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 temperatures. These factors are coupled since AIS chan...
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| Auteurs principaux: | , , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
Copernicus Publications
2024-01-01
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| Collection: | Climate of the Past |
| Accès en ligne: | https://cp.copernicus.org/articles/20/257/2024/cp-20-257-2024.pdf |
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