Articles | Volume 12, issue 5
Biogeosciences, 12, 1415–1430, 2015

Special issue: KEOPS2: Kerguelen Ocean and Plateau Study 2

Biogeosciences, 12, 1415–1430, 2015

Research article 05 Mar 2015

Research article | 05 Mar 2015

Use of Ra isotopes to deduce rapid transfer of sediment-derived inputs off Kerguelen

V. Sanial1, P. van Beek1, B. Lansard1,2, M. Souhaut1, E. Kestenare1, F. d'Ovidio3, M. Zhou4, and S. Blain5,6 V. Sanial et al.
  • 1LEGOS, Laboratoire d'Etudes en Géophysique et Océanographie Spatiales, (CNRS-CNES-IRD-UPS), Observatoire Midi Pyrénées, 14 avenue Edouard Belin, 31400 Toulouse, France
  • 2LSCE, Laboratoire des Sciences du Climat et de l'Environnement (IPSL-CEA-CNRS-UVSQ-IPSL), avenue de la Terrasse, 91198 Gif-sur-Yvette, France
  • 3Sorbonne Universités, UPMC Univ Paris 06, CNRS, LOCEAN-IPSL, 4 place Jussieu, 75005 Paris, France
  • 4Department of Environment Earth and Ocean Sciences, University of Massachusetts Boston, Boston, Massachusetts, USA
  • 5Sorbonne Universités, UPMC Univ Paris 06, UMR7621, Laboratoire d'Océanographie Microbienne, Observatoire Océanologie, 66650 Banyuls/mer, France
  • 6CNRS, UMR7621, Laboratoire d'Océanologie Microbienne, Observatoire Océanologie, 66650 Banyuls/mer, France

Abstract. The Southern Ocean is known to be the largest high-nutrient, low-chlorophyll (HNLC) region of the global ocean due to iron limitation. However, a large phytoplankton bloom develops annually downstream of the Kerguelen Islands, a bloom which is sustained partly by iron released from the sediments deposited onto the shelves. In the framework of the KEOPS-2 project, we used radium isotopes (224Ra, T1/2 = 3.66 d; 223Ra, T1/2 = 11.4 d; 228Ra, T1/2 = 5.75 yr) to provide information on the origin of iron fertilization and on the timescales of the transfer of sediment-derived inputs (including iron and other micronutrients) towards offshore waters. Significant 224Ra and 223Ra activities were found in the near vicinity of the Kerguelen Islands, in agreement with the short half-lives of these isotopes. Significant 224Ra and 223Ra activities were also detected up to 200 km downstream of the islands and more unexpectedly in offshore waters south of the polar front. These observations thus clearly indicate (i) that the sediment-derived inputs are rapidly transferred towards offshore waters (on timescales on the order of several days up to several weeks) and (ii) that the polar front is not a physical barrier for the chemical elements released from the sediments of the Kerguelen Plateau. The Ra data set suggests that iron and other micronutrients released by the shelves of the Kerguelen Islands may contribute to fueling the phytoplankton bloom downstream of the islands, despite the presence of the polar front. However, the heterogeneous distribution of the 224Ra and 223Ra activities in surface waters suggests that this supply across the front is not a continuous process but rather a process that is highly variable in space and time.

Short summary
We investigated the origin and mechanisms of the natural iron fertilization that sustains a phytoplankton bloom downstream of the Kerguelen Islands. We used radium isotopes to trace the fate of shelf waters that may transport iron and other micronutrients towards offshore waters. We show that shelf waters are rapidly transferred offshore and may be transported across the polar front (PF). The PF may thus not be a strong physical barrier for chemical elements released by the shelf sediments.
Final-revised paper