“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 255 — #278
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[21] Pagani, M., Zachos, J. C., Freeman, K. H., Tipple, B. et Bohaty, S. (2005),
« Marked Decline in Atmospheric Carbon Dioxide Concentrations during
the Paleogene », Science, 309, pp. 600-603.
[22] Pucéat, E. et al. (2010), « Revised Phosphate-Water Fractionation Equation Reassessing Paleotemperatures Derived from Biogenic Apatite »,
Earth and Planetary Science Letters, 298, pp. 135-142.
[23] Raymo, M. E. (1991), « Geochemical Evidence Supporting T.C. Chamberlin’s Theory of Glaciation », Geology, 19, pp. 344-347.
[24] Royer, D. L. (2006), « CO 2 -Forced Climate Thresholds During the Phanerozoic », Geochimica and Cosmochimica Acta, 70, pp. 5 665-5 675.
[25] Royer, D. L., Berner, R. A. et Beerling, D. J. (2001), « Phanerozoic
Atmospheric CO 2 Change: Evaluating Geochemical and Paleobiological
Approaches », Earth-Science Reviews, 54, pp. 349-392.
[26] Scher, H. D. et Martin, E. E. (2006), « Timing and Climatic Consequences
of the Opening of Drake Passage », Science, 312, pp. 428-431.
[27] Shaviv, N. J. et Veizer, J. (2003), « Celestial Driver of Phanerozoic Climate ? », GSA Today, 13(7), pp. 4-10.
[28] Veizer, J. et al. (1999), «
87 Sr/
86 Sr, δ
13 C and δ
18 O Evolution of Phanerozoic Seawater » Chemical Geology, 161, pp. 59-88.
[29] Veizer, J., Goddéris, Y. et François, L. M. (2000), « Evidence for Decoupling of Atmospheric CO 2 and Global Climate during the Phanerozoic
Eon » Nature, 408, pp. 698-701.
[30] Zachos, J. C., Dickens, G. R. et Zeebe, R. E. (2008), « An early Cenozoic Perspective on Greenhouse Warming and Carbon-Cycle Dynamics »,
Nature, 451(17), doi:10.1038/nature.
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i
i
i
6. Les climats du Phanérozoïque
255
[21] Pagani, M., Zachos, J. C., Freeman, K. H., Tipple, B. et Bohaty, S. (2005),
« Marked Decline in Atmospheric Carbon Dioxide Concentrations during
the Paleogene », Science, 309, pp. 600-603.
[22] Pucéat, E. et al. (2010), « Revised Phosphate-Water Fractionation Equation Reassessing Paleotemperatures Derived from Biogenic Apatite »,
Earth and Planetary Science Letters, 298, pp. 135-142.
[23] Raymo, M. E. (1991), « Geochemical Evidence Supporting T.C. Chamberlin’s Theory of Glaciation », Geology, 19, pp. 344-347.
[24] Royer, D. L. (2006), « CO 2 -Forced Climate Thresholds During the Phanerozoic », Geochimica and Cosmochimica Acta, 70, pp. 5 665-5 675.
[25] Royer, D. L., Berner, R. A. et Beerling, D. J. (2001), « Phanerozoic
Atmospheric CO 2 Change: Evaluating Geochemical and Paleobiological
Approaches », Earth-Science Reviews, 54, pp. 349-392.
[26] Scher, H. D. et Martin, E. E. (2006), « Timing and Climatic Consequences
of the Opening of Drake Passage », Science, 312, pp. 428-431.
[27] Shaviv, N. J. et Veizer, J. (2003), « Celestial Driver of Phanerozoic Climate ? », GSA Today, 13(7), pp. 4-10.
[28] Veizer, J. et al. (1999), «
87 Sr/
86 Sr, δ
13 C and δ
18 O Evolution of Phanerozoic Seawater » Chemical Geology, 161, pp. 59-88.
[29] Veizer, J., Goddéris, Y. et François, L. M. (2000), « Evidence for Decoupling of Atmospheric CO 2 and Global Climate during the Phanerozoic
Eon » Nature, 408, pp. 698-701.
[30] Zachos, J. C., Dickens, G. R. et Zeebe, R. E. (2008), « An early Cenozoic Perspective on Greenhouse Warming and Carbon-Cycle Dynamics »,
Nature, 451(17), doi:10.1038/nature.