Articles | Volume 11, issue 13
Biogeosciences, 11, 3707–3719, 2014
https://doi.org/10.5194/bg-11-3707-2014
Biogeosciences, 11, 3707–3719, 2014
https://doi.org/10.5194/bg-11-3707-2014

Research article 15 Jul 2014

Research article | 15 Jul 2014

Revisiting the disappearance of terrestrial dissolved organic matter in the ocean: a δ13C study

K. Lalonde1, A. V. Vähätalo2,3, and Y. Gélinas1 K. Lalonde et al.
  • 1GEOTOP and Department of Chemistry and Biochemistry, Concordia University Montreal, Quebec, Canada
  • 2Department of Bio- and Environmental Science, University of Helsinki, Finland
  • 3present address: Department of Biological and Environmental Science, University of Jyväskylä, Finland

Abstract. Organic carbon (OC) depleted in 13C is a widely used tracer for terrestrial organic matter (OM) in aquatic systems. Photochemical reactions can, however, change δ13C of dissolved organic carbon (DOC) when chromophoric, aromatic-rich terrestrial OC is selectively mineralized. We assessed the robustness of the δ13C signature of DOC (δ13CDOC) as a tracer for terrestrial OM by estimating its change during the photobleaching of chromophoric DOM (CDOM) from 10 large rivers. These rivers cumulatively account for approximately one-third of the world's freshwater discharge to the global ocean. Photobleaching of CDOM by simulated solar radiation was associated with the photochemical mineralization of 16 to 43% of the DOC and, by preferentially removing compounds depleted in 13C, caused a 1 to 2.9‰ enrichment in δ13C in the residual DOC. Such solar-radiation-induced photochemical isotopic shift could bias the calculations of terrestrial OM discharge in coastal oceans towards the marine end-member. Shifts in terrestrial δ13CDOC should be taken into account when constraining the terrestrial end-member in global calculation of terrestrially derived DOM in the world ocean.

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