Upper-ocean-to-atmosphere radiocarbon offsets imply fast deglacial carbon dioxide release.

• Main Authors: Rose, Kathryn A, Sikes, Elisabeth L, Guilderson, Thomas P, Shane, Phil, Hill, Tessa M, Zahn, Rainer, Spero, Howard J
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2010
• Subjects: Plankton; Carbon Dioxide; Carbon Radioisotopes; Atmosphere; Ice Cover; Seawater; Water Movements; Environmental Monitoring; Geologic Sediments; Oceans and Seas; Foraminifera; Global Warming; General Science & Technology; Pacific; Southern Ocean
• Online Access: https://escholarship.org/uc/item/5486407b

Radiocarbon in the atmosphere is regulated largely by ocean circulation, which controls the sequestration of carbon dioxide (CO(2)) in the deep sea through atmosphere-ocean carbon exchange. During the last glaciation, lower atmospheric CO(2) levels were accompanied by increased atmospheric radiocarbon concentrations that have been attributed to greater storage of CO(2) in a poorly ventilated abyssal ocean. The end of the ice age was marked by a rapid increase in atmospheric CO(2) concentrations that coincided with reduced (14)C/(12)C ratios (Delta(14)C) in the atmosphere, suggesting the release of very 'old' ((14)C-depleted) CO(2) from the deep ocean to the atmosphere. Here we present radiocarbon records of surface and intermediate-depth waters from two sediment cores in the southwest Pacific and Southern oceans. We find a steady 170 per mil decrease in Delta(14)C that precedes and roughly equals in magnitude the decrease in the atmospheric radiocarbon signal during the early stages of the glacial-interglacial climatic transition. The atmospheric decrease in the radiocarbon signal coincides with regionally intensified upwelling and marine biological productivity, suggesting that CO(2) released by means of deep water upwelling in the Southern Ocean lost most of its original depleted-(14)C imprint as a result of exchange and isotopic equilibration with the atmosphere. Our data imply that the deglacial (14)C depletion previously identified in the eastern tropical North Pacific must have involved contributions from sources other than the previously suggested carbon release by way of a deep Southern Ocean pathway, and may reflect the expanded influence of the (14)C-depleted North Pacific carbon reservoir across this interval. Accordingly, shallow water masses advecting north across the South Pacific in the early deglaciation had little or no residual (14)C-depleted signals owing to degassing of CO(2) and biological uptake in the Southern Ocean.