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The Taghanic Event was a significant mass extinction event during the Devonian Period, approximately 419.2 to 359 million years ago. This event, along with others like the Kellwasser and Hangenberg events, contributed to the elimination of a substantial percentage of marine species. The Taghanic Event specifically marked a period of extinction for goniatites, corals, and brachiopods.12

While the exact cause of Devonian extinctions remains debated, potential contributing factors include excessive sedimentation, rapid climate shifts (warming or cooling), meteorite impacts, and increased nutrient runoff from continents. Evidence suggests that periods of low oxygen (hypoxic or anoxic conditions) in Devonian seas were strongly linked to these extinctions. It is likely that a combination of these stresses led to the widespread loss of life during this era.12

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