Abstract
The question addressed here is whether global chemical weathering and erosion rates have increased over Cenozoic time in response to uplift of the Himalayas.1–2 Chemical weathering of the continents is a process whereby carbonic acid (derived from the atmosphere or from soil respiration and decomposition) is consumed. Thus it represents a sink for atmospheric CO2 and provides one link between uplift and climate change. The prevailing hypothesis concerning the cause of the long-term cooling of Cenozoic climates states that as a result of increased rates of silicate weathering, atmospheric CO2 levels have fallen, the magnitude of the greenhouse effect has been reduced, and thus the globally averaged climate has cooled. Such a scenario is consistent with the secular record of seawater Sr isotopic composition preserved in carbonates1,3–6 (Fig. la), which becomes increasingly radiogenic with time through the Cenozoic. This trend implies a growing influence of continental weathering, relative to seafloor hydrothermal activity, on the Sr isotopic composition of seawater.7
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Raymo, M. E., Ruddiman, W. F., and Froelich, P. N. (1988). Geology 16, p. 649.
Raymo, M. E. (1989). Geology 19, p. 344.
Hodeil, D. A., Mueller, P. A, McKenzie, J. A., and Mead, G. A. (1989). Earth Planet. Sci. Lett. 92, p. 165.
Hodell, D. A., Mead, G. A., and Mueller, P. A. (1990). Chem. Geol. 80, p. 1.
Capo, R. C., and DePaolo, D. J. (1990). Science 249, p. 51.
Richter, F. M., Rowley, D. B., and DePaolo, D. J. (1992). Earth Planet. Sci. Lett. 109, p. 11.
Brass, G. W. (1976). Geochim. Cosmochim. Acta 40, p. 721.
Caldeira, K., Arthur, M. A., Berner, R. A., and Lasaga, A. C. (1993). Nature 361, p. 123.
Volk, T. (1993). Nature 361, p. 123.
Walker, J. C. G., Hays, P. B., and Kasting, J. F. (1981). J.Geophys. Res. 86, p. 9776.
Berner, R. A., Lasaga, A. C., and Garrels, R. M. (1983). Am. J. Sci. 283, p. 641.
François, L. M., and Walker, J. C. G. (1992). Am. J. Sci. 292, p. 81.
Gibbs, M., and Kump, L. R. (1994). Paleoceanography 9, p. 529.
Kominz, M. A. (1984). Am. Assoc. Pet. Geol. Mem. 36, p. 109.
Larson, R. L. (1991). Geology 19, p. 547.
Engebretson, D. C., Kelley, K. P., Cashman, H. J., and Richards, M. A. (1992). GSA Today 2, p. 93.
Caldeira, K. (1992). Nature 357, p. 578.
Kerrick, D. M., and Caldeira, K. (1993). Chem. Geol. 108, p. 201.
Beck, R. A., Burbank, D. W., Sercombe, W. J., Olson, T. L., and Khan, A. M. (1995). Geology 23, p. 387.
Caldeira, K. (1995). Am. J. Sci. 295, p. 1077.
Palmer, M. R., and Elderfield, H. (1985). Nature 314, p. 526.
Kump, L. R. (1989). Am. J. Sci. 289, p. 390.
Berner, R. A., and Rye, D. (1992). Am. J. Sci. 292, p. 136.
Berner, R. A. (1991). Am. J. Sci. 291, p. 339.
Goddéris, Y. and François, L. M. (1995). Chem. Geol. 126, p. 169.
Veizer, J. (1989). Ann. Rev. Earth Planet. Sci. 17, p. 141.
Graham, D. W., Bender, M. L., Williams, D. F., and Keigwin, L. D. Jr. (1982). Geochim. Cosmochim. Acta 46, p. 1281.
Chaudhuri, S., and Clauer, N. (1986). Chem. Geol. 59, p. 293.
Holland, H. D. (1978). The Chemistry of the Atmosphere and Oceans, Wiley-Interscience, New York.
Blatt, H., and Jones, R. L. (1975). Geol. Soc. Am. Bull. 86, p. 1085.
Meybeck, M. (1987). Am. J. Sci. 287, p. 401.
Faure, G. (1986). Principles of Isotope Geology. John Wiley, New York.
Edmond, J. M., Measures, C., McDuff, R. E., Chan, L. H, Collier, R., Grant, B., Gordon, L. J., and Corliss, J. B. (1979). Earth Planet. Sci. Lett. 46, p. 1.
Albarede, F., Michard, A., Monster, J. F., and Michard, G. (1981). Earth Planet. Sci. Lett. 55, p. 229.
Berner, R. A. (1994). Am. J. Sci. 294, p. 56.
Barron, E. J., Sloan, J. L. II, and Harrison, C. G. A. (1980). Palaeogeogr. Palaeoclim. Palaeoecol. 30, p. 17.
Bluth, G. J. S. (1990). Effects of Paleogeology, Chemical Weathering, and Climate on the Global Geochemical Cycle of Carbon Dioxide. Ph.D. Dissertation, Pennsylvania State University, University Park, Pennsylvania.
Bluth, G. J. S., and Kump, L. R. (1991). Am. J. Sci. 291, p. 284.
