Detecting holocene changes in thermohaline circulation.
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.
Keigwin
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LD
Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. lkeigwin@whoi.edu
Boyle
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EA
D000818:Animals; D001267:Atlantic Ocean; D002247:Carbon Isotopes; D002980:Climate; D007053:Ice; D010103:Oxygen Isotopes; D010933:Plankton; D013995:Time
D002247:Carbon Isotopes; D007053:Ice; D010103:Oxygen Isotopes