Barium and Lithium in Foraminifera: Glacial-Interglacial Changes in the North Atlantic
The trace element content of calcareous foraminifera provides a powerful tool to the study of glacial-interglacial changes in the physical and chemical properties of the ocean. Foraminifera incorporate barium in direct proportion to its concentration in seawater. Using barium as a nutrient proxy, Ba...
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| Format: | Others |
| Language: | en |
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LSU
2002
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| Online Access: | http://etd.lsu.edu/docs/available/etd-0710102-192931/ |