole, BP 32607, Auzeville Tolosane, 31326 Castanet Tolosan Cedex, France.
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  • P. J. Depetris,

    1. Centro de Investigaciones Geoquímicas y de Procesos de la Superficie (CIGeS), FCEFyN, Universidad Nacional de Córdoba, Avenida Vélez Sarsfield 1611, X5016GCA Córdoba, Argentina
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  • F. Gauthier Lafaye,

    1. Centre de Géochimie de la Surface (CGS), UMR no. 7517 CNRS–Université Louis Pasteur, 1 rue Blessig, 67084 Strasbourg Cedex, France
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  • P. Stille

    1. Centre de Géochimie de la Surface (CGS), UMR no. 7517 CNRS–Université Louis Pasteur, 1 rue Blessig, 67084 Strasbourg Cedex, France
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Abstract

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 δ13C isotopic signature. The δ13CDIC values vary between −12·8 and −1·8‰ 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, δ13CDIC 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, δ13CDIC also appears to be controlled by the oxidation of organic carbon, showing a negative relationship between δ13CDIC 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 δ13CDIC alone to distinguish these contributions.

The annual DIC flux exported by Patagonian Rivers to the South Atlantic Ocean averages 621 × 109 g. of C, i.e. a specific yield of 2·7 g m−2 year−1. The mean δ13CDIC can be estimated to − 4·9‰, which is high compared with other rivers of the world. Copyright © 2005 John Wiley & Sons, Ltd.

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