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  • Abrantes, F. (2000), 200,000 yr diatom records from Atlantic upwelling sites reveal maximum productivity during LGM and a shift in phytoplankton community structure at 185,000 yr, Earth Planet. Sci. Lett., 176, 716.
  • Bacon, M. P. (1984), Glacial to interglacial changes in carbonate and clay sedimentation in the Atlantic Ocean estimated from 230Th measurements, Isot. Geosci., 2, 97111.
  • Bard, E. (1998), Geochemical and geophysical implications of the radiocarbon calibration, Geochim. Cosmochim. Acta, 62, 20252038.
  • Bard, E., B. Hamelin, R. G. Fairbanks, and A. Zindler (1990), Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals, Nature, 345, 405410.
  • Barker, S., M. Greaves, and H. Elderfield (2003), A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry, Geochem. Geophys. Geosyst., 4(9), 8407, doi:10.1029/2003GC000559.
  • Bassinot, F., and L. Labeyrie (1996), Les rapports de campagne à la mer à bord du Marion-Dufresne: Campagne IMAGES MD 101, Rep. 96-1, 217 pp., Inst. Fr. pour la Rech. et la Technol. Pol., Plouzane, France.
  • Bé, A. W. H. (1960), Ecology of recent planktonic foraminifera. part II: Bathymetric and seasonal distributions in the Sargasso Sea off Bermuda, Micropaleontology, 6, 373392.
  • Berger, A. L. (1978), Long-term variations of daily insolation and quaternary climatic changes, J. Atmos. Sci., 35, 23622367.
  • Blunier, T., and E. J. Brook (2001), Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period, Science, 291, 109112.
  • Bond, G., et al. (1992), Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period, Nature, 360, 245249.
  • Broecker, W. S., and T. H. Peng (1982), Tracers in the Sea, Eldigio, Palisades, N. Y.
  • Broecker, W., G. Bond, M. Klas, E. Clark, and J. McManus (1992), Origin of the northern Atlantic's Heinrich events, Clim. Dyn., 6, 265273.
  • Chapman, M. R., and M. A. Maslin (1999), Low-latitude forcing of meridional temperature and salinity gradients in the subpolar North Atlantic and the growth of glacial ice sheets, Geology, 27, 875878.
  • Chapman, M. R., and N. J. Shackleton (1998), Millennial-scale fluctuations in North Atlantic heat flux during the last 150,000 years, Earth Planet. Sci. Lett., 159, 5770.
  • Chase, Z., R. F. Anderson, M. Q. Fleisher, and P. W. Kubik (2002), The influence of particle composition and particle flux on scavenging of Th, Pa and Be in the ocean, Earth Planet. Sci. Lett., 204, 215229.
  • Chi, J., and J. Mienert (1996), Linking physical property records of Quaternary sediments to Heinrich events, Mar. Geol., 131, 5773.
  • CLIMAP Project Members (1976), The surface of the ice-age Earth, Science, 191, 11311137.
  • Cortijo, E. (1995), La Variabilité climatique rapide dans l'Atlantique nord depuis 128,000 ans: Relations entre les calottes de glace et l'océan de surface, Ph.D. thesis, Univ. de Paris-Sud, Orsay, France.
  • Cortijo, E., L. Labeyrie, L. Vidal, M. Vautravers, M. Chapman, J.-C. Duplessy, M. Elliot, M. Arnold, J.-L. Turon, and G. Auffret (1997), Changes in sea surface hydrology associated with Heinrich event 4 in the North Atlantic Ocean between 40° and 60°N, Earth Planet. Sci. Lett., 146, 2945.
  • Cortijo, E., J.-C. Duplessy, L. Labeyrie, J. Duprat, and D. Paillard (2005), Heinrich events: Hydrological impact, C. R. Geosci., 337, 897904.
  • Dansgaard, W., et al. (1993), Evidence for general instability of past climate from a 250-kyr ice-core record, Nature, 364, 218220.
  • Death, R., M. J. Siegert, G. R. Bigg, and M. R. Wadley (2006), Modelling iceberg trajectories, sedimentation rates and meltwater input to the ocean from the Eurasian ice sheet at the Last Glacial Maximum, Palaeogeogr. Palaeoclimatol. Palaeoecol., 236, 135150.
  • Denton, G. H., R. B. Alley, G. C. Comer, and W. S. Broecker (2005), The role of seasonality in abrupt climate change, Quat. Sci. Rev., 24, 11591182.
