Glacial CO<sub>2</sub> decrease and deep-water deoxygenation by iron fertilization from glaciogenic dust
<p>Increased accumulation of respired carbon in the deep ocean associated with enhanced efficiency of the biological carbon pump is thought to be a key mechanism of glacial <span class="inline-formula">CO<sub>2</sub></span> drawdown. Despite greater oxygen sol...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-06-01
|
| Series: | Climate of the Past |
| Online Access: | https://www.clim-past.net/15/981/2019/cp-15-981-2019.pdf |