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  • Anand, P., H. Elderfield, and M. H. Conte (2003), Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series, Paleoceanography, 18(2), 1050, doi:10.1029/2002PA000846.
  • Andersen, C., N. Koc, and M. Moros (2004), A highly unstable Holocene climate in the subpolar North Atlantic: Evidence from diatoms, Quat. Sci. Rev., 23, 21552166.
  • Andersson, C., B. Risebrobakken, E. Jansen, and S. O. Dahl (2003), Late Holocene surface ocean conditions of the Norwegian Sea (Vøring Plateau), Paleoceanography, 18(2), 1044, doi:10.1029/2001PA000654.
  • Azetsu-Scott, K., and F. C. Tan (1997), Oxygen isotope studies from Iceland to an East Greenland fjord: Behavior of a glacial meltwater plume, Mar. Chem., 56, 239251.
  • 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.
  • Bauch, D., P. Schlosser, and R. G. Fairbanks (1995), Freshwater balance and the sources of deep and bottom waters in the Arctic Ocean inferred from the distribution of H218O, Prog. Oceanogr., 35, 5380.
  • Birks, C. J. A., and N. Koc (2002), A high-resolution diatom record of late-Quaternary sea-surface temperatures and oceanographic conditions from the eastern Norwegian Sea, Boreas, 31, 323344.
  • Boyle, E. A., and L. D. Keigwin (1985), Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: Changes in deep ocean circulation and chemical inventories, Earth Planet. Sci. Lett., 76, 135150.
  • Broecker, W. S., and T. H. Peng (1982), Tracers in the Sea, 690 pp., Eldigio Press, New York.
  • Brown, S. J., and H. Elderfield (1996), Variations in Mg/Ca and Sr/Ca ratios of planktonic foraminifera caused by postdepositional dissolution: Evidence of shallow Mg-dependent dissolution, Paleoceanography, 11, 543551.
  • 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.
  • Dekens, P. S., D. W. Lea, D. K. Pak, and H. J. Spero (2002), Core top calibration of Mg/Ca in tropical foraminifera: Refining paleotemperature estimation, Geochem. Geophys. Geosyst., 3(4), 1022, doi:10.1029/2001GC000200.
  • Dokken, T., and E. Jansen (1999), Rapid changes in the mechanism of ocean convection during the last glacial period, Nature, 401, 458461.
  • Dreger, D. (1999), Decadal-to-centennial-scale sediment records of ice advance on the Barents shelf and meltwater discharge into the north-eastern Norwegian Sea over the last 40 kyr, Ph.D. thesis, 79 pp., Univ. of Kiel, Kiel, Germany.
  • Elderfield, H., and G. M. Ganssen (2000), Past temperature and δ18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios, Nature, 405, 442445.
  • Elderfield, H., M. Vautravers, and M. Cooper (2002), The relationship between shell size and Mg/Ca, Sr/Ca, δ18O, and δ13C of species of planktonic foraminifera, Geochem. Geophys. Geosyst., 3(8), 1052, doi:10.1029/2001GC000194.
  • Fevang, A. (2001), Klimaendringer i de nordiske hav is i siste glasiale maksimum og Terminasjon 1, Cand. sci. thesis, 106 pp. Univ. of Bergen, Bergen, Norway.
  • Frank, M. (1996), Spurenstoffuntersuchungen zur zirkulation im Eurasischen Becken des Nordpolarmeeres, Ph.D. thesis, Ruprecht Karls Univ., Heidelberg, Germany.
  • Goldschmidt, P. M. (1994), The ice-rafting history in the Norwegian-Greenland Sea for the last two glacial/interglacial cycles, Rep. 313, 103 pp., Univ. of Kiel, Kiel, Germany.
  • Hastings, D. W., A. D. Russell, and S. R. Emerson (1998), Foraminiferal magnesium in Globigerinoides sacculifer as a paleotemperature proxy, Paleoceanography, 13, 161169.
  • Henrich, R. (1992), Beckenanalyse des Europäischen Nordmeeres: Pelagische und glaziomarine Sedimenteinflüsse im Zeitraum 2.6 Ma bis rezent, Habilitationsschr. Math.-Nat. Fak., 345 pp., Univ. of Kiel, Kiel, Germany.
  • Huber, R., H. Meggers, K.-H. Baumann, and R. Henrich (2000), Recent and Pleistocene carbonate dissolution in sediments of the Norwegian-Greenland Sea, Mar. Geol., 165, 123136.
  • Israelson, C., and B. Buchardt (1999), Strontium and oxygen isotopic composition of East Greenland rivers and surface waters: Implication for palaeoenvironmental interpretation, Palaeogeogr. Palaeoclimatol. Palaeoecol., 153, 93104.
  • Jansen, E., and M. Meland (2001), Stratigraphy of IMAGES cores in the Faeroese-Shetland area, Tech. Rep. 01–01, Bjerknes Cent. for Clim. Res., Bergen, Norway.
