Articles | Volume 11, issue 22
Biogeosciences, 11, 6377–6387, 2014
Biogeosciences, 11, 6377–6387, 2014

Research article 26 Nov 2014

Research article | 26 Nov 2014

The percentage of living bacterial cells related to organic carbon release from senescent oceanic phytoplankton

S. Lasternas1 and S. Agustí1,2 S. Lasternas and S. Agustí
  • 1Global Change Research Department, IMEDEA (CSIC-UIB), Miquel Marqués 21, 07190 Esporles, Spain
  • 2The UWA Oceans Institute and School of Plant Biology, The University of Western Australia, 35 Stirling Highway, 6009 Crawley, Australia

Abstract. Bacteria recycle vast amounts of organic carbon, playing key biogeochemical and ecological roles in the ocean. Bacterioplankton dynamics are expected to be dependent on phytoplankton primary production, but there is a high diversity of processes (e.g., sloppy feeding, cell exudation, viral lysis) involved in the transfer of primary production to dissolved organic carbon available to bacteria. Here, we show the percentage of living heterotrophic bacterioplankton in the subtropical NE Atlantic Ocean in relation to phytoplankton extracellular carbon release (PER). PER represents the fraction of primary production released as dissolved organic carbon. PER variability was explained by phytoplankton cell death, with communities experiencing higher phytoplankton cell mortality showing a larger proportion of phytoplankton extracellular carbon release. Both PER and the percentage of dead phytoplankton cells increased from eutrophic to oligotrophic waters, while abundance of heterotrophic bacteria was highest in the intermediate waters. The percentage of living heterotrophic bacterial cells (range: 60–95%) increased with increasing phytoplankton extracellular carbon release from productive to oligotrophic waters in the subtropical NE Atlantic. The lower PERs, observed at the upwelling waters, have resulted in a decrease in the flux of phytoplankton dissolved organic carbon (DOC) per bacterial cell. The results highlight phytoplankton cell death as a process influencing the flow of dissolved photosynthetic carbon in this region of the subtropical NE Atlantic Ocean, and suggest a close coupling between the fraction of primary production released and heterotrophic bacterial cell survival.

Final-revised paper