1 Prell, W.L., W.H. Hutson, D.F. Williams, A.W.H. Be', K. Geitzenauer, and B. Molfino, 1980. Surface circulation of the Indian Ocean during the last Glacial Maximum, approximately 18,000 yr. B.P. Quaternary Research 14: 309-336. 2 Pisias, N.G., D.G. Martinson, T.C. Moore Jr., N.J. Shackleton, W. Prell, J. Hays, and G. Boden, in press. High resolution stratigraphic correlation of benthic oxygen isotopic records spanning the last 300,000 years. 3 Hutson, W.H., and W.L. Prell, 1980. A paleoecological transfer function, FI-2, for Indian Ocean planktonic foraminifera. Journal of Paleontology 54 (2):381-399. 4 Van Campo, E., J.C. Duplessy, and M. Rossignol-Strick, 1982. Climatic conditions deduced from a 150-kyr. oxygen isotope-pollen record from the Arabian Sea. Nature 296:56-59. 5 Prell, W.L., 1984. Variation of monsoonal upwelling: a response to changing solar radiation. in "Climate processes and climate sensitivity." (J.E. Hansen and T. Takahashi, Eds.), pp. 48-57, M. Ewing Vol. 5, Geophysical Monograph 29, American Geophysical Union, Washington, D.C.. 6 Prell, W.L., 1984. Monsoonal climate of the Arabian Sea during the Late Quaternary: a response to changing solar radiation. in "Milankovitch and climate" (A. Berger and J. Imbrie, Eds.), pp. 349-366, D. Reidel Publishing Company, Dororecht, Holland. 7 Curry, W.B., and R.K. Matthews, 1981. Paleo-oceanographic utility of oxygen isotopic measurements on planktonic foraminifera: Indian Ocean core-top evidence. Palaeogeography, Palaeoclimatology, Palaeoecology 33:173-191. 8 Curry, W.B., and R.K. Matthews, 1981. Equilibrium 18-O fractionation in small size fraction planktic foraminifera: evidence from recent Indian Ocean sediments. Marine Micropaleontology 6:327-337. 9 Marvil, R., and W.L. Prell, 1984. unpublished data.