Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery
Oceanic anoxia is invoked for driving the Permo-Triassic Mass Extinction, but the timing, distribution and chemical state are poorly understood. Here, the authors show that fluctuations of anoxic, non-sulfidic (ferruginous) conditions were important for the delayed biotic recovery in the Neo-Tethys.
| Main Authors: | , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2016-07-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms12236 |