
In Our Time The Late Devonian Extinction
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Mar 11, 2021 Jessica Whiteside, an Associate Professor of Geochemistry, and David Bond, a Professor of Geology, dive into the mysteries of the Late Devonian Extinction, a catastrophic event that wiped out about 70% of species. They discuss how early land plants and their soil formation caused algal blooms, leading to oxygen depletion in oceans. The pair also explore climate dynamics and geological evidence, highlighting the extensive impact on marine and terrestrial life and drawing intriguing parallels to modern climate change.
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Fish to Tetrapods
- Fish evolved into tetrapods during the Devonian, fins transforming into legs.
- This transition was driven by opportunities on land, like the expanding plant life.
Multiple Extinction Events
- Multiple anoxic black shale events occurred throughout the Devonian period.
- The Kellwasser and Hangenberg events, separated by 30 million years, were distinct extinctions.
Hangenberg Event and Ozone
- The Hangenberg event, a fiery and icy climax, involved ozone depletion.
- This potentially stemmed from increased temperatures or a cosmic event like a supernova.
