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Late Devonian Extinction

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A prolonged interval of elevated extinction spanning the Kellwasser event, around 372 million years ago near the Frasnian-Famennian boundary, and the Hangenberg event at the very end of the Devonian around 359 million years ago. Roughly 40 percent of marine species were lost, with reef-building organisms especially hard hit, amid widespread oceanic anoxia.

Facts
Magnitude or Scale
Around 40 percent of marine species went extinct; on a finer scale, 57 percent of genera and at least 75 percent of species did not survive into the Carboniferous. 1
Location
Global, with the heaviest losses among tropical reef ecosystems. 1
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Sources
1. Late Devonian Extinction (Wikipedia)
Wikimedia FoundationLead section
Quote, Lead section
A mass extinction event which occurred around 372.15 million years ago, at the boundary between the Frasnian and Famennian ages of the Late Devonian period.
View the Source
1. Late Devonian Extinction (Wikipedia)
Wikimedia FoundationExtinction magnitude section
Quote, Extinction magnitude section
A mass extinction event which occurred around 372.15 million years ago, at the boundary between the Frasnian and Famennian ages of the Late Devonian period.
View the Source
1. Late Devonian Extinction (Wikipedia)
Wikimedia FoundationGeography section
Quote, Geography section
A mass extinction event which occurred around 372.15 million years ago, at the boundary between the Frasnian and Famennian ages of the Late Devonian period.
View the Source
1. Late Devonian Extinction (Wikipedia)
Wikimedia FoundationAssociated With: DevonianView the Source
1. Late Devonian Extinction (Wikipedia)
Wikimedia FoundationAssociated With: CarboniferousView the Source
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