File:Figure 3.14 - Climate and environmental records of Termination I.png
Climate and environmental records of Termination I. From top to bottom: yellow, 60°N June insolation (W m-2) (Berger and Loutre, 1991[1]); black, global sea level change (m) (Lambeck and Chappell, 2001[2]; Waelbroeck et al., 2002[3]); blue-grey, Greenland NorthGRIP ice core δ18O (‰), a proxy of Greenland temperature change (NorthGRIP-community-members, 2004); composite Greenland (light green) and EPICA Dome C (EDC) (dark green) atmospheric methane concentration records (ppbv) (EPICA, 2006[4]) (Loulergue et al., submitted); red, Antarctic EDC and Vostok stacked atmospheric CO2 concentration record (ppm) (Monnin et al., 2001[5]; Petit et al., 1997[6]); non sea-salt calcium flux, a proxy for continental aerosols, from EPICA Dronning Maud Land (EDML) (brown) and EDC (orange) ice cores (µg/m²yr) (Wolff et al., 2006[7]; Fischer et al., 2007a); sea-salt sodium flux, a proxy for marine aerosols, from EDML (light grey) and EDC (dark grey) (µg/m²yr) (Wolff et al., 2006[7]; Fischer et al., 2007a); blue, EDML δ18O (‰), a proxy of EDML temperature (EPICA, 2006[4]); and finally, in light blue, EDC δD (‰), a proxy of EDC temperature (Jouzel et al., 2007[8]).
- ↑ Berger, A. and Loutre, M.F. 1991. Insolation values for the climate of the last 10 million years, Quaternary Sciences Reviews, 10, 297-317.
- ↑ Lambeck, K. and Chappell, J. 2001. Sea level change through the last glacial cycle, Science, 292, 679-686.
- ↑ Waelbroeck, C., Labeyrie, L., Michel, E., Duplessy, J.C., McManus, J.F., Lambeck, K., Balbon, E. and Labracherie, M. 2002. Sea level and deep water temperature changes derived from bentic foraminifera isotopic records, Quat. Sci. Rev., 21, 295-305.
- ↑ 4.0 4.1 EPICA community members. 2006. One-to-one coupling of glacial climate variability in Greenland and Antarctica, Nature, 444, 195-198.
- ↑ Monnin, E., Indermuhle, A., Dallenbach, A., Fluckiger, J., Stauffer, B., Stocker, T.F., Raynaud, D. and Barnola, J-M. 2001. Atmospheric CO2 Concentrations over the Last Glacial Termination, Science, 291, 112-114.
- ↑ Petit, J.R., Basile, I., Leruyuet, A., Raynaud, D., Lorius, C., Jouzel, J., Stievenard, M., Lipenkov, V.Y., Barkov, N.I., Kudryashov, B.B., Davis, M., Saltzman, E. and Kotlyakov, V. 1997. Four climatic cycles in Vostok ice core, Nature, 387, 359.
- ↑ 7.0 7.1 Wolff, E.W., Fischer, H., Fundel, F., Ruth, U., Twarloh, B., Littot, G.C., Mulvaney, R., Röthlisberger, R., De Angelis, M., Boutron, C.F., Hansson, M., Jonsell, U., Hutterli, M.A,, Lambert, F., Kaufmann, P., Stauffer, B., Stocker, T.F., Steffensen, J.P., Bigler, M., Siggaard-Andersen, M.L., Udisti, R., Becagli, S., Castellano, E., Severi, M., Wagenbach, D., Barbante, C., Gabrielli, P. and Gaspari, V. 2006. Southern Ocean sea-ice extent, productivity and iron flux over the past eight glacial cycles, Nature, 440, 491-496 (doi:10.1038/nature04614).
- ↑ Jouzel, J., Masson-Delmotte, V., Cattani, O., Dreyfus, G., Falourd, S., Hoffmann, G., Minster, B., Nouet, J., Barnola, J.M., Chappellaz, J., Fischer, H., Gallet, J.C., Johnsen, S., Leuenberger, M., Loulergue, L., Luethi, D., Oerter, H., Parrenin, F., Raisbeck, G., Raynaud, D., Schilt, A., Schwander, J., Selmo, E., Souchez, R., Spahni, R., Stauffer, B., Steffensen, J.P., Stenni, B.S., Tison, J.L., Werner, M. and Wolff, E. 2007. Orbital and millenial Antarctic climate variability over the past 800,000 years, Science, 317, 793-796.
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