Relationships between bottom water carbonate saturation and element/Ca ratios in coretop samples of the benthic foraminifera <i>Oridorsalis umbonatus</i>
Elemental ratios in benthic foraminifera have been used to reconstruct bottom water temperature and carbonate saturation (Δ[CO<sub>3</sub><sup>2−</sup>]). We present elemental data for the long-ranging benthic foraminifera <i>Oridorsalis umbonatus<...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2012-08-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/9/3029/2012/bg-9-3029-2012.pdf |