“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 209 — #232
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[17] Kaufman, A. J. et Xiao, S. H. (2003), « High CO 2 Levels in the Proterozoic Atmosphere Estimated from Analyses of Individual Microfossils »,
Nature, 425, pp. 279-282.
[18] Knauth, L. P. et Epstein, S. (1976), « Hydrogen and Oxygen Isotope
Ratios in Nodular and Bedded Cherts », Geochimica Cosmochimica Acta,
40, pp. 1 095-1 108.
[19] Kump, L. R., Kasting, J. F. et Barley, M. E. (2001), « Rise of Atmospheric Oxygen and the “Upside-Down” Archean Mantle », Geochemistry
Geophysics Geosystems, 2(1), doi: 10.1029/2000GC000114.
[20] Le Hir, G., Goddéris, Y., Ramstein, G. et Donnadieu, Y. (2007), « A
Scenario for the Evolution of the Atmospheric pCO 2 during a Snowball
Earth », Geology (in press).
[21] Lowe, D. R. et Tice, M. M. (2004), « Geologic Evidence for Archean
Atmospheric and Climatic Evolution: Fluctuating Levels of CO 2 , CH 4 ,
and O 2 with an Overriding Tectonic Control », Geology, 32(6), pp. 493496.
[22] McKay, C. P. (2000), « Thickness of Tropical Ice and Photosynthesis on
a Snowball Earth », Geophys. Res. Lett., 27, pp. 2 153-2 156.
[23] Papineau, D., Mojzsis, S. J. et Schmitt, A. K. (2007), « Multiple Sulfur
Isotopes from Paleoproterozoic Huronian Interglacial Sediments and the
Rise of Atmospheric Oxygen », Earth and Planetary Science Letters, 255,
pp. 188-212.
[24] Pavlov, A. A., Hurtgen, M. T., Kasting, J. F. et Arthur, M. A. (2003),
« Methane-Rich Proterozoic Atmosphere », Geology, 31, pp. 87-90.
[25] Pavlov, A. A., Kasting, J. F., Brown, L. L., Rages, K. A. et Freedman,
R. (2000), « Greenhouse Warming by CH 4 in the Atmosphere of Early
Earth », Journal of Geophysical Research, 105(E5), pp. 11 981-119 .
[26] Pierrehumbert, R. T. (2004), « High Levels of Atmospheric Carbon Dioxyde Necessary for the Termination of Global Glaciation », Nature, 429,
pp. 646-649.
[27] Pollard, D. et Kasting, J. F. (2005), « Snowball Earth: a Thin-Ice Solution
with Flowing Sea Glaciers », Journal of Geophysical Research, 111.
[28] Robert, F. et Chaussidon, M. (2006), « A Palaeotemperature Curve for
the Precambrian Oceans Based on Silicon Isotopes in Cherts », Nature,
443, pp. 969-972.
[29] Torsvik, T. H. et al. (2001), « Rodinia Refined or Obscured: Paleomagnetism of the Malani Igneous Suite (NW India) », Precamb. Res., 108,
pp. 319-333.
[30] Walker, J. C. G., Hays, P. B. et Kasting, J. F. (1981), « A Negative
Feedback Mechanism for the Long-Term Stabilization of Earth’s Surface
Temperature », Journal of Geophysical Research, 86, pp. 9 776-9 782.
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5. Le climat au Précambrien
209
[17] Kaufman, A. J. et Xiao, S. H. (2003), « High CO 2 Levels in the Proterozoic Atmosphere Estimated from Analyses of Individual Microfossils »,
Nature, 425, pp. 279-282.
[18] Knauth, L. P. et Epstein, S. (1976), « Hydrogen and Oxygen Isotope
Ratios in Nodular and Bedded Cherts », Geochimica Cosmochimica Acta,
40, pp. 1 095-1 108.
[19] Kump, L. R., Kasting, J. F. et Barley, M. E. (2001), « Rise of Atmospheric Oxygen and the “Upside-Down” Archean Mantle », Geochemistry
Geophysics Geosystems, 2(1), doi: 10.1029/2000GC000114.
[20] Le Hir, G., Goddéris, Y., Ramstein, G. et Donnadieu, Y. (2007), « A
Scenario for the Evolution of the Atmospheric pCO 2 during a Snowball
Earth », Geology (in press).
[21] Lowe, D. R. et Tice, M. M. (2004), « Geologic Evidence for Archean
Atmospheric and Climatic Evolution: Fluctuating Levels of CO 2 , CH 4 ,
and O 2 with an Overriding Tectonic Control », Geology, 32(6), pp. 493496.
[22] McKay, C. P. (2000), « Thickness of Tropical Ice and Photosynthesis on
a Snowball Earth », Geophys. Res. Lett., 27, pp. 2 153-2 156.
[23] Papineau, D., Mojzsis, S. J. et Schmitt, A. K. (2007), « Multiple Sulfur
Isotopes from Paleoproterozoic Huronian Interglacial Sediments and the
Rise of Atmospheric Oxygen », Earth and Planetary Science Letters, 255,
pp. 188-212.
[24] Pavlov, A. A., Hurtgen, M. T., Kasting, J. F. et Arthur, M. A. (2003),
« Methane-Rich Proterozoic Atmosphere », Geology, 31, pp. 87-90.
[25] Pavlov, A. A., Kasting, J. F., Brown, L. L., Rages, K. A. et Freedman,
R. (2000), « Greenhouse Warming by CH 4 in the Atmosphere of Early
Earth », Journal of Geophysical Research, 105(E5), pp. 11 981-119 .
[26] Pierrehumbert, R. T. (2004), « High Levels of Atmospheric Carbon Dioxyde Necessary for the Termination of Global Glaciation », Nature, 429,
pp. 646-649.
[27] Pollard, D. et Kasting, J. F. (2005), « Snowball Earth: a Thin-Ice Solution
with Flowing Sea Glaciers », Journal of Geophysical Research, 111.
[28] Robert, F. et Chaussidon, M. (2006), « A Palaeotemperature Curve for
the Precambrian Oceans Based on Silicon Isotopes in Cherts », Nature,
443, pp. 969-972.
[29] Torsvik, T. H. et al. (2001), « Rodinia Refined or Obscured: Paleomagnetism of the Malani Igneous Suite (NW India) », Precamb. Res., 108,
pp. 319-333.
[30] Walker, J. C. G., Hays, P. B. et Kasting, J. F. (1981), « A Negative
Feedback Mechanism for the Long-Term Stabilization of Earth’s Surface
Temperature », Journal of Geophysical Research, 86, pp. 9 776-9 782.