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Southern Ocean control of silicon stable isotope distribution in the deep Atlantic Ocean
de Souza, G.F.; Reynolds, B.C.; Rickli, J.; Frank, M.; Saito, M.A.; Gerringa, L.J.A.; Bourdon, B. (2012). Southern Ocean control of silicon stable isotope distribution in the deep Atlantic Ocean. Global Biogeochem. Cycles 26.
In: Global Biogeochemical Cycles. American Geophysical Union: Washington, DC. ISSN 0886-6236; e-ISSN 1944-9224, meer
Peer reviewed article  

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  • de Souza, G.F.
  • Reynolds, B.C.
  • Rickli, J.
  • Frank, M.
  • Saito, M.A.
  • Gerringa, L.J.A., meer
  • Bourdon, B.

    The fractionation of silicon (Si) stable isotopes by biological activity in the surface ocean makes the stable isotope composition of silicon (delta Si-30) dissolved in seawater a sensitive tracer of the oceanic biogeochemical Si cycle. We present a high-precision dataset that characterizes the delta Si-30 distribution in the deep Atlantic Ocean from Denmark Strait to Drake Passage, documenting strong meridional and smaller, but resolvable, vertical delta Si-30 gradients. We show that these gradients are related to the two sources of deep and bottom waters in the Atlantic Ocean: waters of North Atlantic and Nordic origin carry a high delta(30)Sisignature of >=+1.7 parts per thousand into the deep Atlantic, while Antarctic Bottom Water transports Si with a low delta Si-30 value of around +1.2 parts per thousand. The deep Atlantic delta Si-30 distribution is thus governed by the quasi-conservative mixing of Si from these two isotopically distinct sources. This disparity in Si isotope composition between the North Atlantic and Southern Ocean is in marked contrast to the homogeneity of the stable nitrogen isotope composition of deep ocean nitrate (delta N-15-NO3). We infer that the meridional delta Si-30 gradient derives from the transport of the high delta Si-30 signature of Southern Ocean intermediate/mode waters into the North Atlantic by the upper return path of the meridional overturning circulation (MOC). The basin-scale deep Atlantic delta Si-30 gradient thus owes its existence to the interaction of the physical circulation with biological nutrient uptake at high southern latitudes, which fractionates Si isotopes between the abyssal and intermediate/mode waters formed in the Southern Ocean.

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