HIGHLIGHTS
SUMMARY
Following the arrows in Fig 2A, the formation of the North Atlantic Deep Water (NADW) introduces well-equilibrated surface waters (and therefore young 14C ventilation ages) to the Rafter et_al, Sci. The result of this modern ocean overturning circulation is that the modern mid-depth Pacific Ocean-not Pacific bottom water-has the oldest 14C ventilation ages of any water mass in the modern ocean. LOESS provides a conservative estimate of the deep-sea 14C ventilation age because it applies different weights to values according to their distance from the binned mean value while . . .
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