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Particulate barium tracing of significant mesopelagic carbon remineralisation in the North Atlantic

Authors
  • Lemaitre, Nolwenn
  • Planquette, Hélène
  • Planchon, Frédéric
  • Sarthou, Géraldine
  • Jacquet, Stéphanie
  • García-Ibáñez, Maribel
  • Gourain, Arthur
  • Cheize, Marie
  • Monin, Laurence
  • André, Luc
  • Laha, Priya
  • Terryn, Herman
  • Dehairs, Frank
Publication Date
Apr 09, 2018
Identifiers
DOI: 10.5194/bg-15-2289-2018
OAI: oai:HAL:hal-02024247v1
Source
HAL-SHS
Keywords
Language
English
License
Unknown
External links

Abstract

The remineralisation of sinking particles by prokaryotic heterotrophic activity is important for controlling oceanic carbon sequestration. Here, we report mesopelagic particulate organic carbon (POC) remineralisation fluxes in the North Atlantic along the GEOTRACES-GA01 section (GEOVIDE cruise; May-June 2014) using the particulate biogenic barium (excess barium; Ba xs) proxy. Important mesopelagic (100-1000 m) Ba xs differences were observed along the transect depending on the intensity of past blooms, the phytoplankton community structure, and the physical forcing, including downwelling. The subpolar province was characterized by the highest mesopelagic Ba xs content (up to 727 pmol L −1), which was attributed to an intense bloom averaging 6 mg chl a m −3 between January and June 2014 and by an intense 1500 m deep convection in the central Labrador Sea during the winter preceding the sampling. This down-welling could have promoted a deepening of the prokaryotic heterotrophic activity, increasing the Ba xs content. In comparison , the temperate province, characterized by the lowest Ba xs content (391 pmol L −1), was sampled during the bloom period and phytoplankton appear to be dominated by small and calcifying species, such as coccolithophorids. The Ba xs content, related to oxygen consumption, was converted into a remineralisation flux using an updated relationship, proposed for the first time in the North Atlantic. The estimated fluxes were of the same order of magnitude as other fluxes obtained using independent methods (moored sediment traps, incubations) in the North Atlantic. Interestingly, in the subpolar and subtropical provinces, mesopelagic POC remineralisa-tion fluxes (up to 13 and 4.6 mmol C m −2 d −1 , respectively) were equalling and occasionally even exceeding upper-ocean POC export fluxes, deduced using the 234 Th method. These results highlight the important impact of the mesopelagic remineralisation on the biological carbon pump of the studied area with a near-zero, deep (> 1000 m) carbon sequestration efficiency in spring 2014.

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