Glacial-interglacial sea surface temperature changes across the subtropical front east of New Zealand based on alkenone unsaturation ratios and foraminiferal assemblages-Reference-Cited by-同舟云学术

Glacial-interglacial sea surface temperature changes across the subtropical front east of New Zealand based on alkenone unsaturation ratios and foraminiferal assemblages

Published:2002-04-30 Issue:2 Volume:17 Page:2-1-2-13
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Sikes E. L.¹,Howard W. R.¹,Neil H. L.²,Volkman J. K.³

Affiliation:

1. Cooperative Research Centre for Antarctic and Southern Ocean Environment; Hobart Tasmania Australia

2. National Institute for Water and Atmosphere; Kilbirnie Wellington New Zealand

3. CSIRO Marine Research; Hobart Tasmania Australia

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference76 articles.

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3. Sea surface temperatures of the southwest Pacific Ocean during the Last Glacial Maximum;Barrows;Paleoceanography,2000

4. Subtropical Convergence fluctuations and Quaternary climates in the middle latitudes of the Indian Ocean;Bé;Science,1976

5. Southern Ocean fronts from the Greenwich meridian to Tasmania;Belkin;J. Geophys. Res.,1996

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