Ocean currents generate large footprints in marine palaeoclimate proxies-Reference-Cited by-同舟云学术

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Ocean currents generate large footprints in marine palaeoclimate proxies

Published:2015-03-04 Issue:1 Volume:6 Page:
ISSN:2041-1723
Container-title:Nature Communications
language:en
Short-container-title:Nat Commun

Author:

van Sebille Erik,Scussolini Paolo,Durgadoo Jonathan V.,Peeters Frank J. C.,Biastoch Arne,Weijer Wilbert,Turney Chris,Paris Claire B.,Zahn Rainer

Publisher

Springer Science and Business Media LLC

Subject

General Physics and Astronomy,General Biochemistry, Genetics and Molecular Biology,General Chemistry

Link

http://www.nature.com/articles/ncomms7521.pdf

Reference42 articles.

1. Katz, M. E. et al. Traditional and emerging geochemical proxies in foraminifera. J. Foraminiferal Res. 40, 165–192 (2010) .

2. Ganssen, G. M. et al. Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years. Clim. Past 7, 1337–1349 (2011) .

3. Emiliani, C. Pleistocene temperatures. J. Geol. 63, 538–578 (1955) .

4. Mix, A. C., Ruddiman, W. F. & McIntyre, A. Late quaternary paleoceanography of the Tropical Atlantic, 1: spatial variability of annual mean sea-surface temperatures, 0-20,000 years B.P. Paleoceanography 1, 43–66 (1986) .

5. Peeters, F. J. C. et al. Vigorous exchange between the Indian and Atlantic oceans at the end of the past five glacial periods. Nature 430, 661–665 (2004) .

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