Heterotrophic bacterial production in the eastern South Pacific: Longitudinal trends and coupling with primary production

F. Van Wambeke, I. Obernosterer, T. Moutin, S. Duhamel, O. Ulloa, H. Claustre

Research output: Contribution to journalArticlepeer-review

26 Scopus citations


Spatial variation of heterotrophic bacterial production and phytoplankton primary production were investigated across the eastern South Pacific Ocean (-141° W, -8° S to -72° W, -35° S) in November-December 2004. Bacterial production (3H leucine incorporation) integrated over the euphotic zone encompassed a wide range of values, from 43mg C m -2d-1 in the hyper-oligotrophic South Pacific Gyre to 392 mg C m-2 d-1 in the upwelling off Chile. In the gyre (120° W, 22° S) records of low phytoplankton biomass (7mg Total Chla m-2) were obtained and fluxes of in situ 14C-based particulate primary production were as low as 153 mgC m-2 d -1, thus equal to the value considered as a limit for primary production under strong oligotrophic conditions. Average rates of 3H leucine incorporation rates, and leucine incorporation rates per cell (5-21 Pmol 1-1 h-1 and 15-56×l0-21 mol cell -1 h-1, respectively) determined in the South Pacific gyre, were in the same range as those reported for other oligotrophic subtropical and temperate waters. Fluxes of dark community respiration, determined at selected stations across the transect varied in a narrow range (42-97 mmol O2 m-2 d-1), except for one station in the upwelling off Chile (245 mmol O2 m-2 d -1). Bacterial growth efficiencies varied between 5 and 38%. Bacterial carbon demand largely exceeded 14C particulate primary production across the South Pacific Ocean, but was lower or equal to gross community production.

Original languageEnglish (US)
Pages (from-to)157-169
Number of pages13
Issue number1
StatePublished - 2008
Externally publishedYes

ASJC Scopus subject areas

  • Ecology, Evolution, Behavior and Systematics
  • Earth-Surface Processes


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