Bickle, M. J. (1994). Nature 367, p. 699.
Scotese, C. R., Gahagan, L. M., and Larson, R. L. (1988). Tectonophysics 155, p. 27.
Gaffin, S. R. (1987). Am. J. Sci. 287, p. 596.
Arthur, M. A., Dean, W. E., and Claypool, G. E. (1985). Nature 315, p. 216.
Dean, W. E., Arthur, M. A., and Claypool, G. E. (1986). Mar. Geol. 70, p. 119.
Popp, B. N., Takigiku, T., Hayes, J. M., Louda, J. W., and Baker, E. W. (1989). Am. J. Sci. 289, p. 436.
Rau, G. H., Takahashi, T., and Des Marais, D. J. (1898). Nature 341, p. 516.
Rau, G. H., Froelich, P. N., Takahashi, T., and Des Marais, D. J. (1991). Paleoceanography 6, p. 335.
Laws, E. A., Popp, B. N., Bidigare, R. R, Kennicutt, M. C., and Macko, S. A. (1995). Geochim. Cosmochim. Acta 59, p. 1131.
Lasaga, A. C., Berner, R. A., and Garrels, R. M. (1985). In: The Carbon Cycle and Atmospheric CO 2: Natural Variations Archean to Present, (E. T. Sundquist and W. S. Broecker, eds.), pp. 397–411. American Geophysical Union, Washington, D.C.
Volk, T. (1987). Am. J. Sci. 287, p. 763.
Edmond, J. M., Palmer, M. R., Measures, C. I., Grant, B., and Stallard, R. F. (1995). Geochim. Cosmochim. Acta 59, p. 3301.
Davies, T. A., and Worsley, T. R. (1981). Soc. Econ. Paleont. Mineral. Spec. Pub. 32, p. 169.
Delaney, M. L., and Boyle, E. A. (1988). Paleoceanography 3, p. 137.
Opdyke, B. N., and Wilkinson, B. H. (1988). Paleoceanography 3, p. 685.
Milliman, J. D. (1993). Global Biogeochem. Cycles 7, p. 927.
Broecker, W. S., and Peng, T. S. (1982). Tracers in the Sea. Lamont-Doherty Geological Observatory, New York.
Berner, E. K., and Berner, R. A. (1987). The Global Water Cycle: Geochemistry and Environment. Prentice-Hall, Englewood Cliffs, NJ.
Morse, J. W., and Mackenzie, F. T. (1990). Geochemistry of Sedimentary Carbonates. Elsevier, Amsterdam.
Raymo, M. E., and Ruddiman, W. F. (1992). Nature 359, p. 117.
Derry, L. A., and France-Lanord, C. (1996). Paleoceanography 11, p. 267.
Delaney, M. L., and Filippelli, G. M. (1994). Paleoceanography 9, p. 513.
Filippelli, G. M., and Delaney, M. L. (1994). Paleoceanography 9, p. 643.
Palmer, M. R., and Edmond, J. (1992). Geochim. Cosmochim. Acta 56, p. 2099.
Derry, L. A., and France-Lanord, C. (1996). Earth Planet. Sci. Lett. 142, p. 59.
Barron, E. J. (1985). Palaeogeogr. Palaeoclim. Palaeoecol. 50, p. 729.
Barron, E. J., and Washington, W. M. (1985). In: The Carbon Cycle and Atmospheric CO2: Natural Variations Archean to Present (E. T. Sundquist and W. S. Broeker, eds.), pp. 546–553. American Geophysical Union, Washington, D.C.
Freeman, K. H., and Hayes, J. M. (1992). Global Biogeochem. Cycles 6, p. 185.
Drever, J. I., and Zobrist, J. (1992). Geochim. Cosmochim. Acta 56, p. 3209.
Armstrong, R. E. (1971) Nature Phys. Sci. 230, p. 132.
Kump, L. R., and Alley, R. B. (1994). In: Material Fluxes on the Surface of the Earth (Board on Earth Sciences, ed.), pp. 46–60. National Academy Sciences, Washington, D.C.
Berner, R. A. (1992). Geochim. Cosmochim. Acta 56, p. 3225.
Schwartzmann, D. W., and Volk, T. (1989). Nature 340, p. 457.
Kump, L. R., and Volk, T. (1991). In: Scientists on Gaia (S. H. Schneider and P. J. Boston, eds.), pp. 191–199. MIT Press, Cambridge, Mass.
Stallard, R. F., and Edmond, J. M. (1983). J. Geophys. Res. 88, p. 9671.
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1997 Springer Science+Business Media New York
About this chapter
Cite this chapter
Kump, L.R., Arthur, M.A. (1997). Global Chemical Erosion during the Cenozoic: Weatherability Balances the Budgets. In: Ruddiman, W.F. (eds) Tectonic Uplift and Climate Change. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-5935-1_18
Download citation
DOI: https://doi.org/10.1007/978-1-4615-5935-1_18
Publisher Name: Springer, Boston, MA
Print ISBN: 978-1-4613-7719-1
Online ISBN: 978-1-4615-5935-1
eBook Packages: Springer Book Archive