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Middle Maastrichtian Event
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The Middle Maastrichtian Event (MME) was a climatic perturbation that occurred during the Maastrichtian stage of the Late Cretaceous epoch. The event featured global drying, warming, and changes to ocean circulation and chemistry.
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Timeline
The MME occurred approximately 69.5 Ma.[1]
Causes
The MME is believed to have been caused by increased volcanic CO2 emissions.[2]
Effects
In central Alaska, mean annual precipitation (MAP) precipitously declined; it was 353–1050 mm before the MME and 475–1451 mm after the MME but only 168–470 mm during the MME.[1]
The combination of global warming, ocean circulation disruption, ocean acidification, and toxic metal influx caused the extinction of inoceramid bivalves.[2] In northwestern Europe, benthic foraminiferal assemblages remained relatively unchanged.[3]
References
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