| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445688 | Quaternary Science Reviews | 2013 | 18 Pages |
Abstract
⺠Large seasonal shifts in δ2H and δ18O reflect changes in water balance. ⺠Upper limit of δ30Si values for dissolved Si in natural waters is increased by 1â°. ⺠Progressive downstream enrichment in δ30Si represents Si uptake by aquatic ecosystems. ⺠δ30Si values are enriched in dry season due to biological demand exceeding DSi supply. ⺠DSi flux to the oceans can be expected to vary on a glacial/interglacial time scale.
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Earth and Planetary Sciences
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Authors
H.E. Cockerton, F.A. Street-Perrott, M.J. Leng, P.A. Barker, M.S.A. Horstwood, V. Pashley,