

The Late Devonian Extinction
18 snips 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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Late Devonian Extinction Overview
- The Late Devonian extinction was a slower mass extinction, unlike asteroid impacts.
- It devastated around 70% of species roughly 370 million years ago.
Devonian Earth
- Earth looked different in the Devonian period, with continents mainly in the southern hemisphere.
- The first trees and soils were emerging, but land was largely barren.
Devonian Marine Life
- The Devonian period, known as the Age of Fishes, had diverse marine life, including armored fish.
- Reefs were built by corals and sponges different from today's.