Detecting holocene changes in thermohaline circulation.

Keigwin, L D; Boyle, E A · Proc Natl Acad Sci U S A · 2000

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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.

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