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Pichegru, L., Ryan, P.G., van der Lingen, C.D., Coetzee, J., Ropert-Coudert, Y. & Grémillet, D. (2008). Foraging behaviour and energetics of Cape gannets Morus capensis feeding on live prey and fishery discards in the Benguela upwelling system. Mar. Ecol. Prog. Ser., 350, 127–136.
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Grémillet D. (2006). Des pêcheurs efficaces: les cormorans. Pour la science, 347, 62–67.
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Lorius, C.; Jouzel, J.; Raynaud, D.; Hansen, J.; Treut, H.L. (1990). The ice-core record: climate sensitivity and future greenhouse warming. Nature, 347(6289), 139–145.
Abstract: The prediction of future greenhouse-gas-induced warming depends critically on the sensitivity of Earth's climate to increasing atmospheric concentrations of these gases. Data from cores drilled in polar ice sheets show a remarkable correlation between past glacial–interglacial temperature changes and the inferred atmospheric concentration of gases such as carbon dioxide and methane. These and other palaeoclimate data are used to assess the role of greenhouse gases in explaining past global climate change, and the validity of models predicting the effect of increasing concentrations of such gases in the atmosphere.
Programme: 159
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Van Vliet-Lanoë B. , Guðmundsson A., Guillou H. , Duncan R.A. , Genty D. , Gassem B. , Gouy S., Récourt P., Scaillet S. (2007). Limited glaciation and very early deglaciation in central Iceland: Implications for climate change. Comptes Rendus de Géoscience, 339, 1–12.
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Duplessy J.C., Cortijo E., Masson Delmotte V. & Paillard D. (2005). Reconstructing the variability of the climate system : facts and theories. C.R. Acad. Sci. Paris, 337(10-11), 888–896.
Abstract: On the 102- to 103-year timescale, internal reorganizations of the climate system result in abrupt climatic changes of great magnitude. Although a large body of data has been obtained, the physical mechanisms responsible for these changes are still poorly understood. Instrumental data are too short to fully record the variability of the climate system. Palaeoclimatic records provide estimates of the past atmospheric composition, temperature, precipitation, vegetation, extension of glaciers, and past ocean circulation. On the 104- to 106-year timescale, the astronomical theory of palaeoclimates accounts for most of the reconstructed variations. To cite this article: J.-C. Duplessy et al., C. R. Geoscience 337 (2005).
Programme: 960
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Masson-Delmotte V, Landais A, Combourieu-Nebout N, von Grafenstein U, Jouzel J, Caillon N, Chappellaz J, Dahl-Jensen D, Johnsen SJ, Stenni B. (2005). Rapid climate variability during warm and cold periods in polar regions and Europe. C.R. Acad. Sci. Paris, 337, 935–946.
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Landais A, Jouzel J, Masson-Delmotte V, Caillon N. (2005). Large temperature variations over rapid climatic events in Greenland: a method based on air isotopic measurements. C.R. Acad. Sci. Paris, 337, 947–956.
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Jouzel J, Masson-Delmotte V, Stievenard M, Landais A, Vimeux F, Johnsen SJ, Sveinbjornsdottir AE, White JW. (2005). Rapid deuterium-excess changes in Greenland ice cores: a link between the ocean and the atmosphere. C.R. Acad. Sci. Paris, 337(10-11), 957–969.
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Montagnat M., Duval P., Bastie P., Hamelin B., Brissaud O., De Angelis M., Petit J.R., . & Lipenkov V.Y. (2001). High crystalline quality of large single crystals of subglacial ice above Lake Vostok (Antarctica) revealead by hard X-ray diffaction. Earth Planet. Sci. Lett., 333, 419–425.
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Enstipp, M.R., Grémillet, D. & Jones D.R. (2007). Investigating the functional link between prey abundance and seabird predatory performance. Mar. Ecol. Prog. Ser., 331, 267–279.
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