Exploring the mechanisms of Devonian oceanic anoxia: impact of ocean dynamics, palaeogeography, and orbital forcing
<p>The Devonian is a warmer-than-present geological period spanning from 419 to 359 million years ago (Ma) characterized by multiple identified ocean anoxic/hypoxic events. Despite decades of extensive investigation, no consensus has been reached regarding the drivers of these anoxic events. While...
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| Автори: | , , , , , , |
|---|---|
| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
Copernicus Publications
2025-01-01
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| Серія: | Climate of the Past |
| Онлайн доступ: | https://cp.copernicus.org/articles/21/239/2025/cp-21-239-2025.pdf |
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