Radiocarbon evidence for a possible abyssal front near 3.1 km in the glacial equatorial Pacific Ocean

We investigate the radiocarbon ventilation age in deep equatorial Pacific sediment cores using the difference in conventional C-14 age between coexisting benthic and planktonic foraminifera, and integrate those results with similar data from around the North Pacific Ocean in a reconstruction for the last glaciation (15 to 25 conventional C-14 ka). Most new data from both the Equatorial Pacific and the Emperor Seamounts in the northwestern Pacific come from maxima in abundance of benthic taxa because this strategy reduces the effect of bioturbation. Although there remains considerable scatter in the ventilation age estimates, on average, ventilation ages in the Equatorial Pacific were significantly greater below 3.2 km (similar to 3080 +/- 1125 yrs, n = 15) than in the depth interval 1.9 to 3.0 km (similar to 1610 +/- 250 yrs, n = 12). When compared to the average modem seawater Delta C-14 profile for the North Pacific, the Equatorial Pacific glacial data suggest an abyssal front located somewhere between 3.0 and 3.2 km modern water depth. Above that depth, the data may indicate slightly better ventilation than today, and below that depth, glacial Equatorial Pacific data appear to be as old as last glacial maximum (LGM) deep water ages reported for the deep southern Atlantic. This suggests that a glacial reservoir of aged waters extended throughout the circumpolar Southern Ocean and into the Equatorial Pacific. Renewed ventilation of such a large volume of aged (and, by corollary, carbon-rich) water would help to account for the rise in atmospheric pCO(2) and the fall in Delta C-14 as the glaciation drew to a close. (C) 2015 Elsevier B.V. All rights reserved.