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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.
  • 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.
  • 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.
  • Bauch, D., J. Carstens, and G. Wefer (1997), Oxygen isotope composition of living Neogloboquadrina pachyderma (sin) in the Arctic Ocean, Earth Planet. Sci. Lett., 146(1–2), 4758.
  • Bauch, D., H. Erlenkeuser, G. Winckler, G. Pavlova, and J. Thiede (2002), Carbon isotopes and habitat of polar planktic foraminifera in the Okhotsk Sea: The “carbonate ion effect” under natural conditions, Mar. Micropaleontol., 45, 8399.
  • Bauch, D., K. Darling, J. Simstich, H. A. Bauch, H. Erlenkeuser, and D. Kroon (2003), Palaeoceanographic implications of genetic variation in living North Atlantic Neogloboquadrina pachyderma, Nature, 424, 299302.
  • Bé, A. W. H., and D. Tolderlund (1971), Distribution and ecology of living planktonic foraminifera in surface waters of Atlantic and Indian Oceans, in Micropaleontology of Oceans, edited by B. M. Funnell, and W. R. Riedel, pp. 105149, Cambridge Univ. Press, New York.
  • Bemis, B. E., H. J. Spero, J. Bijma, and D. W. Lea (1998), Re-evaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations, Paleoceanography, 13, 150160.
  • Berstad, I. M., H. P. Sejrup, D. Klitgaard-Kristensen, and H. Haflidason (2003), Variability in temperature and geometry of the Norwegian Current over the past 600 yr: Stable isotopes and grain size evidence from the Norwegian margin, J. Quat. Sci., 18, 591602.
  • Birks, C. J. A., and N. Koç (2002), A high-resolution diatom record of late-Quaternary sea-surface temperatures and oceanographic conditions from the eastern Norwegian Sea, Boreas, 31(4), 323344.
  • Boyle, E. (1981), Cadmium, zinc, copper and barium in foraminifera tests, Geochim. Cosmochim. Acta, 47, 18151819.
  • Boyle, E., 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.
  • Briffa, K. R. (2000), Annual climate variability in the Holocene: Interpreting the message of ancient trees, Quat. Sci. Rev., 19, 87105.
  • Calvo, E., J. Grimalt, and E. Jansen (2002), High resolution U37K sea surface temperature reconstruction in the Norwegian Sea during the Holocene, Quat. Sci. Rev., 21, 13851394.
  • Chave, K. E. (1954), Aspects of the biogeochemistry of magnesium 1. Calcareous marine organisms, J. Geol., 62, 266283.
  • Craig, H., and L. I. Gordon (1965), Deuterium and oxygen 18 variations in the ocean and the marine atmosphere, in Stable Isotopes in Oceanographic Studies and Paleotemperatures, edited by E. Tongiorgi,. pp. 9130, Cons. Naz. Del Ric., Pisa, Italy.
  • Cronblad, H. G., and B. A. Malmgren (1981), Climatically controlled variation of Sr and Mg in Quaternary planktic foraminifera, Nature, 291, 6164.
  • Cronin, T. M., G. S. Dwyer, T. Kamiya, S. Schwede, and D. A. Willard (2003), Medieval Warm Period, Little Ice Age and 20th century temperature variability from Chesapeake Bay, Global Planet. Change, 36, 1729.
  • Dahl-Jensen, D., K. Mosegaard, N. Gundestrup, G. D. Clow, S. J. Johnsen, A. W. Hansen, and N. Ballin (1998), Past temperatures directly from the Greenland ice sheet, Science, 282, 268271.
  • 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.
  • deMenocal, P., J. Ortiz, T. Guilderson, and M. Sarnthein (2000), Coherent high- and low-latitude climate variability during the Holocene Warm Period, Science, 288, 21982202.
  • Dokken, T. M., and E. Jansen (1999), Rapid changes in the mechanism of ocean convection during the last glacial period, Nature, 401, 458461.
  • Elderfield, H., and G. Ganssen (2000), Past temperature and δ18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios, Nature, 405, 442445.
  • Grove, J. M., and R. Switsur (1994), Glacial geological evidence for the Medieval Warm Period, Clim. Change, 24, 143169.
  • Huber, R., H. Meggers, K. H. Baumann, M. E. Raymo, and R. Henrich (2000), Shell size variation of the planktonic foraminifer Neogloboquadrina pachyderma sin. in the Norwegian-Greenland Sea during the last 1.3 Myrs: Implications for paleoceanographic reconstructions, Palaeogeogr. Palaeoclimatol. Palaeoecol., 160(3–4), 193212.
