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Published Online February 28, 2008
Science DOI: 10.1126/science.1150595

Reports

Submitted on September 17, 2007
Accepted on February 19, 2008

Covariant Glacial-Interglacial Dust Fluxes in the Equatorial Pacific and Antarctica

Gisela Winckler 1*, Robert F. Anderson 2, Martin Q. Fleisher 1, David McGee 2, Natalie Mahowald 3

1 Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.
2 Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.; Department of Earth and Environmental Sciences, Columbia University, New York, NY 10027, USA.
3 Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY 14853, USA.

* To whom correspondence should be addressed.
Gisela Winckler , E-mail: winckler{at}ldeo.columbia.edu

Dust plays a critical role in Earth’s climate system and serves as a natural source of iron and other micronutrients to remote regions of the ocean. We have generated records of dust deposition over the past 500,000 years at three sites spanning the breadth of the equatorial Pacific Ocean. Equatorial Pacific dust fluxes are highly correlated with global ice volume and with dust fluxes to Antarctica, suggesting that dust generation in interhemispheric source regions exhibited a common response to climate change over late-Pleistocene glacial cycles. Our results provide quantitative constraints on the variability of aeolian iron supply to the equatorial Pacific Ocean and, more generally, on the potential contribution of dust to past climate change and to related changes in biogeochemical cycles.


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Atmospheric CO2 and Climate on Millennial Time Scales During the Last Glacial Period.
J. Ahn and E. J. Brook (2008)
Science 322, 83-85
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Science. ISSN 0036-8075 (print), 1095-9203 (online)