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From:Climate of the Past (Vol. 19, Issue 1) Peer-Reviewed
Unraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2.The mid-Pliocene warm period (3.264-3.025 Ma) is the most recent geological period in which the atmospheric CO.sub.2 concentration was approximately equal to the concentration we measure today (ca. 400 ppm). Sea surface...
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