4.5 Article

Landscape Control on the Spatial and Temporal Variability of Chromophoric Dissolved Organic Matter and Dissolved Organic Carbon in Large African Rivers

Journal

ECOSYSTEMS
Volume 18, Issue 7, Pages 1224-1239

Publisher

SPRINGER
DOI: 10.1007/s10021-015-9894-5

Keywords

Carbon cycle; Colored dissolved organic matter; Tropical rivers; Land cover; Landscape; Carbon isotopes

Categories

Funding

  1. European Research Council [ERC-StG 240002]
  2. Fonds National de la Recherche Scientifique (FRNS) [14711103]
  3. Research Foundation Flanders (FWO-Vlaanderen)
  4. Belgian Federal Science Policy (BELSPO-SSD project COBAFISH)
  5. Arctic Great Rivers Observatory [NSF-0732522, NSF-1107774]

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The characteristics of colored dissolved organic matter (CDOM) as well as the concentrations and stable isotope composition (delta C-13) of dissolved organic carbon (DOC) were characterized in several large rivers of Africa including the Congo, Niger, Zambezi, and Ogoou, basins. We compared the spatial and temporal patterns of dissolved organic matter (DOM) quantity and quality along with various environmental gradients, including hydrology, river size, catchment vegetation, and connectivity to land. The optical proxies used include the absorption coefficient at 350 nm, the specific ultra-violet absorbance, and the spectral slope ratio (S (R) = 275-295-nm slope divided by 350-400-nm slope). Our results show that land cover plays a primary role in controlling both DOC concentration and optical properties of DOM in tropical freshwaters. A higher cover of dense forest in the catchment leads to a higher quantity of highly aromatic DOM in the river network, whereas an increasing savannah cover results in lower DOC concentrations and less absorptive DOM. In addition to land cover, the watershed morphology (expressed by the average slope) exerts a strong control on DOC and CDOM in tropical rivers. Our results also show that the percentage of C3 and C4 vegetation cover is not an accurate predictor for DOM and CDOM quality in rivers due to the importance of the spatial distribution of land cover within the drainage network. The comparison of our results with previously published CDOM data in temperate and high-latitude rivers highlights that DOM in tropical freshwaters is generally more aromatic, and shows a higher capacity for absorbing sunlight irradiance.

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