Skinner, L. C.Scrivner, A EVance, DerekBarker, SFallon, StewartWaelbroeck, Claire2015-12-130091-7613http://hdl.handle.net/1885/72804Past glacial-interglacial climate transitions were accompanied by millennial-scale pulses in atmospheric CO2 that are widely thought to have resulted from the release of CO2 via the Southern Ocean. However, direct proxy evidence for a Southern Ocean roleKeywords: Air-sea exchange; Antarctic regions; Climate transition; Global climates; Last deglaciation; Neodymium isotopes; Ocean ventilations; Ocean-atmosphere; Carbon dioxide; Isotopes; Ventilation; Oceanography; air-sea interaction; carbon dioxide; deep water ven201310.1130/G34133.12016-02-24