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Volume 7, issue 5
Ocean Sci., 7, 533–547, 2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The BONUS-GoodHope IPY project: dynamics and biogeochemistry...

Ocean Sci., 7, 533–547, 2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 Sep 2011

Research article | 06 Sep 2011

Silicon pool dynamics and biogenic silica export in the Southern Ocean inferred from Si-isotopes

F. Fripiat1,2, A.-J. Cavagna3, F. Dehairs3, S. Speich4, L. André1, and D. Cardinal1,* F. Fripiat et al.
  • 1Section of Mineralogy and Petrography, Royal Museum for Central Africa, Tervuren, Belgium
  • 2Department of Earth and Environmental Sciences, Université Libre de Bruxelles, Bruxelles, Belgium
  • 3Analytical and Environmental Chemistry & Earth System Sciences, Vrije Universiteit Brussel, Brussels, Belgium
  • 4Laboratoire de Physique des Océans, UMR6523, IFREMER, CNRS, IRD, UBO, Plouzane, France
  • *now at: Laboratoire d'Océanographie et du Climat: Expérimentations et Approches Numériques, Université Pierre & Marie Curie, Paris, France

Abstract. Silicon isotopic signatures (δ30Si) of water column silicic acid (Si(OH)4) were measured in the Southern Ocean, along a meridional transect from South Africa (Subtropical Zone) down to 57° S (northern Weddell Gyre). This provides the first reported data of a summer transect across the whole Antarctic Circumpolar Current (ACC). δ30Si variations are large in the upper 1000 m, reflecting the effect of the silica pump superimposed upon meridional water transfer across the ACC: the transport of Antarctic surface waters northward by a net Ekman drift and their convergence and mixing with warmer upper-ocean Si-depleted waters to the north. Using Si isotopic signatures, we determine different mixing interfaces: the Antarctic Surface Water (AASW), the Antarctic Intermediate Water (AAIW), and thermoclines in the low latitude areas. The residual silicic acid concentrations of end-members control the δ30Si alteration of the mixing products and with the exception of AASW, all mixing interfaces have a highly Si-depleted mixed layer end-member. These processes deplete the silicic acid AASW concentration northward, across the different interfaces, without significantly changing the AASW δ30Si composition. By comparing our new results with a previous study in the Australian sector we show that during the circumpolar transport of the ACC eastward, the δ30Si composition of the silicic acid pools is getting slightly, but significantly lighter from the Atlantic to the Australian sectors. This results either from the dissolution of biogenic silica in the deeper layers and/or from an isopycnal mixing with the deep water masses in the different oceanic basins: North Atlantic Deep Water in the Atlantic, and Indian Ocean deep water in the Indo-Australian sector. This isotopic trend is further transmitted to the subsurface waters, representing mixing interfaces between the surface and deeper layers.

Through the use of δ30Si constraints, net biogenic silica production (representative of annual export), at the Greenwich Meridian is estimated to be 5.2 ± 1.3 and 1.1 ± 0.3 mol Si m−2 for the Antarctic Zone and Polar Front Zone, respectively. This is in good agreement with previous estimations. Furthermore, summertime Si-supply into the mixed layer of both zones, via vertical mixing, is estimated to be 1.6 ± 0.4 and 0.1 ± 0.5 mol Si m−2, respectively.

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