REFERENCES

Berggren, W.A., Kent, D.V., Swisher, C.C., III, and Aubry, M.-P., 1995. A revised Cenozoic geochronology and chronostratigraphy. In Berggren, W.A., Kent, D.V., Aubry, M.-P., and Hardenbol, J. (Eds.), Geochronology, Time Scales and Global Stratigraphic Correlation. Spec. Publ.—SEPM, 54:129-212.

Berner, R.A., 1980. Early Diagenesis: A Theoretical Approach: Princeton, NJ (Princeton Univ. Press).

Borowski, W.S., Paull, C.K., and Ussler, W., III, 1996. Marine pore-water sulfate profiles indicate in situ methane flux from underlying gas hydrate. Geology, 24:655-658.

Clague, D., Maher, N., and Paull, C.K., 2001. High-resolution multibeam survey of Hydrate Ridge, offshore Oregon. In Paull, C.K., and Dillon, W.P. (Eds), Natural Gas Hydrates: Occurrence, Distribution, and Detection. Am. Geophys. Union, Geophys. Monogr. Ser., 124:297-306.

Collett, T.S., and Ladd, J., 2000. Detection of gas hydrate with downhole logs and assessment of gas hydrate concentrations (saturations) and gas volumes on the Blake Ridge with electrical resistivity log data. In Paull, C.K., Matsumoto, R., Wallace, P.J., and Dillon, W.P. (Eds.), Proc. ODP, Sci. Results, 164: College Station, TX (Ocean Drilling Program), 179-191. [HTML version]

Deyhle, A., Kopf, A., and Eisenhauer A., 2001. Boron systematics of authigenic carbonates: anew approach to identify fluid processes in accretionary prisms. Earth Planet. Sci. Lett., 187:191-205.

Duan, Z., Møller, N., Greenberg, J., and Weare, J.H., 1992. The prediction of methane solubility in natural waters to high ionic strengths from 0° to 250°C and from 0 to 1600 bar. Geochim. Cosmochim. Acta, 56:1451-1460.

Duncan, J.R., Fowler, G.A., and Kulm, L., 1970. Planktonic foraminiferal-radiolarian ratios and Holocene-late Pleistocene deep sea stratigraphy off Oregon. Geol. Soc. Am. Bull., 81:561-566.

Goldhaber, M.B., and Kaplan, I.R., 1974. The sulfur cycle. In Goldberg, E.D. (Ed.), The Sea (Vol. 5): Marine Chemistry: The Sedimentary Cycle: New York (Wiley-Interscience), 569-655.

Handa, Y.P., 1990. Effect of hydrostatic pressure and salinity on the stability of gas hydrates. J. Phys. Chem., 94:2652-2657.

Kastner, M., Kvenvolden, K.A., Whiticar, M.J., Camerlenghi, A., and Lorenson, T.D., 1995. Relation between pore fluid chemistry and gas hydrates associated with bottom-simulating reflectors at the Cascadia margin, Sites 889 and 892. In Carson, B., Westbrook, G.K., Musgrave, R.J., and Suess, E. (Eds.), Proc. ODP, Sci. Results, 146 (Pt. 1): College Station, TX (Ocean Drilling Program), 175-187.

Kitano, Y., Okumaura, M., and Idogak, M., 1978. Uptake of phosphate ions by calcium carbonate. Geochem. J., 12:29-37.

Odin, G.S., and Matter, A., 1981. Die glauconarium origine. Sedimentology, 28:611-643.

Paull, C.K., Matsumoto, R., Wallace, P.J., et al., 1996. Proc. ODP, Init. Repts., 164: College Station, TX (Ocean Drilling Program). [HTML version]

Rothwell, R.G., Thomson, J., and Kahler, G., 1998. Low-sea-level emplacement of a very large late Pleistocene megaturbidite in the western Mediterranean Sea. Nature, 392:377-380.

Spivack, A.J., and You, C.F., 1997. Boron isotopic geochemistry of carbonates and pore waters, Ocean Drilling Program Site 851. Earth Planet. Sci. Lett., 152:113-122.

You, C.-F., Spivack, A.J., Gieskes, J.M., Martin, J.B., and Davisson, M.L., 1996. Boron contents and isotopic compositions in pore waters: a new approach to determine temperature induced artifacts-geochemical implications. Mar. Geol., 129:351-361.