  • de Villiers, S., M. Greaves, and H. Elderfield (2002), An intensity ratio calibration method for the accurate determination of Mg/Ca and Sr/Ca of marine carbonates by ICP-AES, Geochem. Geophys. Geosyst., 3(1), 1001, doi:10.1029/2001GC000169.
  • Dickson, R. R., and J. Brown (1994), The production of North Atlantic Deep Water: Sources, rates, and pathways, J. Geophys. Res., 99(C6), 12,31912,341.
  • Dokken, T. M., and E. Jansen (1999), Rapid changes in the mechanism of ocean convection during the last glacial period, Nature, 401, 458461.
  • Duplessy, J.-C., L. Labeyrie, A. Juillet-Leclerc, F. Maitre, J. Duprat, and M. Sarnthein (1991), Surface salinity reconstruction of the North Atlantic Ocean during the last glacial maximum, Oceanol. Acta, 14, 311324.
  • Elderfield, H., and G. Ganssen (2000), Past temperature and δ18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios, Nature, 405, 442445.
  • Elliot, M. (1999), Variabilité millénaire du climat et de l'hydrologie de l'océan atlantique nord lors de la dernière période glaciaire (60,000–10,000 ans), report, Univ. de Paris-Sud, Orsay, France.
  • Elliot, M., L. Labeyrie, T. M. Dokken, and S. Manthé (2001), Coherent patterns of ice rafted debris deposits in the Nordic regions during the last glacial (10–60 ka), Earth Planet. Sci. Lett., 194, 151163.
  • François, R., and M. P. Bacon (1994), Heinrich events in the North Atlantic: Radiochemical evidence, Deep Sea Res., Part I, 41, 315334.
  • Francois, R., M. Frank, M. M. Rutgers van der Loeff, and M. P. Bacon (2004), 230Th normalization: An essential tool for interpreting sedimentary fluxes during the late Quaternary, Paleoceanography, 19, PA1018, doi:10.1029/2003PA000939.
  • Gherardi, J.-M., L. Labeyrie, J. F. McManus, R. Francois, L. C. Skinner, and E. Cortijo (2005), Evidence from the northeastern Atlantic basin for variability of the meridional overturning circulation through the last deglaciation, Earth Planet. Sci. Lett., 240, 710723.
  • Grousset, F. E., L. Labeyrie, J. A. Sinko, M. Cremer, G. Bond, J. Duprat, E. Cortijo, and S. Huon (1993), Patterns of ice-rafted detritus in the glacial North Atlantic, Paleoceanography, 8, 175192.
  • Heinrich, H. (1988), Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years, Quat. Res., 29, 142152.
  • Henderson, G. M., and R. F. Anderson (2003), The U-series toolbox for paleoceanography, Rev. Mineral. Geochem., 52, 493531.
  • Kissel, C., C. Laj, B. Lehman, and L. Labeyrie (1997), Changes in the strength of the Iceland-Scotland Overflow Water in the last 200,000 years: Evidence from magnetic anisotropy analysis of core SU90-33, Earth Planet. Sci. Lett., 152, 2536.
  • Kissel, C., C. Laj, L. Labeyrie, T. Dokken, A. Voelker, and D. Blamart (1999), Rapid climatic variations during climatic stage 3: Magnetic analysis of sediments from Nordic Seas and North Atlantic, Earth Planet. Sci. Lett., 171, 489502.
  • Koç Karpuz, N., and H. Schrader (1990), Surface sediment diatom distribution and Holocene paleotemperature variations in the Greenland, Iceland and Norwegian Sea, Paleoceanography, 5, 557580.
  • Koç, N., E. Jansen, M. Hald, and L. Labeyrie (1996), Late glacial–Holocene sea surface temperatures and gradients between the North Atlantic and the Norwegian Sea: Implications for the Nordic heat pump, Geol. Soc. Spec. Publ., 111, 177185.
  • Labeyrie, L. (1990), PALEOCINAT (Paleocirculation de l'Atlantique nord), preliminary report, Inst. Fr. de Rech. Pout l'Exploit. de la Mer, Brest, France.
  • Labeyrie, L., et al. (1995), Surface and deep hydrology of the northern Atlantic Ocean during the past 150 000 years, Philos. Trans. R. Soc. London, Ser. B, 348, 255264.
