Hostname: page-component-76c49bb84f-ndtt8 Total loading time: 0 Render date: 2025-07-13T01:20:53.787Z Has data issue: false hasContentIssue false
  • English
  • Français

Comments on: “Surface Circulation of the Indian Ocean during the Last Glacial Maximum Approximately 18,000 yr B.P.” by Warren L. Prell et al.

Published online by Cambridge University Press:  20 January 2017

Peter J. Webster  and
Neil A. Streten
Peter J. Webster
Affiliation:
CSIRO Division of Atmospheric Physics Aspendale, Victoria 3195, Australia
Neil A. Streten
Affiliation:
Australian Numerical Meteorology Research Centre Melbourne, Victoria 3000, Australia
Get access Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'

Information

Type
Letters to the Editor
Information
Quaternary Research , Volume 16 , Issue 3 , November 1981 , pp. 421 - 423
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

References

Aharon, P. 1981. Surface ocean temperature variations during the late Wisconsin stages 180/160 isotopic evidence from coral reef terraces in eastern New Guinea. In “Proceedings of the CLIMANZ Conference Australian Academy of Science Canberra(in press)Google Scholar
Bowler, J.M., Hope, G.S., Jennings, J.N., Singh, G., Walker, D. 1976. Late Quaternary climates of Australia and New Guinea. Quaternary Research 6. 359–399.Google Scholar
CLIMAP. 1976. The surface of the ice-age Earth. Science 191. 1131–1137.Google Scholar
Prell, W.L., Hutson, W.H., Williams, D.F., Bé, A.W., Geitzenauer, K., Molfino, B. 1980. Surface circulation of the Indian Ocean during the last glacial maximum, approximately 18,000 yr B.P.. Quaternary Research 14. 309–336.CrossRefGoogle Scholar
Shackleton, N.J., Opdyke, N.D. 1976. Oxygen-isotope and paleomagnetic stratigraphy of Pacific Core V28–239 Late Pleocene to Latest Pleistocene. Geological Society of America Memoirs 145. 449–464.Google Scholar
Webster, P.J., Streten, N.A. 1978. Late Quaternary ice age climates of tropical Australasia: Interpretations and reconstructions. Quaternary Research 10. 279–309.Google Scholar