Close mass balance of long-term carbon fluxes from ice-core CO2 and ocean chemistry records

Nature Geoscience

Volumn 1, Issue 5, 2008, Pages 312-315

  Zeebe, Richard E ^a   Caldeira, Ken ^b  

^a UNIVERSITY OF HAWAII   (United States)

^b GEOPHYSICAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 55849094669     PISSN: 17520894     EISSN: 17520908     Source Type: Journal    
DOI: 10.1038/ngeo185     Document Type: Article

References (27)

1. Walker, J. C. G., Hays, P. B. & Kasting, J. F. Negative feedback mechanism for the long-term stabilization of earth's surface temperature. J. Geophys. Res. 86, 9776-9782 (1981).
2. Berner, R. A., Lasaga, A. C. & Garrels, R. M. The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years. Am. J. Sci. 283, 641-683 (1983).
3. Caldeira, K. Enhanced Cenozoic chemical weathering and the subduction of pelagic carbonate. Nature 357, 578-581 (1992).
4. Volk, T. Cooling in the late Cenozoic. Nature 361, 123 (1993).
5. Raymo, M. E., Ruddiman, W. F. & Froelich, P. N. Influence of late Cenozoic mountain building on ocean geochemical cycles. Geology 16, 649-653 (1988).
6. 86Sr isotopic ratio of seawater. Am. J. Sci. 292, 81-135 (1992).
7. Bickle, M. J. Metamorphic decarbonation, silicate weathering and the long-term carbon cycle. Terra Nova 8, 270-276(1996).
8. McCauley, S. E. & DePaolo, D. J. in Tectonic Uplift and Climate Change (ed. Ruddiman, W F.) 428-465 (Plenum, New York, 1997).
9. 2. Earth Planet. Sci. Lett. 216, 125-139 (2003).
10. Petit, J. R. et al. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399, 429-436 (1999).
11. 2 around the last three glacial terminations. Science 283, 1712-1714 (1999).
12. Siegenthaler, U. et al. Stable carbon cycle-climate relationship during the Late Pleistocene. Science 310, 1313-1317 (2005).
13. Walker, J. C. G. & Kasting, J. F. Effects of fuel and forest conservation on future levels of atmospheric carbon dioxide. Palaeogeogr. Palaeoclimatol. Palaeoecol. 97, 151-189 (1992).
14. Key, R. M. et al. A global ocean carbon climatology: Results from GLODAP. Glob. Biogeochem. Cycles 18, GB4031 (2004).
15. 86Sr ratio of seawater. Earth Planet. Sci. Lett. 188, 459-474 (2001).
16. 2 over Phanerozoic time. Am. J. Sci. 291, 339-376 (1991).
17. 2. Quat. Sci. Rev. 10, 283-296 (1991).
18. Kasting, J. F. & Catling, D. Evolution of a habitable planet. Annu. Rev. Astron. Astrophys. 41, 429-63 (2003).
19. Berner, R.A.& Caldeira, K. The need for mass balance and feedback in the geochemical carbon cycle. Geology 25, 955-956 (1997).
20. 2 police the rate of chemical weathering? Glob. Biogeochem. Cycles 12, 403-408 (1998).
21. 2 in Seawater: Equilibrium, Kinetics, Isotopes 346pp (Elsevier Oceanography Series, Elsevier, Amsterdam, 2001).
22. 2 change. Glob. Biogeochem. Cycles 1, 5-29 (1987).
23. 3 saturation state of the ocean: The 'Strangelove', the 'Neritan', and the 'Cretan' Ocean. Geochem. Geophys. Geosyst. 4, 1104 (2003).
24. 3 preservation: An 800,000 year bathymetric reconstruction from the central equatorial Pacific Ocean. Paleoceanography 4, 447-466 (1989).
25. Zachos, J. C., Dickens, G. R. & Zeebe, R. E. An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature 451, 279-283 (2008).
26. 3 flux variations and their uncertainties. Glob. Planet. Change 33, 155-176(2002).
27. Foster, G. L. & Vance, D. Negligible glacial-interglacial variation in continental chemical weathering rates. Nature 444, 918-921 (2006).