  • Labeyrie, L., H. Leclaire, C. Waelbroeck, E. Cortijo, J.-C. Duplessy, L. Vidal, M. Elliot, and B. Le Coat (1999), Temporal variability of the surface and deep waters of the north west Atlantic Ocean at orbital and millennial scales, in Mechanisms of Global Climate Change at Millennial Time Scales, Geophys. Monogr. Ser., vol. 122, edited by P. U. Clark, R. S. Webb, and L. D. Keigwin, pp. 7798, AGU, Washington, D. C.
  • Laj, C., C. Kissel, A. Mazaud, J. E. T. Channell, and J. Beer (2000), North Atlantic palaeointensity stack since 75 ka (NAPIS-75) and the duration of the Laschamp event, Philos. Trans. R. Soc. London, Ser. A, 358, 10091025.
  • Longhurst, A. (1998), Ecological Geography of the Sea, 398 pp., Elsevier, New York.
  • Manighetti, B. (1993), The glacial to Holocene sedimentary regime in the northeast Atlantic Ocean, Ph.D. thesis, Univ. of Cambridge, Cambridge, U. K.
  • Manthé, S., (1998), Variabilité de la circulation thermohaline glaciaire et interglaciaire tracée par les foraminifères planctoniques et de la microfaune benthique, Ph.D. thesis, Univ. Bordeaux I, Bordeaux, France.
  • Marchitto, T. M.Jr., D. W. Oppo, and W. B. Curry (2002), Paired benthic foraminiferal Cd/Ca and Zn/Ca evidence for a greatly increased presence of Southern Ocean water in the glacial North Atlantic, Paleoceanography, 17(3), 1038, doi:10.1029/2000PA000598.
  • Marshall, J., Y. Kushnir, D. Battisti, P. Chang, A. Czaja, R. Dickson, J. Hurrell, M. McCartney, R. Saravanan, and M. Visbeck (2001), North Atlantic climate variability: Phenomena, impacts and mechanisms, Int. J. Climatol., 21, 18631898.
  • Maslin, M. A., N. J. Shackleton, and U. Pflaumann (1995), Surface water temperature, salinity, and density changes in the northeast Atlantic during the last 45,000 years: Heinrich events, deep water formation, and climatic rebounds, Paleoceanography, 10, 527544.
  • McCartney, M. S., S. L. Bennett, and M. E. Woodgate-Jones (1991), Eastward flow through the Mid-Atlantic Ridge at 11°N and its influence on the abyss of the Eastern basin, J. Phys. Oceanogr., 21, 10891121.
  • McManus, J. F., R. Francois, J.-M. Gherardi, L. D. Keigwin, and S. Brown-Leger (2004), Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes, Nature, 428, 834837.
  • Oppo, D. W., and S. J. Lehman (1995), Suborbital timescale variability of North Atlantic Deep Water during the past 200,000 years, Paleoceanography, 10, 901910.
  • Ostermann, D. R., and W. B. Curry (2000), Calibration of stable isotopic data: An enriched δ18O standard used for source gas mixing detection and correction, Paleoceanography, 15, 353360.
  • Paillard, D., L. Labeyrie, and P. Yiou (1996), Macintosh program performs time-series analysis, Eos Trans. AGU, 77, 379.
  • Parsons, T. R., and C. M. Lalli (1988), Comparative oceanic ecology of the plankton communities of the subarctic Atlantic and Pacific oceans, Oceanogr. Mar. Biol., 26, 317359.
  • Pastouret, L., G. A. Auffret, M. Hoffert, M. Melguen, H. D. Needham, and C. Latouche (1975), Sédimentation sur la Ride de Terre-Neuve, Can. J. Earth Sci., 12, 10191035.
  • Rasmussen, T. L., E. Thomsen, T. C. E. van Weering, and L. Labeyrie (1996), Rapid changes in surface and deep water conditions at the Faeroe Margin during the last 58,000 years, Paleoceanography, 11, 757771.
  • Reynolds-Sautter, L., and R. C. Thunell (1989), Seasonal succession of planktonic foraminifera: Results from a four-year time-series sediment trap experiment in the northeast Pacific, J. Foraminiferal Res., 19, 253267.
  • Ruddiman, W. F. (1977), Late Quaternary deposition of ice-rafted sand in the subpolar North Atlantic (lat 40° to 65°N), Geol. Soc. Am. Bull., 88, 18131827.
  • Ruddiman, W. F., and A. McIntyre (1981), The North Atlantic Ocean during the last deglaciation, Palaeoceanogr. Palaeoclimatol. Palaeoecol., 35, 145214.
