Neodymium isotope evidence for glacial-interglacial variability of deepwater transit time in the Pacific Ocean
The response of deep Pacific overturning to glacial-interglacial climate change is still debated. Here the authors show a generally faster deep Pacific overturning operated in recent glacial periods based on a novel application of Nd isotopes recorded in foraminifera.
| Main Authors: | , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2018-11-01
|
| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-018-07079-z |