Accelerator mass spectrometry radiocarbon stratigraphies in deep Labrador Sea cores: paleoceanographic implications
Foraminiferal accelerator mass spectrometry (AMS) 14 C ages and benthic–planktonic age differences in surface-layer sediments of Labrador Sea are influenced by bioturbation and by changes in the relative abundance of foraminiferal species carrying the 14 C signal. Using benthic-mixing models we demo...
| Published in: | Canadian Journal of Earth Sciences |
|---|---|
| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Canadian Science Publishing
1994
|
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1139/e94-005 http://www.nrcresearchpress.com/doi/pdf/10.1139/e94-005 |
| Summary: | Foraminiferal accelerator mass spectrometry (AMS) 14 C ages and benthic–planktonic age differences in surface-layer sediments of Labrador Sea are influenced by bioturbation and by changes in the relative abundance of foraminiferal species carrying the 14 C signal. Using benthic-mixing models we demonstrate that inverse benthic–planktonic age differences can be generated when the effect of benthic mixing and abundance change exceeds apparent age differences between surface water and deep water. AMS 14 C ages obtained put constraints on the timing of major paleoceanographic changes in the basin, notably on the history of the Western Boundary Undercurrent, which was clearly reinitiated during the mid-deglaciation and intensified during the last 2–3 ka. |
|---|