Reduced North Atlantic Deep Water flux to the glacial Southern Ocean inferred from neodymium isotope ratios-Reference-Cited by-同舟云学术

Reduced North Atlantic Deep Water flux to the glacial Southern Ocean inferred from neodymium isotope ratios

Published:2000-06 Issue:6789 Volume:405 Page:935-938
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Rutberg Randye L.,Hemming Sidney R.,Goldstein Steven L.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/35016049.pdf

Reference34 articles.

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2. Curry, W. B. & Lohmann, G. P. Reduced advection into Atlantic Ocean deep eastern basins during last glaciation maximum. Nature 308, 317–342 ( 1983).

3. Oppo, D. W. & Fairbanks, R. G. Variability in the deep and intermediate water circulation of the Atlantic Ocean during the past 25,000 years: Northern Hemisphere modulation of the Southern Ocean. Earth Planet. Sci. Lett. 86, 1–15 (1987).

4. Charles, C. D. & Fairbanks, R. G. Evidence from Southern Ocean sediments for the effect of North Atlantic deep-water flux on climate. Nature 355, 416–419 ( 1992).

5. Labeyrie, L. et al. Hydrographic changes of the Southern Ocean (southeast Indian sector) over the last 230 kyr. Paleoceanography 11, 57–76 (1996).

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