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Exploring interacting influences on the silicon isotopic composition of the surface ocean: a case study from the Kerguelen Plateau

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Figure

Fig. 1. Map of the study area in the Atlantic and Indian sectors of the Southern Ocean
Fig. 2. Schematic representation of the box model, adapted from Platt et al. (2003). Dissolved silicon in the mixed layer (DSiML) is suppliedby the Winter Water (WW) through mixing, by the dissolution of non-living diatoms (BSiD) in the mixed layer (ML), a
Table 3. Abbreviations and subscripts used in the model equations.
Fig. 3. Profiles of30δ (A) DSi concentration data versus depth and (B)SiDSi versus depth from the CTD stations.
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