Project Details
Description
In this study, the PIs will test and develop a new paleoclimate proxy- Rare Earth Element (REE) abundances of carbonate sediments that contain metalliferous sediment originating from hydrothermal plumes. In combination, the PIs will use Nd isotope values (?Nd) as a proxy to help unravel differences in weathering rates and sources from variations in seawater REE abundances due to other causes. The short residence times of the REE (
| Status | Finished |
|---|---|
| Effective start/end date | 3/1/02 → 2/28/05 |
Funding
- National Science Foundation: $183,197.00
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