“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 42 — #65
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Paléoclimatologie
Références bibliographiques
Ahn, J., Wahlen, M., Deck, B. L., Brook, E. J., Mayewski, P. A., Taylor, K.
C. et White, J. W. C. (2004), « A Record of Atmospheric CO 2 during the
Last 40 000 Years from the Siple Dome, Antarctica Ice Core », J. Geophys.
Res., 109, D13305, doi:10.1029/2003JD004415.
Archer, D., Winguth, A., Lea, D. et Mahowald, N. (2000), « What Caused the
Glacial/Interglacial Atmospheric pCO 2 Cycles ? », Reviews of Geophysics,
38, pp. 159-189.
Bernard, S., Rockmann, T., Kaiser, J., Barnola, J. M., Fischer, H., Blunier, T.
et Chappellaz, J. (2006), « Constraints on N 2 O Budget Changes since PreIndustrial Time from New Firn Air and Ice Core Isotope Measurements »,
Atmospheric Chemistry and Physics, 6, pp. 493-503.
Barnola, J. M., Raynaud, D., Korotkevich, Y. S. et Lorius, C. (1987), « Vostok
Ice Core Provides 160,000-Year Record of Atmospheric CO 2 », Nature, 329,
pp. 408-414.
Broecker, W. S. et Henderson, G. M. (1998), « The Sequence of Events Surrounding Termination II and their Implications for the Cause of GlacialInterglacial CO 2 Changes », Paleoceanography, 13, pp. 352-364.
Chappellaz, J., Barnola, J. M., Raynaud, D., Korotkevich, Y. S. et Lorius, C.
(1990), « Ice-Core Record of Atmospheric Methane over the Past 160,000
Years », Nature, 345, pp. 127-131.
Chappellaz, J. A., Fung, I. Y. et Thompson, A. M. (1993), « The Atmospheric
CH 4 Increase since the Last Glacial Maximum. 1. Source Estimates »,
Tellus, 45B, pp. 228-241.
Chappellaz, J., Blunier, T., Kints, S., Dallenbach, A., Barnola, J. M.,
Schwander, J., Raynaud, D. et Stauffer, B. (1997), « Changes in the Atmospheric CH 4 Gradient between Greenland and Antarctica during the
Holocene », Journal of Geophysical Research, 102, pp. 15 987-15 997.
Charlson, R. J., Lovelock, J. E., Andreae, M. O. et Warren, S. G. (1987),
« Oceanic Phytoplankton, Atmospheric Sulfur, Cloud Albedo and Climate », Nature, 326, pp. 655-661.
Delmas R., Ascencio, J. M. et Legrand, M. (1980), « Polar Ice Evidence that
Atmospheric CO 2 20,000 Year BP Was 50% of Present », Nature, 284,
pp. 155-157.
Falkowski, P. G. (1997), « Evolution of the Nitrogen Cycle and its Influence on
the Biological Sequestration of CO 2 in the Ocean », Nature, 387, pp. 272275.
i
i
i
i
i
i
i
i
42
Paléoclimatologie
Références bibliographiques
Ahn, J., Wahlen, M., Deck, B. L., Brook, E. J., Mayewski, P. A., Taylor, K.
C. et White, J. W. C. (2004), « A Record of Atmospheric CO 2 during the
Last 40 000 Years from the Siple Dome, Antarctica Ice Core », J. Geophys.
Res., 109, D13305, doi:10.1029/2003JD004415.
Archer, D., Winguth, A., Lea, D. et Mahowald, N. (2000), « What Caused the
Glacial/Interglacial Atmospheric pCO 2 Cycles ? », Reviews of Geophysics,
38, pp. 159-189.
Bernard, S., Rockmann, T., Kaiser, J., Barnola, J. M., Fischer, H., Blunier, T.
et Chappellaz, J. (2006), « Constraints on N 2 O Budget Changes since PreIndustrial Time from New Firn Air and Ice Core Isotope Measurements »,
Atmospheric Chemistry and Physics, 6, pp. 493-503.
Barnola, J. M., Raynaud, D., Korotkevich, Y. S. et Lorius, C. (1987), « Vostok
Ice Core Provides 160,000-Year Record of Atmospheric CO 2 », Nature, 329,
pp. 408-414.
Broecker, W. S. et Henderson, G. M. (1998), « The Sequence of Events Surrounding Termination II and their Implications for the Cause of GlacialInterglacial CO 2 Changes », Paleoceanography, 13, pp. 352-364.
Chappellaz, J., Barnola, J. M., Raynaud, D., Korotkevich, Y. S. et Lorius, C.
(1990), « Ice-Core Record of Atmospheric Methane over the Past 160,000
Years », Nature, 345, pp. 127-131.
Chappellaz, J. A., Fung, I. Y. et Thompson, A. M. (1993), « The Atmospheric
CH 4 Increase since the Last Glacial Maximum. 1. Source Estimates »,
Tellus, 45B, pp. 228-241.
Chappellaz, J., Blunier, T., Kints, S., Dallenbach, A., Barnola, J. M.,
Schwander, J., Raynaud, D. et Stauffer, B. (1997), « Changes in the Atmospheric CH 4 Gradient between Greenland and Antarctica during the
Holocene », Journal of Geophysical Research, 102, pp. 15 987-15 997.
Charlson, R. J., Lovelock, J. E., Andreae, M. O. et Warren, S. G. (1987),
« Oceanic Phytoplankton, Atmospheric Sulfur, Cloud Albedo and Climate », Nature, 326, pp. 655-661.
Delmas R., Ascencio, J. M. et Legrand, M. (1980), « Polar Ice Evidence that
Atmospheric CO 2 20,000 Year BP Was 50% of Present », Nature, 284,
pp. 155-157.
Falkowski, P. G. (1997), « Evolution of the Nitrogen Cycle and its Influence on
the Biological Sequestration of CO 2 in the Ocean », Nature, 387, pp. 272275.