  • Rühlemann, C., P. J. Müller, and R. R. Schneider (1999), Organic carbon and carbonate as paleoproductivity proxies: Examples from high and low productivity areas of the tropical Atlantic, in Use of Proxies in Paleoceanography: Examples From the South Atlantic, edited by G. Fischer, and G. Wefer, pp. 315344, Springer, New York.
  • Sancetta, C. (1992), Primary production in the glacial North Atlantic and North Pacific oceans, Nature, 360, 249251.
  • Schrader, H.-J., and G. Schuette (1968), Marine diatoms, in The Sea, edited by C. Emiliani, pp. 11791231, John Wiley, Hoboken, N. J.
  • Shackleton, N. J. (1974), Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus Uvigerina: Isotopic changes in the ocean during the last glacial, in Les méthodes quantitatives d'étude des variations du climat au cours du pléistocène, pp. 203210, Gif/Yvette Colloq. Int. du Cent. Natl. de la Rech. Sci., Paris.
  • Stuiver, M., and T. F. Braziunas (1993), Sun, ocean, climate and atmosphere 14CO2: An evaluation of causal and spectral relationships, Holocene, 3, 289305.
  • Stuiver, M., P. J. Reimer, E. Bard, J. W. Beck, G. S. Burr, K. A. Hughen, B. Kromer, F. G. McCormac, J. Plicht, and M. Spurk (1998a), INTCAL98 radiocarbon age calibration 24,000-0 cal BP, Radiocarbon, 40, 10411083.
  • Stuiver, M., P. J. Reimer, and T. F. Braziunas (1998b), High-precision radiocarbon age calibration for terrestrial and marine samples, Radiocarbon, 40, 11271151.
  • Sverdrup, H. U. (1953), On conditions of the vernal blooming of phytoplankton, J. Cons. Cons. Int. Explor. Mer, 18, 287295.
  • Thomas, E., L. Booth, M. Maslin, and N. J. Shackleton (1995), Northeastern Atlantic benthic foraminifera during the last 45,000 years: Changes in productivity seen from the bottom up, Paleoceanography, 10, 545562.
  • Vautravers, M. (1997), Sédimentation et dissolution des carbonates biogéniques aux moyennes latitudes Nord et Sud: Approche quantitative et relations avec les paléocirculations océaniques des derniers 150,000 ans, Ph.D. thesis, Univ. Bordeaux I, Bordeaux, France.
  • Vidal, L., L. Labeyrie, E. Cortijo, M. Arnold, J. C. Duplessy, E. Michel, S. Becqué, and T. C. E. van Weering (1997), Evidence for changes in the North Atlantic Deep Water linked to meltwater surges during the Heinrich events, Earth Planet. Sci. Lett., 146, 1327.
  • Villanueva, J., J. O. Grimalt, E. Cortijo, L. Vidal, and L. Labeyrie (1997), A biomarker approach to the organic matter deposited in the North Atlantic during the last climatic cycle, Geochim. Cosmochim. Acta, 61, 46334646.
  • Waelbroeck, C., J.-C. Duplessy, E. Michel, L. Labeyrie, D. Paillard, and J. Duprat (2001), The timing of the last deglaciation in North Atlantic climate records, Nature, 412, 724727.
  • Wagner, T., and L. M. Dupont (1999), Terrestrial organic matter in marine sediments: Analytical approaches and eolian-marine records in the central equatorial Atlantic, in Use of Proxies in Paleoceanography: Examples From the South Atlantic, edited by G. Fischer, and G. Wefer, pp. 547574, Springer, New York.
  • Weeks, R. J., C. Laj, L. Endignoux, A. Mazaud, L. Labeyrie, A. P. Roberts, C. Kissel, and E. Blanchard (1995), Normalized natural remanent magnetisation intensity during the last 240,000 years in piston cores from the central North Atlantic Ocean: Geomagnetic field intensity or environmental signal? Phys. Earth Planet. Inter., 87, 213229.
  • Wefer, G., W. H. Berger, J. Bijma, and G. Fischer (1999), Clues to ocean history: A brief overview of proxies, in Use of Proxies in Paleoceanography: Examples From the South Atlantic, edited by G. Fischer, and G. Wefer, pp. 168, Springer, New York.
  • Yu, E.-F., R. Francois, M. P. Bacon, and A. P. Fleer (2001), Fluxes of 230Th and 231Pa to the deep sea: Implications for the interpretation of excess 230Th and 231Pa/230Th profiles in sediments, Earth Planet. Sci. Lett., 191, 219230.