Nonetheless, it is critical to point out that any Mg/Ca sw correction of Mg/Ca-derived SSTs results in the decrease of Site 806 temperatures from the late Miocene to the Pliocene and Pleistocene, in stark contrast with the uncorrected SSTs which do not show a clear trend over the last 10 Myr (Fig. 2b ).
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Persistent high latitude amplification of the Pacific Ocean over the past 10 million years.
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