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| The research group collecting samples. Photo Credit Ben Gill |
A decline in the element molybdenum across the planet’s oceans preceded a significant extinction event approximately 183 million years ago, new research from Florida State University shows.
The decrease may have contributed to the mass extinction, in which up to 90% of species in the oceans perished, and it suggests that much more organic carbon was buried in the extinction event than had been previously estimated. The work is published in AGU Advances.
“This research tells us more about what was happening with molybdenum during this extinction event, but we also take it a step further,” said Jeremy Owens, an associate professor in FSU’s Department of Earth, Ocean and Atmospheric Science and a paper co-author. “Our findings help us understand how much carbon was cycling through the system, and it’s much larger than previously thought — potentially on the scale of modern atmospheric and oceanic increases due to human activities.”
Previous research showed decreases in molybdenum during the main phase of the ancient mass extinction, but it was unclear how widespread the decrease was, how early it started or how long it lasted.
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