title: Detecting holocene changes in thermohaline circulation.
abstract: Throughout the last glacial cycle, reorganizations of deep ocean water masses were coincident with rapid millennial-scale changes in climate. Climate changes have been less severe during the present interglacial, but evidence for concurrent deep ocean circulation change is ambiguous.
authors.affiliation: Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. lkeigwin@whoi.edu
authors.forename: L D
authors.initials: LD
authors.lastname: Keigwin
authors.forename: E A
authors.initials: EA
authors.lastname: Boyle
mesh_terms: D000818:Animals; D001267:Atlantic Ocean; D002247:Carbon Isotopes; D002980:Climate; D007053:Ice; D010103:Oxygen Isotopes; D010933:Plankton; D013995:Time
chemical_list: D002247:Carbon Isotopes; D007053:Ice; D010103:Oxygen Isotopes