“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 208 — #231
i
i
i
i
i
i
i
i
208
Paléoclimatologie
[2] Caldeira, K. et Kasting, J. F. (1992), « Susceptibility of the Early Earth
to Irreversible Glaciation Caused by Carbon Dioxide Clouds », Nature,
359, pp. 226-228.
[3] Catling, D. C. et Claire, M. W. (2005)„ « How Earth’s Atmosphere Evolved to an Oxic State: A Status Report », Earth and Planetary Science
Letters, 237, pp. 1-20.
[4] Donnadieu, Y., Fluteau, F., Ramstein, G., Ritz, C. et Besse, J. (2003),
« Is there a Conflict between the Neoproterozoic Glacial Deposits and the
Snowball Earth Interpretation: an Improved Understanding with Numerical Modeling », Earth and Planetary Science Letters, 208, pp. 101-112.
[5] Donnadieu, Y., Goddéris, Y., Ramstein, G., Nédelec, A. et Meert, J. G.
(2004), « Snowball Earth Triggered by Continental Break-Up through
Changes in Runoff », Nature, 428, pp. 303-306.
[6] Evans, D. A. D. (2000), « Stratigraphic, Geochronological, and Paleomagnetic Constraints upon the Neoproterozoic Climatic Paradox », American Journal of Science, 300, pp. 347-433.
[7] François, L. M. et Goddéris, Y. (1998), « Isotopic Constraints on the Cenozoic Evolution of the Carbon Cycle », Chemical Geology, 145, pp. 177212.
[8] Gaucher, E. A., Govindarajan, S. et Ganesh, O. K. (2008) ; « Palaeotemperature Trend for Precambrian Life Inferred from Resurrected Proteins », Nature, 451, pp. 704-708.
[9] Goddéris, Y. et al. (2003), « The Sturtian Glaciation: Fire and Ice »,
Earth and Planetary Science Letters, 211, pp. 1-12.
[10] Goddéris, Y. et Veizer, J. (2000), « Tectonic Control of Chemical and
Isotopic Composition of Ancient Oceans: The Impact of Continental
Growth », American Journal of Science, 300, pp. 434-461.
[11] Goodman, J. C. (2006), « Through Thick and Thin: Marine and Meteoric Ice in a “Snowball Earth” Climate », Geophys. Res. Lett., 33,
doi:10.1029/2006GL026840.
[12] Halverson, G. P., Hoffman, P. F., Schrag, D. P., Maloof, A. C. et Rice,
A. H. N. (2005), « Towards a Neoproterozoic Composite Carbon Isotope
Record », Geological Society of America Bulletin, 117, pp. 1 181-1 207.
[13] Hoffman, P. F., Kaufman, A. J., Halverson, G. P. et Schrag, D. P. (1998),
« A Neoproterozoic Snowball Earth ». Science, 281, pp. 1 342-1 346.
[14] Hyde, W. T., Crowley, T. J., Baum, S. K. et Peltier, W. R. (2000), « Neoproterozoic “Snowball Earth” Simulations with a Coupled Climate/Ice
Sheet Model », Nature, 405, pp. 425-429.
[15] Kasting, J. F. et Howard, M. T. (2006), « Atmospheric Composition and
Climate on the Early Earth », Philosophical Transaction Royal Society
London B, 361, pp. 1 733-1 742.
[16] Kasting, J. F. et al. (2006), « Paleoclimates, Ocean Depth, and the Oxygen Isotopic Composition of Seawater », Earth and Planetary Science
Letters, 252, pp. 82-93.
i
i
i
i
i
i
i
i
208
Paléoclimatologie
[2] Caldeira, K. et Kasting, J. F. (1992), « Susceptibility of the Early Earth
to Irreversible Glaciation Caused by Carbon Dioxide Clouds », Nature,
359, pp. 226-228.
[3] Catling, D. C. et Claire, M. W. (2005)„ « How Earth’s Atmosphere Evolved to an Oxic State: A Status Report », Earth and Planetary Science
Letters, 237, pp. 1-20.
[4] Donnadieu, Y., Fluteau, F., Ramstein, G., Ritz, C. et Besse, J. (2003),
« Is there a Conflict between the Neoproterozoic Glacial Deposits and the
Snowball Earth Interpretation: an Improved Understanding with Numerical Modeling », Earth and Planetary Science Letters, 208, pp. 101-112.
[5] Donnadieu, Y., Goddéris, Y., Ramstein, G., Nédelec, A. et Meert, J. G.
(2004), « Snowball Earth Triggered by Continental Break-Up through
Changes in Runoff », Nature, 428, pp. 303-306.
[6] Evans, D. A. D. (2000), « Stratigraphic, Geochronological, and Paleomagnetic Constraints upon the Neoproterozoic Climatic Paradox », American Journal of Science, 300, pp. 347-433.
[7] François, L. M. et Goddéris, Y. (1998), « Isotopic Constraints on the Cenozoic Evolution of the Carbon Cycle », Chemical Geology, 145, pp. 177212.
[8] Gaucher, E. A., Govindarajan, S. et Ganesh, O. K. (2008) ; « Palaeotemperature Trend for Precambrian Life Inferred from Resurrected Proteins », Nature, 451, pp. 704-708.
[9] Goddéris, Y. et al. (2003), « The Sturtian Glaciation: Fire and Ice »,
Earth and Planetary Science Letters, 211, pp. 1-12.
[10] Goddéris, Y. et Veizer, J. (2000), « Tectonic Control of Chemical and
Isotopic Composition of Ancient Oceans: The Impact of Continental
Growth », American Journal of Science, 300, pp. 434-461.
[11] Goodman, J. C. (2006), « Through Thick and Thin: Marine and Meteoric Ice in a “Snowball Earth” Climate », Geophys. Res. Lett., 33,
doi:10.1029/2006GL026840.
[12] Halverson, G. P., Hoffman, P. F., Schrag, D. P., Maloof, A. C. et Rice,
A. H. N. (2005), « Towards a Neoproterozoic Composite Carbon Isotope
Record », Geological Society of America Bulletin, 117, pp. 1 181-1 207.
[13] Hoffman, P. F., Kaufman, A. J., Halverson, G. P. et Schrag, D. P. (1998),
« A Neoproterozoic Snowball Earth ». Science, 281, pp. 1 342-1 346.
[14] Hyde, W. T., Crowley, T. J., Baum, S. K. et Peltier, W. R. (2000), « Neoproterozoic “Snowball Earth” Simulations with a Coupled Climate/Ice
Sheet Model », Nature, 405, pp. 425-429.
[15] Kasting, J. F. et Howard, M. T. (2006), « Atmospheric Composition and
Climate on the Early Earth », Philosophical Transaction Royal Society
London B, 361, pp. 1 733-1 742.
[16] Kasting, J. F. et al. (2006), « Paleoclimates, Ocean Depth, and the Oxygen Isotopic Composition of Seawater », Earth and Planetary Science
Letters, 252, pp. 82-93.