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The Kellwasser Event was a significant mass extinction event that primarily impacted marine life during the Devonian Period, approximately 372 million years ago. This event is characterized by widespread anoxic (low-oxygen) conditions in the oceans, evidenced by layers of black shale.1

The Kellwasser Event led to the extinction of various marine groups, including specific types of goniatites (an ancient group of cephalopods), many conodont species, most colonial corals, several trilobite groups, and certain brachiopods. While a meteorite impact has been considered a potential cause, with evidence of an impact crater dated to around the time of the event, its direct link to the Kellwasser Event is still debated. Environmental factors, such as global cooling and increased nutrient runoff from continents, are also considered contributing factors to this extinction.1

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