  • Jansen, E., and T. Veum (1990), Evidence for two-step deglaciation and its impact on North Atlantic deep-water circulation, Nature, 343, 612616.
  • Jensen, S. (1998), Planktische Foraminiferen im Europäischen Nordmeer: Verbreitung und Vertikalfluss sowie ihre Entwicklung während der letzten 15 000 Jahre, Ber. Sonderforschungsbereich 313, 75, Christian-Albrechts-Univ., Kiel, Germany.
  • Johannessen, T. (1992), Stable isotopes as climatic indicators in ocean and lake sediments, Doctor of Sci. thesis, Univ. of Bergen, Bergen, Norway.
  • Koc, N., and E. Jansen (1994), Response of the high-latitude Northern Hemisphere to orbital climate forcing: Evidence from the Nordic Seas, Geology, 22, 523526.
  • Kohfeld, K. E. (1996), Neogloboquadrina pachyderma (sinistral coiling) as paleoceanographic tracers in polar oceans: Evidence from Northeast Water Polynya plankton tows, sediment traps, and surface sediments, Paleoceanography, 11, 679699.
  • Kuroyanagi, A., and H. Kawahata (2004), Vertical distribution of living planktonic foraminifera in the seas around Japan, Mar. Micropaleontol., 53, 173196.
  • Lassen, S., A. Kuijpers, H. Kunzendorf, H. Lindgren, J. Heinemeier, E. Jansen, and K. L. Knudsen (2002), Intermediate water signal leads surface water response during Northeast Atlantic deglaciation, Global Planet. Change, 32, 111125.
  • Lea, D. W., T. A. Mashiotta, and H. J. Spero (1999), Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing, Geochim. Cosmochim. Acta, 63, 23692379.
  • Lear, C. H., Y. Rosenthal, and N. Slowey (2002), Benthic foraminiferal Mg/Ca-paleothermometry: A revised core-top calibration, Geochim. Cosmochim. Acta, 66, 33753387.
  • Levitus, S., and T. P. Boyer (1994), World Ocean Atlas 1994, vol. 4, Temperature, NOAA Atlas NES-DIS, vol. 4, 129 pp. Natl. Oceanic and Atmos. Admin., Silver Spring, Md.
  • Manighetti, B., I. N. McCave, M. Maslin, and N. J. Shackleton (1995), Chronology for climate change: Developing age models for the Biogeochemical Ocean Flux Study cores, Paleoceanography, 10, 513525.
  • Maslin, M. (1992), A study of the paleoceanography of the N. E. Atlantic in the late Pleistocene, Ph.D. thesis, Univ. of Cambridge, Cambridge, UK.
  • Meland, M. Y., E. Jansen, and H. Elderfield (2005), Constraints on SST estimates for the northern North Atlantic/Nordic Seas during the LGM, Quat. Sci. Rev., 24, 835852.
  • Meredith, M., K. Heywood, P. Dennis, L. Goldson, R. White, E. Fahrbach, U. Schauer, and S. Østerhus (2001), Freshwater fluxes through the western Fram Strait, Geophys. Res. Lett., 28, 16151618.
  • Mikalsen, G., and H. P. Sejrup (2000), Oxygen isotope composition of fjord and river water in the Sognefjorden drainage area, western Norway: Implications for paleoclimate studies, Estuarine Coastal Shelf Sci., 50, 441448.
  • Moros, M., R. Endler, K. L. Lackschewitz, H. J. Wallrabe-Adams, J. Mienert, and W. Lemke (1997), Physical properties of Reykjanes Ridge sediments and their linkage to high-resolution Greenland Ice Sheet Project 2 ice core data, Paleoceanography, 12, 687695.
  • Nürnberg, D. (1995), Magnesium in tests of Neogloboquadrina pachyderma sinistral from high northern and southern latitudes, J. Foraminiferal Res., 25, 350368.
  • Nürnberg, D., J. Bijma, and C. Hemleben (1996), Assessing the reliability of magnesium in foraminiferal calcite as a proxy for water mass temperatures, Geochim. Cosmochim. Acta, 60, 803814.
  • Nyland, B. F., E. Jansen, C. Andersson, and H. Elderfield (2006), Mg/Ca records from N. pachyderma (dextral and sinistral) in the Norwegian Sea at decadal resolution and their paleoclimatic implications, Geochem. Geophys. Geosyst., doi:10.1029/2005GC001055, in press.
  • Østbø, M. (2000), Oxygen isotope characterization of water masses and mixing in the Nordic Seas, diploma thesis, Norw. Univ. of Sci. and Technol., Trondheim, Norway.
  • Østlund, H. G., and C. Grall (1993), Arctic tritium: 1973–1991, Data Rep. 19, Rosenstiel School of Mar. and Atmos. Sci., Univ. of Miami, Miami, Fla.
  • Østlund, H. G., H. Craig, W. S. Broecker, and D. Spencer (1987), GEOSECS Atlantic, Pacific and Indian Ocean expeditions: Shorebased data and graphics, Tech. Rep. 7, Natl. Sci. Found., Washington, D. C.
