Last Glacial Maximum and deglacial abyssal seawater oxygen isotopic ratios
An earlier analysis of pore-water salinity (chlorinity) in two deep-sea cores, using terminal constraint methods of control theory, concluded that although a salinity amplification in the abyss was possible during the LGM, it was not required by the data. Here the same methodology is applied to δ[su...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Article |
| Published: |
Copernicus GmbH
2018
|
| Online Access: | http://hdl.handle.net/1721.1/113851 https://orcid.org/0000-0001-6808-3664 |