Muerdter, D. R., J. P. Kennett, and R. C. Thunell (1984). Late Quaternary sapropel sediments in the eastern Mediterranean Sea: Faunal variations and chronology, Quaternary Research 21, 385-403.

Oeschger, H., M. Welten, U. Eicher, M. Möll, T. Riesen, U. Siegenthaler, and S. Wegmüiller (1980). ¹⁴C and other parameters during the Younger Dryas cold phase, Radiocarbon 22, 299-310.

Oglesby, R. J., K. A. Maasch, and B. Saltzman (1989). Glacial meltwater cooling of the Gulf of Mexico: GCM implications for Holocene and present-day climates, Climate Dynamics 3, 115-133.

Overpeck, J. T., L. C. Peterson, N. Kipp, J. Imbrie, and D. Rind (1989). Climate change in the circum-North Atlantic region during the last deglaciation, Nature 338, 553-557.

Pedersen, T. F., M. Pickering, J. S. Vogel, J. N. Southon, and D. E. Nelson (1988). The response of benthic foraminifera to productivity cycles in the eastern equatorial Pacific: Faunal and geochemical constraints on glacial bottom water oxygen levels , Paleoceanography 3, 157-168.

Prest, V. K. (1970). Quaternary geology, in Geology and Economic Minerals of Canada, R. J. W. Douglas, ed., Department of Energy, Mines and Resources, Ottawa, pp. 675-764.

Prest, V. K., D. R. Grant, and V. N. Rampton (1968). Glacial Map of Canada, Map 1253A, Geological Survey of Canada, Ottawa.

Ruddiman, W. F. (1969). Planktonic foraminifera of the subtropical North Atlantic gyre, Ph.D. thesis, Columbia University, New York, 291 pp.

Ruddiman, W. F., and A. McIntyre (1981). The mode and mechanism of the last deglaciaton: Oceanic evidence, Quaternary Research 16, 125-134.

Sancetta, C. (1979). Oceanography of the North Pacific during the last 18,000 years: Evidence from fossil diatoms, Marine Micropaleontology 4, 103-123.

Shackleton, N. J. (1977). The oxygen isotopic stratigraphic record of the late Pleistocene, Philosophical Transactions of the Royal Society of London 280, 169-182.

Sidner, B. R., and C. W. Poag (1972). Late Quaternary climates indicated by foraminifers from the southwestern Gulf of Mexico, Gulf Coast Association of Geological Societies Transactions 22, 305-313.

Spero, H. J., and M. J. DeNiro (1987). The influence of symbiont photosynthesis on the d¹⁸O and d¹³C values of planktonic foraminiferal shell calcite, Symbiosis 4, 213-228.

Spero, H. J., and D. F. Williams (1988). Extracting environmental information from planktonic foraminiferal d¹³C data, Nature 335, 717-719.

Spero, H. J., and D. F. Williams (1990). Evidence for low-salinity surface waters in the Gulf of Mexico over the last 16,000 years, Paleoceanography 5, 963-975.

Thunell, R. C. (1976). Calcium carbonate dissolution history in late Quaternary deep-sea sediments, Western Gulf of Mexico, Journal of Quaternary Research 6, 281-297.

Thunell, R. C. (1978). Distribution of Recent planktonic foraminifera in surface sediments of the Mediterranean Sea, Marine Micropaleontology 3, 147-173.

Thunell, R. C., D. F. Williams, and J. P. Kennett (1977). Late Quaternary paleoclimatology, stratigraphy and sapropel history in eastern Mediterranean deep-sea sediments , Marine Micropaleontology 2, 371-388.

Thunell, R. C., W. B. Curry, and S. Honjo (1983a). Seasonal variation in the flux of planktonic foraminifera: Time series trap results from the Panama Basin, Earth and Planetary Science Letters 64, 44-55.

Thunell, R. C., W. B. Curry, and S. Honjo (1983b). Seasonal changes in the isotopic composition of planktonic foraminifera collected in Panama Basin sediment traps, Earth and Planetary Science Letters 64, 33-43.

Tolderlund, D. S., and A. W. H. Bé (1971). Seasonal distribution of planktonic foraminifera in the western North Atlantic, Micropaleontology 17, 297-329.