“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 254 — #277
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[7] Donnadieu, Y. et al. (2011), « A Mechanism for Brief Glacial Episodes in the Mesozoic Greenhouse ». Paleoceanography, 26,
doi:10.1029/2010PA002100.
[8] Donnadieu, Y. et al. (2006), « A GEOCLIM Simulation of Climatic and
Biogeochemical Consequences of Pangea Breakup », Geochemistry Geophysics Geosystems, 7(11), doi:10.1029/2006GC001278.
[9] Dromart, G. et al. (2003), « Ice Age at the Middle-Late Jurassic Transition ? », Earth and Planetary Science Letters, 213, pp. 205-220.
[10] Finnegan, S. et al. (2011), « The Magnitude and Duration of Late
Ordovician-Early Silurian Glaciation », Science, 331, pp. 903-906.
[11] Frakes, L. A., Francis, J. E. et Syktus, J. I. (1992), Climate Modes of the
Phanerozoic, Cambridge University press, Cambridge.
[12] France-Lanord, C. et Derry, L. A. (1997), « Organic Carbon Burial Forcing of the Carbon Cycle from Himalaya Erosion », Nature, 390, pp. 6567.
[13] Galy, V. et al. (2007), « Efficient Organic Carbon Burial in the Bengal Fan
Sustained by the Himalayan Erosional System », Nature, 450, pp. 407410.
[14] Goddéris, Y. et al. (2008), « Causal of Casual Link between the Rise of
Nannoplankton Calcification and a Tectonically-Driven Massive Decrease
in the Late Triassic Atmospheric CO 2 ? », Earth and Planetary Science
Letters, 267, pp. 247-255.
[15] Goddéris, Y. et François, L. M. (1996), « Balancing the Cenozoic Carbon
and Alkalinity Cycles: Constraints from Isotopic Records », Geophysical
research letters, 23(25), pp. 3 743-3 746.
[16] Hayes, J. M., Strauss, H. et Kaufman, A. J. (1999), « The Abundance of
13 C in Marine Organic Matter and Isotopic Fractionation in the Global
Biogeochemical Cycle of Carbon during the Past 800 Ma », Chemical
Geology, 161, pp. 103-125.
[17] Huber, M. et Nof, D. (2006), « The Ocean Circulation in the Southern
Hemisphere and its Climatic Impacts in the Eocene », Palaeogeography,
Palaeoclimatology, Palaeoecology, 231, pp. 9-28.
[18] Kump, L. R. et al. (1999), « A Weathering Hypothesis for Glaciation at
High Atmospheric pCO 2 during the Late Ordovician », Palaeogeography,
Palaeoclimatology, Palaeoecology, 152, pp. 173-187.
[19] McInerney, F. A. et Wing, S. L. (2011), « The Paleocene-Eocene Thermal
Maximum: A Perturbation of Carbon Cycle, Climate, and Biosphere with
Implications for the Future », Annu. Rev. Earth Planet. Sci., 39, pp. 489516.
[20] Nardin, E. et al. (2011), « Modeling the Early Paleozoic Long-Term Climatic Trend », Geological Society of America Bulletin, 123, pp. 1 1811 192.
i
i
i
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i
i
i
i
254
Paléoclimatologie
[7] Donnadieu, Y. et al. (2011), « A Mechanism for Brief Glacial Episodes in the Mesozoic Greenhouse ». Paleoceanography, 26,
doi:10.1029/2010PA002100.
[8] Donnadieu, Y. et al. (2006), « A GEOCLIM Simulation of Climatic and
Biogeochemical Consequences of Pangea Breakup », Geochemistry Geophysics Geosystems, 7(11), doi:10.1029/2006GC001278.
[9] Dromart, G. et al. (2003), « Ice Age at the Middle-Late Jurassic Transition ? », Earth and Planetary Science Letters, 213, pp. 205-220.
[10] Finnegan, S. et al. (2011), « The Magnitude and Duration of Late
Ordovician-Early Silurian Glaciation », Science, 331, pp. 903-906.
[11] Frakes, L. A., Francis, J. E. et Syktus, J. I. (1992), Climate Modes of the
Phanerozoic, Cambridge University press, Cambridge.
[12] France-Lanord, C. et Derry, L. A. (1997), « Organic Carbon Burial Forcing of the Carbon Cycle from Himalaya Erosion », Nature, 390, pp. 6567.
[13] Galy, V. et al. (2007), « Efficient Organic Carbon Burial in the Bengal Fan
Sustained by the Himalayan Erosional System », Nature, 450, pp. 407410.
[14] Goddéris, Y. et al. (2008), « Causal of Casual Link between the Rise of
Nannoplankton Calcification and a Tectonically-Driven Massive Decrease
in the Late Triassic Atmospheric CO 2 ? », Earth and Planetary Science
Letters, 267, pp. 247-255.
[15] Goddéris, Y. et François, L. M. (1996), « Balancing the Cenozoic Carbon
and Alkalinity Cycles: Constraints from Isotopic Records », Geophysical
research letters, 23(25), pp. 3 743-3 746.
[16] Hayes, J. M., Strauss, H. et Kaufman, A. J. (1999), « The Abundance of
13 C in Marine Organic Matter and Isotopic Fractionation in the Global
Biogeochemical Cycle of Carbon during the Past 800 Ma », Chemical
Geology, 161, pp. 103-125.
[17] Huber, M. et Nof, D. (2006), « The Ocean Circulation in the Southern
Hemisphere and its Climatic Impacts in the Eocene », Palaeogeography,
Palaeoclimatology, Palaeoecology, 231, pp. 9-28.
[18] Kump, L. R. et al. (1999), « A Weathering Hypothesis for Glaciation at
High Atmospheric pCO 2 during the Late Ordovician », Palaeogeography,
Palaeoclimatology, Palaeoecology, 152, pp. 173-187.
[19] McInerney, F. A. et Wing, S. L. (2011), « The Paleocene-Eocene Thermal
Maximum: A Perturbation of Carbon Cycle, Climate, and Biosphere with
Implications for the Future », Annu. Rev. Earth Planet. Sci., 39, pp. 489516.
[20] Nardin, E. et al. (2011), « Modeling the Early Paleozoic Long-Term Climatic Trend », Geological Society of America Bulletin, 123, pp. 1 1811 192.