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March 19 2013
Ancient rises in sea levels and global warming are partially attributable to cyclical activity below the earth's surface, researchers from New York University and Ottawa's Carleton University have concluded in an analysis of geological studies.
However, the article's authors, NYU's Michael Rampino and Carleton University's Andreas Prokoph, note that changes spurred by the earth's interior are gradual, taking place in periods ranging from 60 million to 140 million years—far less rapidly than those brought on by human activity.
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