  • Paetsch, H. (1991), Sedimentation im Europäischen Nordmeer, Ber. Sonderforschungsbereich 313, 29, 102 pp., Christian-Albrechts-Univ., Kiel, Germany.
  • Roe, A. B. (1998), Hurtige klimavariasjoner i havområdet øst for Scoresbysund, Grønland–isotoptrinn 3 og 2, Cand. sci. thesis, Univ. of Bergen, Bergen, Norway.
  • Rosenthal, Y., E. A. Boyle, and N. Slowey (1997), Temperature control on the incorporation of magnesium, strontium, fluorine, and cadmium into benthic foraminiferal shells from Little Bahama Bank: Prospects for thermocline paleoceanography, Geochim. Cosmochim. Acta, 61, 36333643.
  • Russell, A. D., S. Emerson, B. K. Nelson, J. Erez, and D. W. Lea (1994), Uranium in foraminiferal calcite as a recorder of seawater uranium concentrations, Geochim. Cosmochim. Acta, 58, 671681.
  • Russell, A. D., B. Hönisch, H. J. Spero, and D. W. Lea (2004), Effects of seawater carbonate ion concentration and temperature on shell U, Mg, and Sr in cultured planktonic foraminifera, Geochim. Cosmochim. Acta, 68, 43474361.
  • Sarnthein, M., et al. (1995), Variations in Atlantic surface ocean paleoceanography, 50°–80°N: A time-slice record of the last 30,000 years, Paleoceanography, 10, 10631094.
  • Schmidt, M., R. Botz, P. Stoffers, T. Anders, and G. Bohrmann (1997), Oxygen isotopes in marine diatoms: A comparative study of analytical techniques and new results on the isotope composition of recent marine diatoms, Geochim. Cosmochim. Acta, 61, 22752280.
  • Schrøder-Ritzrau, A., A. Mangini, and M. Lomitschka (2003), Deep-sea corals evidence periodic reduced ventilation in the North Atlantic during the LGM/Holocene transition, Earth Planet. Sci. Lett., 216, 399410.
  • Schulz, H. (1995), Meeresoberflächentemperaturen vor 10,000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums, Rep. 73, 156 pp., Univ. of Kiel, Kiel, Germany.
  • 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, Colloq. Int. Cent. Natl. Rech. Sci., 219, 203209.
  • Simstich, J. (1999), Die ozeanische Deckschicht des Europäischen Nordmeers im Abbild stabiler Isotope von Kalkgehäusen unterschiedlicher Planktonforaminiferarten, Ber. 2, 96 pp., Christian-Albrechts-Univ., Kiel, Germany.
  • Simstich, J., M. Sarnthein, and H. Erlenkeuser (2003), Paired δ18O signals of Neogloboquadrina pachyderma (s) and Turborotalita quinqueloba show thermal stratification structure in Nordic Seas, Mar. Micropaleontol., 48, 107125.
  • Veum, T., E. Jansen, M. Arnold, I. Beyer, and J.-C. Duplessy (1992), Water mass exchange between the North Atlantic and the Norwegian Sea during the last 28,000 years, Nature, 356, 783785.
  • Vogelsang, E. (1990), Paläo-Ozeanographie des Europäischen Nordmeeres an Hand stabiler Kohlenstoff- und Sauerstoffisotope, Ph.D. thesis, Univ. of Kiel, Kiel, Germany.
  • Vogelsang, E., M. Sarnthein, and U. Pflaumann. (2000), δ18O stratigraphy, chronology, and sea surface temperatures of Atlantic sediment records (GLAMAP-2000 Kiel), Rep. 13, 11 pp., Univ. of Kiel, Kiel, Germany.
  • von Gyldenfeldt, A.-B., J. Carstens, and J. Meincke (2000), Estimation of the catchment area of a sediment trap by means of current meters and foraminiferal tests, Deep Sea Res,. Part II, 47, 17011717.
  • von Langen, P. J., D. K. Pak, H. J. Spero, and D. W. Lea (2005), Effects of temperature on Mg/Ca in neogloboquadrinid shells determined by live culturing, Geochem. Geophys. Geosyst., 6, Q10P03, doi:10.1029/2005GC000989.
  • Weinelt, M., M. Sarnthein, U. Pflaumann, H. Schulz, S. J. A. Jung, and H. Erlenkeuser (1996), Ice-free Nordic Seas during the Last Glacial Maximum? Potential sites of deepwater formation, Paleoclimates, 1, 283309.
  • Weinelt, M.et al. (2001), Paleoceanographic proxies in the northern North Atlantic, in The Northern North Atlantic, edited by P. Schäfer et al., pp. 319352, Springer, New York.
  • Weinelt, M., E. Vogelsang, M. Kucera, U. Pflaumann, M. Sarnthein, A. Voelker, H. Erlenkeuser, and B. A. Malmgren (2003), Variability of North Atlantic heat transfer during MIS 2, Paleoceanography, 18(3), 1071, doi:10.1029/2002PA000772.