Hostname: page-component-77c89778f8-vsgnj Total loading time: 0 Render date: 2024-07-17T06:38:28.133Z Has data issue: false hasContentIssue false

Reply to Comments by P. J. Webster and N. A. Streten Regarding “Surface Circulation of the Indian Ocean during the Last Glacial Maximum, Approximately 18,000 YBP”

Published online by Cambridge University Press:  20 January 2017

Warren L. Prell*
Affiliation:
Department of Geological Sciences, Brown University Providence, Rhode Island 02912

Abstract

Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Letters to the Editor
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.)

References

CLIMAP Project Members, . 1976. The surface of the ice-age Earth. Science 191, 11311137.Google Scholar
Coulbourn, W.T. Parker, F.L. Berger, W.H. (1980). Faunal and solution patterns of planktonic foraminifera in surface sediments of the North Pacific. Marine Micropaleontology 5, 329399.Google Scholar
Epstein, S. Buchsbaum, R. Lowenstam, H. Urey, H.C. (1953). Revised carbonate-water isotopic temperature scale. Bulletin of the Geological Society of America 64, 13151326.Google Scholar
Hutson, W.H. Prell, W.L. (1980). A paleoecological transfer function, FI-2, for Indian Ocean planktonic foraminifera. Journal of Paleontology 54, 381399.Google Scholar
Imbrie, J. Kipp, N.G. (1971). A new micropaleontological method for quantitative paleoclimatology: Application to a late Pleistocene Caribbean core. The Late Cenozoic Glacial Ages Turekian, K.K. Yale University Press. New Haven, Conn. 71181.Google Scholar
Kipp, N.G. (1976). New transfer function for estimating past sea-surface conditions from sea-bed distributions of planktonic foraminiferal assemblages in the North Atlantic. Investigation of Late Quaternary Paleoceanography and Paleoclimatology Cline, R.M. Hays, J.D.Geological Society of America Memoir 145, 341.Google Scholar
Moore, T.C. Jr.. 1978. The distribution of radiolarian assemblages in the modern and ice-age Pacific. Marine Micropaleontology 3, 229266.Google Scholar
Moore, T.C. Jr., Burckle, L.H. Geitzenauer, K. Luz, B. Molina-Cruz, A. Robertson, J.H. Sachs, H. Sancetta, C. Thiede, J. Thompson, P. Wenkam, C. (1980). The reconstruction of sea surface temperatures in the Pacific Ocean of 18,000 B. P.. Marine Micropaleontology 5, 215247.CrossRefGoogle Scholar
Prell, W.L. Hutson, W.H. Williams, D.F. Be, A.W.H. 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, 309336.CrossRefGoogle Scholar
Thompson, P.R. (1981). Planktonic foraminifera evidence of circulation in the western North Pacific during the past 150,000 years: Comparison of modern and fossil assemblages. Palaeogeography, Palaeoecology, Palaeoclimatology(in press).Google Scholar
Webster, P.J. Streten, N.A. (1978). Late Quaternary ice age climates of tropical Australasia: Interpretations and reconstructions. Quaternary Research 10, 279309.Google Scholar