“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 289 — #312
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7. Climat et cycles astronomiques
289
Références bibliographiques
[1] Adkins, J., McIntyre, K. et Schrag, D. (2002), « The Salinity, Temperature and δ
18 O of the Glacial Deep Ocean », Science, 298, pp. 1769-1773.
[2] Arrhenius, S. (1896), « On the Influence of Carbonic Acid in the Air upon
the Temperature of the Ground », Philosophical Magazine and Journal
of Science, 41, pp. 237-276.
[3] Bard, E. (2004), « Greenhouse Effect and Ice Ages: Historical Perspective », C. R. Geoscience, 336, pp. 603-638.
[4] Bard, E., Hamelin, B., Arnold, M., Montaggioni, L., Cabioch, G., Faure,
G. et Rougerie, F. (1996), « Deglacial Sea-Level Record from Tahiti
Corals and the Timing of Global Meltwater Discharge », Nature, 382,
pp. 241-244.
[5] Berger, A. (1978), « Long-Term Variations of Daily Insolation and Quaternary Climatic Change », J. Atmos. Sci., 35, pp. 2362-2367.
[6] Bouttes, N., Paillard, D., Roche, D. M., Brovkin, V. et Bopp, L. (2011),
« Last Glacial Maximum CO 2 and δ
13 C Successfully Reconciled », Geophys. Res. Lett., 38, pp. 1-5.
[7] Broecker, W. et van Donk, J. (1970), « Insolation Changes, Ice Volumes
and the O18 Record in Deep-Sea Cores », Rev. Geophys. Space Phys., 8,
pp. 169-197.
[8] Gale, A. S., Young, J. R., Shackleton, N. J., Crowhurst, S. J. et Wray, D.
S. (1999), « Orbital Tuning of Cenomanian Marly Chalk Successions: Towards a Milankovitch Time-Scale for the Late Cretaceous », Philosophical
Transactions of the Royal Society A, 357, pp. 1 815-1 829.
[9] Hays, J., Imbrie, J. et Shackleton, N. J. (1976), « Variations in the Earth’s
Orbit: Pacemakers of the Ice Ages », Science, 194, pp. 1 121-1 132.
[10] Hofmann, A., Dirks, P. H. G. M., Jelsma, H. A. (2004), « ShallowingUpward Carbonate Cycles in the Belingwe Greenstone Belt, Zimbabwe:
A Record of Archean Sea-Level Oscillations », Journal of Sedimentary
Research, 74, pp. 64-81.
[11] Huybers, P. (2006), « Early Pleistocene Glacial Cycles and the Integrated
Summer Insolation Forcing », Science, 313, pp. 508-511.
[12] Huybers, P., Wunsch, C. (2005), « Obliquity Pacing of the late Pleistocene Glacial Terminations », Nature, 434, pp. 491-494.
[13] Imbrie, J., Hays, J., Martinson, D., McIntyre, A., Mix, A., Morley, J. J.,
Pisias, N., Prell, W., Shackleton, N., Berger, A., Kukla, G., Saltzman,
B. (1984), « The Orbital Theory of Pleistocene Climate: Support from a
Revised Chronology of the Marine d18O Record », dans Berger, A. (Ed.),
Milankovitch and Climate, Kluwer Academic Publishers (Nato ASI Ser.
C), Dordrecht, pp. 269-305.
[14] Joussaume, S., Braconnot, P. (1997), « Sensitivity of Paleoclimate Simulation Results to Season Definitions », J. Geophys. Res. D, 102, pp. 1 9431 956.
i
i
i
i
i
i
i
i
7. Climat et cycles astronomiques
289
Références bibliographiques
[1] Adkins, J., McIntyre, K. et Schrag, D. (2002), « The Salinity, Temperature and δ
18 O of the Glacial Deep Ocean », Science, 298, pp. 1769-1773.
[2] Arrhenius, S. (1896), « On the Influence of Carbonic Acid in the Air upon
the Temperature of the Ground », Philosophical Magazine and Journal
of Science, 41, pp. 237-276.
[3] Bard, E. (2004), « Greenhouse Effect and Ice Ages: Historical Perspective », C. R. Geoscience, 336, pp. 603-638.
[4] Bard, E., Hamelin, B., Arnold, M., Montaggioni, L., Cabioch, G., Faure,
G. et Rougerie, F. (1996), « Deglacial Sea-Level Record from Tahiti
Corals and the Timing of Global Meltwater Discharge », Nature, 382,
pp. 241-244.
[5] Berger, A. (1978), « Long-Term Variations of Daily Insolation and Quaternary Climatic Change », J. Atmos. Sci., 35, pp. 2362-2367.
[6] Bouttes, N., Paillard, D., Roche, D. M., Brovkin, V. et Bopp, L. (2011),
« Last Glacial Maximum CO 2 and δ
13 C Successfully Reconciled », Geophys. Res. Lett., 38, pp. 1-5.
[7] Broecker, W. et van Donk, J. (1970), « Insolation Changes, Ice Volumes
and the O18 Record in Deep-Sea Cores », Rev. Geophys. Space Phys., 8,
pp. 169-197.
[8] Gale, A. S., Young, J. R., Shackleton, N. J., Crowhurst, S. J. et Wray, D.
S. (1999), « Orbital Tuning of Cenomanian Marly Chalk Successions: Towards a Milankovitch Time-Scale for the Late Cretaceous », Philosophical
Transactions of the Royal Society A, 357, pp. 1 815-1 829.
[9] Hays, J., Imbrie, J. et Shackleton, N. J. (1976), « Variations in the Earth’s
Orbit: Pacemakers of the Ice Ages », Science, 194, pp. 1 121-1 132.
[10] Hofmann, A., Dirks, P. H. G. M., Jelsma, H. A. (2004), « ShallowingUpward Carbonate Cycles in the Belingwe Greenstone Belt, Zimbabwe:
A Record of Archean Sea-Level Oscillations », Journal of Sedimentary
Research, 74, pp. 64-81.
[11] Huybers, P. (2006), « Early Pleistocene Glacial Cycles and the Integrated
Summer Insolation Forcing », Science, 313, pp. 508-511.
[12] Huybers, P., Wunsch, C. (2005), « Obliquity Pacing of the late Pleistocene Glacial Terminations », Nature, 434, pp. 491-494.
[13] Imbrie, J., Hays, J., Martinson, D., McIntyre, A., Mix, A., Morley, J. J.,
Pisias, N., Prell, W., Shackleton, N., Berger, A., Kukla, G., Saltzman,
B. (1984), « The Orbital Theory of Pleistocene Climate: Support from a
Revised Chronology of the Marine d18O Record », dans Berger, A. (Ed.),
Milankovitch and Climate, Kluwer Academic Publishers (Nato ASI Ser.
C), Dordrecht, pp. 269-305.
[14] Joussaume, S., Braconnot, P. (1997), « Sensitivity of Paleoclimate Simulation Results to Season Definitions », J. Geophys. Res. D, 102, pp. 1 9431 956.