Boven, K.L., and Rea, D.K., 1998. Partitioning of hemipelagic and eolian sedimentation in Eastern Pacific core TR163-31B. J. Sediment. Res., 68:850–55.
Honjo, S., 1982. Seasonality and interaction of biogenic and lithogenic particulate flux at the Panama Basin. Science, 218:883–884.
Hovan, S.A., and Rea, D.K., 1992. Paleocene/Eocene boundary changes in atmospheric and oceanic circulation: a Southern Hemisphere record. Geology, 20:15–18. doi:10.1130/0091-7613(1992)020<0015:PEBCIA>2.3.CO;2
Janecek, T.R., and Rea, D.K., 1983. Eolian deposition in the northeast Pacific Ocean: Cenozoic history of atmospheric circulation. Geol. Soc. Am. Bull., 94:730–738.
Mehra, O.P., and Jackson, M.L., 1960. Iron oxide removal from soils and clays by a dithionite-citrate system buffered with sodium bicarbonate. Clays Clay Miner., 7:317–327.
Miller, K.G., Janecek, T.R., Katz, M.E., and Keil, D.J., 1987. Abyssal circulation and benthic foraminiferal changes near the Paleocene/Eocene boundary. Paleoceanography, 2:741–761.
Moore, T.C., Jr., Rabinowitz, P.D., et al., 1984. Init. Repts. DSDP, 74: Washington, D.C. (U.S. Govt. Printing Office).
Olivarez Lyle, A., and Lyle, M.W., 2002. Determination of biogenic opal in pelagic marine sediments: a simple method revisited. In Lyle, M., Wilson, P.A., Janecek, T.R., et al., Proc. ODP, Init. Repts., 199: College Station, TX (Ocean Drilling Program), 1–21. doi:10.2973/odp.proc.ir.199.106.2002
Poppe, L.J., Eliason, A.H., Fredericks, J.J., Rendigs, R.R., Blackwood, D.S., and Polloni, C.F., 2000. Grain-size analysis of marine sediments: methodology and data processing. In USGS East-Coast Sediment Analysis: Procedures, Database, and Georeferenced Displays. Open-File Rep.—U. S. Geol. Surv., 00-358. Available from world wide web: <http://pubs.usgs.gov/of/2000/of00-358/text/chapter1.htm>. [Cited 2005-09-09]
Rea, D.K., 1994. The paleoclimatic record provided by eolian deposition in the deep sea: the geologic history of wind. Rev. Geophys., 32(2):159–196. doi:10.1029/93RG03257
Rea, D.K., and Hovan, S.A., 1995. Grain size distribution and depositional processes of the mineral component of abyssal sediments: lessons from the North Pacific. Paleoceanography, 10(2):251–258. doi:10.1029/94PA03355
Rea, D.K., and Janecek, T.R., 1981. Mass-accumulation rates of the non-authigenic inorganic crystalline (eolian) component of deep-sea sediments from the western mid-Pacific Mountains, Deep Sea Drilling Project Site 463. In Theide, J., Vallier, T.L., et al., Init. Repts. DSDP, 62: Washington (U.S. Govt. Printing Office), 653–659.
Rea, D.K., Leinen, M., and Janecek, T.R., 1985. Geologic approach to the long-term history of atmospheric circulation. Science, 227:721–725.
Röhl, U., Bralower, T.J., Norris, R.D., and Wefer, G., 2000. New chronology for the late Paleocene thermal maximum and its environmental implications. Geology, 28(10):927–930. doi:10.1130/0091-7613(2000)028<0927:NCFTLP>2.3.CO;2
von der Borch, C.C., Sclater, J.G., et al., 1974. Init. Repts. DSDP, 22: Washington (U.S. Govt. Printing Office).
Zachos, J.C., Kroon, D., Blum, P., et al., 2004. Proc. ODP, Init. Repts., 208: College Station, TX (Ocean Drilling Program). doi:10.2973/odp.proc.ir.208.2004
Zachos, J.C., Röhl, U., Schellenberg, S.A., Sluijs, A., Hodell, D.A., Kelly, D.C., Thomas, E., Nicolo, M., Raffi, I., Lourens, L.J., McCarren, H., and Kroon, D., 2005. Rapid acidification of the ocean during the Paleocene–Eocene thermal maximum. Science, 308(5728):1611–1615. doi:10.1126/science.1109004