Russon, T.Elliot, M.Kissel, CCabioch, GuyDe Deckker, PatrickCorrege, T.2015-12-100883-8305http://hdl.handle.net/1885/50775The modern δ13CDIC distribution in southwest subtropical Pacific deep waters is consistent with a regional mixing regime between water masses of open Pacific Ocean and Tasman Sea origin. This mixing regime is reconstructed across the middle-late PleistocKeywords: benthic foraminifera; carbon isotope; deep water; mixing; oceanic circulation; Pleistocene; sediment core; New Caledonia [Melanesia]; Pacific Ocean; Southern Ocean; Tasman SeaMiddle-late Pleistocene deep water circulation in the southwest subtropical Pacific200910.1029/2009PA0017552016-02-24