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- W2022357076 abstract "We examined the zinc content of diatom frustules as an indicator of past changes in surface seawater Zn 2+ concentration. Zn/Si data of samples from three cores located in the South Atlantic sector of the Southern Ocean spanning the last interglacial‐glacial transition are presented. Changes in the Zn/Si record are linked to changes in the surface water Zn 2+ concentration. The source of variation in Zn 2+ concentration appears to be via changes in deep water upwelling and circulation. We rule out changes in phytoplankton productivity and aeolian dust input as a source of variation in the Zn/Si record. Likewise, the Zn/Si data are not linked to shifts in the diatom species composition of the sediment or sediment preservation effects. The Zn/Si results presented do not support the zinc hypothesis. There is no link between the uptake of CO 2 by phytoplankton, as inferred from the δ 13 C record, and the Zn/Si record." @default.
- W2022357076 created "2016-06-24" @default.
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- W2022357076 date "2000-10-01" @default.
- W2022357076 modified "2023-10-08" @default.
- W2022357076 title "Variations in the Zn/Si record over the Last Interglacial Glacial Transition" @default.
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- W2022357076 doi "https://doi.org/10.1029/1999pa000470" @default.
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