Bostock, HelenOpdyke, BradleyWilliams, Michael J.M.2015-12-080967-0637http://hdl.handle.net/1885/35209Evidence from geochemical tracers (salinity, oxygen, silicate, nutrients, alkalinity, dissolved inorganic carbon (DIC), carbon isotopes (δ13CDIC) and radiocarbon (Δ14C)) collected during the Pacific Ocean World Ocean Circulation Experiment (WOCE) voyageKeywords: Antarctic intermediate waters; Benthic foraminifera; Carbon isotopes; Conservative tracers; Deep Water; Diatom production; Dissolved inorganic carbon; Eastern equatorial Pacific; Equatorial Pacific; Four-core; Geochemical properties; Geochemical proxies; d13C; d14C; AAIW; Benthic foraminifera; Equatorial intermediate waters; Geochemical tracers; Intermediate depth waters; NPIW; Pacific OceanCharacterising the intermediate depth waters of the Pacific Ocean using δ 13 C and other geochemical tracers201010.1016/j.dsr.2010.04.0052016-02-24