|Glacial-interglacial changes in bottom-water oxygen content on the Portuguese margin|Hoogakker, B.A.A.; Elderfield, H.; Schmiedl, G.; McCave, I.N.; Rickaby, R.E.M. (2015). Glacial-interglacial changes in bottom-water oxygen content on the Portuguese margin. Nature Geoscience 8(1): 40–43. hdl.handle.net/10.1038/ngeo2317
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894, more
|Authors|| || Top |
- Hoogakker, B.A.A.
- Elderfield, H.
- Schmiedl, G.
- McCave, I.N.
- Rickaby, R.E.M.
Some of the glacial CO2 drawdown has been attributed to CO2 storage in the deep Pacific and Southern oceans. Reconstruction of apparent oxygen utilization suggests that respired CO2 storage was also enhanced in the deep northeast Atlantic.