Carbon fluxes in the Canadian Arctic: patterns and drivers of bacterial abundance, production and respiration on the Beaufort Sea margin

14 pages, 6 figures, 5 tables During August 2009, measurements of bacterial abundance and nucleic acid content were made along with production and respiration in coastal waters of the Beaufort Sea (Arctic Ocean), an area influenced by the Mackenzie River inflow. The main purpose was to evaluate bact...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Ortega-Retuerta, E., Jeffrey, W.H., Babin, Marcel, Bélanger, S., Benner, R., Marie, Dominique, Matsuoka, A., Raimbault, P., Joux, Fabien
Format: Article in Journal/Newspaper
Language:English
Published: European Geosciences Union 2012
Subjects:
Arctic
Arctic Ocean
Mackenzie River
Beaufort Sea
Mackenzie river
Online Access:http://hdl.handle.net/10261/59983
https://doi.org/10.5194/bg-9-3679-2012
Description
Summary:14 pages, 6 figures, 5 tables During August 2009, measurements of bacterial abundance and nucleic acid content were made along with production and respiration in coastal waters of the Beaufort Sea (Arctic Ocean), an area influenced by the Mackenzie River inflow. The main purpose was to evaluate bacterial organic carbon processing with respect to local sources, mainly primary production and river inputs. Bacterial production and abundance generally decreased from river to offshore waters and from surface to deep waters. In contrast, the percentage of high nucleic acid bacteria was higher in deep waters rather than in surface or river waters. Statistical analyses indicated that bacterial production was primarily controlled by temperature and the availability of labile organic matter, as indicated by total dissolved amino acid concentrations. Direct comparisons of bacterial carbon demand and primary production indicated net heterotrophy was common in shelf waters. Net autotrophy was observed at stations in the Mackenzie River plume, suggesting that the carbon fixed in plume waters helped fuel net heterotrophy in the Beaufort Sea margin This work was supported by the French National Research Agency, under the grant no. ANR-BLAN08-1 310980 to the MALINA project, the LEFE-CYBER and CNES TOSCA programmes, and the European Space Agency. W.H.J was supported by a University of West Florida faculty scholarly and creative activity award. R. B. was supported by the US NSF (grant no 0713915) Peer reviewed

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