REFERENCES

Baker, P.A., Gieskes, J.M., and Elderfield, H., 1982. Diagenesis of carbonates in deep-sea sediments—evidence from Sr2+/Ca2+ ratios and interstitial dissolved Sr2+ data. J. Sediment. Petrol., 52:71–82.

Burton, J.D., 1996. The ocean: a global geochemical system. In Summerhayes, C.P., and Thorpe, S.A. (Eds.), Oceanography: An Illustrated Guide: London (Manson Publishing Ltd.), 166.

Cande, S.C., and Kent, D.V., 1995. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic. J. Geophys. Res., 100:6093–6095.

Clark, M.W., and Wright, R.C., 1984. Paleogene abyssal foraminifers from the Cape and Angola basins, South Atlantic Ocean: DSDP 73. In Hsü, K.J., LaBrecque, J.L., et al., Init. Repts. DSDP, 73: Washington (U.S. Govt. Printing Office), 459–480.

Deyhle, A., and Kopf, A., 2002. Strong B-enrichment and anomalous boron isotope geochemistry in the Japan forearc. Mar. Geol., 183:1–15.

Gieskes, J.M., 1981. Deep-sea drilling interstitial water studies: implications for chemical alteration of the oceanic crust, layers I and II. In Warme, J.E., Douglas, R.G., and Winterer, E.L. (Eds.), The Deep Sea Drilling Project: A Decade of Progress. Spec. Publ.—Soc. Econ. Paleontol. Mineral., 32:149–167.

Gieskes, J.M., Johnston, K., and Boehm, M., 1984. Interstitial water studies, Leg 74. In Moore, T.C., Rabinowitz, P.D., et al., Init. Repts. DSDP, 74: Washington (U.S. Govt. Printing Office), 701–711.

James, R.H., Allen, D.E., and Seyfried, W.E., Jr., 2003. An experimental study of alteration of oceanic crust and terrigenous sediments at moderate temperatures (51 to 350°C): insights as to chemical processes in near-shore ridge-flank hydrothermal systems. Geochim. Cosmochim. Acta, 67:681–691.

Lourens, L.J., Hilgen, F.J., Laskar, J., Shackleton, N.J., and Wilson, D., in press. The Neogene period. In Gradstein, F.M., Ogg, J., and Smith, A.G. (Eds.), A Geological Time Scale 2004: Cambridge (Cambridge Univ. Press).

Malone, M.J., Claypool, G., Martin, J.B., and Dickens, G.R., 2002. Variable methane fluxes in shallow marine systems over geologic time: the composition of pore waters and authigenic carbonates on the New Jersey shelf. Mar. Geol., 189:175–196.

Moore, T.C., Jr., Rabinowitz, P.D., et al., 1984. Init. Repts. DSDP, 74: Washington, D.C. (U.S. Govt. Printing Office).

Müller-Merz, E., and Oberhänsli, H., 1991. Eocene bathyal and abyssal benthic foraminifera from a South Atlantic transect at 20–30° S. Palaeogeogr., Palaeoclimatol., Palaeoecol., 83:117–171.

Olafsson, G., and Villa, G., 1992. Reliability of sphenoliths as zonal markers in Oligocene sediments from the Atlantic and Indian Oceans. In Proto Decima, F., Monechi, S., and Rio, D. (Eds.), Proc. Int. Nannoplankton Assoc. Conf., Firenze 1989. Mem. Sci. Geol., 43:261–275.

Parker, R.L., and Gee, J.S., 2002. Calibration of the pass-through magnetometer—II. Application. Geophys. J. Int., 150:140–152.

Schmiedl, G., Mackensen, A., and Müller, P.J., 1997. Recent benthic foraminifera from the eastern South Atlantic Ocean: dependence on food supply and water masses. Mar. Micropaleontol., 32:259–287.

Thomas, E., and Shackleton, N., 1996. The Palaeocene–Eocene benthic foraminiferal extinction and stable isotope anomalies. In Knox, R.W.O'B., Corfield, R.M., and Dunay, R.E. (Eds.), Correlation of the Early Paleogene in Northwest Europe. Geol. Soc. Spec. Publ., 101:401–441.

Tjalsma, R.C., 1983. Eocene to Miocene benthic foraminifers from DSDP Site 516, Rio Grande Rise, South Atlantic. In Barker, P.F., Carlson, R.L., Johnson, D.A., et al., Init. Repts. DSDP, 72: Washington (U.S. Govt. Printing Office), 731–756.