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Detecting Holocene Changes in Thermohaline Circulation

L. D. Keigwin and E. A. Boyle
Proceedings of the National Academy of Sciences of the United States of America
Vol. 97, No. 4 (Feb. 15, 2000), pp. 1343-1346
Stable URL: http://www.jstor.org/stable/121472
Page Count: 4
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Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Detecting Holocene Changes in Thermohaline Circulation
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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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