Simulating the climate response to atmospheric oxygen variability in the Phanerozoic: a focus on the Holocene, Cretaceous and Permian
<p>The amount of dioxygen (<span class="inline-formula">O<sub>2</sub></span>) in the atmosphere may have varied from as little as 5 % to as much as 35 % during the Phanerozoic eon (54 Ma–present). These changes in the amount of...
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-08-01
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| Series: | Climate of the Past |
| Online Access: | https://www.clim-past.net/15/1463/2019/cp-15-1463-2019.pdf |