Miocene Antarctic Ice Sheet area adapts significantly faster than volume to CO<sub>2</sub>-induced climate change
<p>The strongly varying benthic <span class="inline-formula"><i>δ</i><sup>18</sup></span>O levels of the early and mid-Miocene (23 to 14 Myr ago) are primarily caused by a combination of changes in Antarctic Ice Sheet (AIS) volume and deep-ocean te...
| Main Authors: | , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-01-01
|
| Series: | Climate of the Past |
| Online Access: | https://cp.copernicus.org/articles/20/257/2024/cp-20-257-2024.pdf |