Paleodust variability since the Last Glacial Maximum and implications for iron inputs to the ocean-Reference-Cited by-同舟云学术

Paleodust variability since the Last Glacial Maximum and implications for iron inputs to the ocean

Published:2016-04-28 Issue:8 Volume:43 Page:3944-3954
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Albani S.¹²,Mahowald N. M.¹,Murphy L. N.³,Raiswell R.⁴,Moore J. K.⁵,Anderson R. F.⁶,McGee D.⁷,Bradtmiller L. I.⁸,Delmonte B.⁹,Hesse P. P.¹⁰,Mayewski P. A.¹¹

Affiliation:

1. Department of Earth and Atmospheric Sciences Cornell University Ithaca New York USA

2. Now at the Institute for Geophysics and Meteorology University of Cologne Cologne Germany

3. Rosenstiel School of Marine and Atmospheric Science University of Miami Miami Florida USA

4. School of Earth and Environment, Faculty of Environment University of Leeds Leeds UK

5. Department of Earth System Science University of California Irvine California USA

6. Lamont‐Doherty Earth Observatory and Department of Earth and Environmental Sciences Columbia University Palisades New York USA

7. Department of Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology Cambridge Massachusetts USA

8. Department of Environmental Studies Macalester College Saint Paul Minnesota USA

9. Department of Earth and Environmental Sciences University of Milano‐Bicocca Milano Italy

10. Department of Environmental Sciences Macquarie University Sydney New South Wales Australia

11. Climate Change Institute University of Maine Orono Maine USA

Funder

NSF

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL067911

Reference90 articles.

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5. Glacial–interglacial variability in the delivery of dust to the central equatorial Pacific Ocean

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