Carbon sequestration in an expanded lake system during the Toarcian oceanic anoxic event
The Early Jurassic Toarcian oceanic anoxic event (∼183 Ma) was marked by marine anoxia–euxinia and globally significant organic-matter burial, accompanied by a major global carbon-cycle perturbation probably linked to Karoo–Ferrar volcanism. Although the Toarcian oceanic anoxic event is well studied...
| Автори: | , , , , , , , , , , |
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| Формат: | Journal article |
| Опубліковано: |
Springer Nature
2017
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