Relevance of silicon isotopes to Si-nutrient utilization and Si-source assessment in Antarctic
| Type | Article | ||||||||
|---|---|---|---|---|---|---|---|---|---|
| Date | 2005-04 | ||||||||
| Language | English | ||||||||
| Author(s) | Cardinal D1, Alleman Ly1, Dehairs F2, Savoye N2, Trull Tw3, Andre L1 | ||||||||
| Affiliation(s) | 1 : Musee Royal Afr Cent, Dept Geol & Mineral, B-3080 Tervuren, Belgium. 2 : Univ Libre Brussels, Dept Analyt & Environm Chem, B-1050 Brussels, Belgium. 3 : Univ Tasmania, CSIRO Marine Res, Antarctic Climate & Ecosyst Cooperat Res Ctr, Hobart, Tas 7001, Australia. |
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| Source | Global Biogeochemical Cycles (0886-6236) (Amer Geophysical Union), 2005-04 , Vol. 19 , N. 2/GB2007 , P. 1-13 | ||||||||
| DOI | 10.1029/2004GB002364 | ||||||||
| WOS© Times Cited | 117 | ||||||||
| Keyword(s) | δ29Si, δ30Si, diatoms, spring Southern Ocean, fractionation factor | ||||||||
| Abstract | We analyzed delta(29) Si of dissolved silicate for eight water column profiles across the Southern Ocean ( south of Australia in spring 2001) from the Seasonal Ice Zone (SIZ) north to the Subantarctic Zone (SAZ), including the first isotopic compositions measured for Si-depleted seawaters. All profiles display mixed layer enrichments in heavy Si isotopes relative to deep water in accordance with preferential uptake of the light isotope by diatoms. As silicate levels decrease from the SIZ northward across the Polar Front Zone (PFZ) to the SAZ, surface and mesopelagic delta(29) Si signatures generally become progressively heavier, but the most Si-depleted SAZ waters do not exhibit delta(29) Si values heavier than in the PFZ. This intricacy appears to derive from variations in the vertical and horizontal supply of silicate to surface waters, and by applying a steady state open system model, we estimate a fractionation factor, (29)epsilon, between diatoms and seawater of -0.45 +/- 0.17%, independently of zones and phytoplankton community. Though encouraging, these results are related to latitudinal changes in mesopelagic delta(29) Si values, complexity in surface silicate - delta(29) Si correlations, and differences from previous studies, which underline the need for caution in the use of silicon isotopes in paleoceanographic studies until systematic efforts have been undertaken to better understand modern variations. | ||||||||
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