  • Hughes, M. K., and H. F. Diaz (1994), Was there a “Medieval Warm Period”, and if so, where and when? Clim, Change, 26, 109142.
  • Jansen, E., and N. Koç (2000), Century to decadal scale records of Norwegian sea surface temperatures variations of the past 2 millennia, PAGES Newsl., 8, 1314.
  • Keigwin, L. D. (1996), The little ice age and medieval warm period in the Sargasso Sea, Science, 274, 15041508.
  • Kiefer, T., and M. Kienast (2005), Patterns of deglacial warming in the Pacific Ocean: A review with emphasis on the time interval of Heinrich event 1, Quat. Sci. Rev., 24, 10631081.
  • Knudsen, K. L., J. Eiriksson, E. Jansen, H. Jiang, F. Rytter, and E. R. Gudmundsdottir (2004), Paleoceanographic changes off North Iceland through the last 1200 years: Foraminifera, stable isotopes, diatoms and ice rafted debris, Quat. Sci. Rev., 23, 22312246.
  • Koç, N., and E. Jansen (1992), A high-resolution diatom record of the last deglaciation from the SE Norwegian Sea: Documentation of rapid climatic changes, Paleoceanography, 7, 499520.
  • Koç, N., and E. Jansen (2002), Holocene climate evolution of the North Atlantic Ocean and the Nordic Seas: A synthesis of new results, in Climate Development and History of the North Atlantic Realm, edited by G. Wefer, pp. 165173, Springer, New York.
  • Kohfeld, K. E., R. G. Fairbanks, S. L. Smith, and I. D. Walsh (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.
  • Kristensen, D. K., H. P. Sejrup, H. Haflidason, I. M. Berstad, and G. Mikalsen (2004), Eight-hundred-year temperature variability from the Norwegian continental margin and the North Atlantic thermohaline circulation, Paleoceanography, 19, PA2007, doi:10.1029/2003PA000960.
  • Kuroyangi, A., and H. Kawahata (2004), Vertical distribution of living planktonic foraminifera in the seas around Japan, Mar. Micropaleontol., 53, 173196.
  • Lamb, H. H. (1979), Climatic variation and changes in the winds and ocean circulation: The Little Ice Age and the Northeast Atlantic, Quat. Res., 11, 120.
  • 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(16), 23692379.
  • Lea, D. W., P. A. Martin, D. K. Pak, and H. J. Spero (2002), Reconstructing a 350 ky history of sea level using planktonic Mg/Ca and oxygen isotope records from a Cocos Ridge core, Quat. Sci. Rev., 21, 283293.
  • Lea, D. W., D. K. Pak, L. C. Peterson, and K. A. Hughen (2003), Synchroneity of tropical and high-latitude Atlantic temperatures over the last glacial termination, Science, 301, 13611364.
  • Mann, M. E., R. S. Bradley, and M. K. Huges (1999), Northern Hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations, Geophys. Res. Lett., 26(6), 759762.
  • Martin, P. A., D. W. Lea, Y. Rosenthal, N. J. Shackleton, M. Sarnthein, and T. Papenfuss (2002), Quaternary deep sea temperature histories derived from benthic foraminiferal Mg/Ca, Earth Planet. Sci. Lett., 198, 193209.
  • Mashiotta, T. A., D. W. Lea, and H. J. Spero (1999), Glacial-interglacial changes in Subantarctica sea surface temperature and δ18O-water using foraminiferal Mg, Earth Planet. Sci. Lett., 170, 417432.
  • Meland, M., 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.
  • Meland, M. Y., E. Jansen, H. Elderfield, T. M. Dokken, A. Olsen, and R. G. J. Bellerby (2006), Mg/Ca ratios in the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in the northern North Atlantic/Nordic Seas, Geochem. Geophys. Geosyst., 7, Q06P14, doi:10.1029/2005GC001078.
  • Moberg, A., D. M. Sonechkin, K. Holmgren, N. M. Datsenko, and W. Karlén (2005), Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data, Nature, 433, 613617.
  • Nesje, A., and S. O. Dahl (2003), The “Little Ice Age” — Only temperatures? Holocene, 13, 139145.
  • Nilsen, J. E. Ø., and E. Falck (2006), Variations of mixed layer depth and water properties in the Norwegian Sea for the period 1949–1999, Prog. Oceanogr., 70, 5890, doi:10.1016/j.pocean.2006.03.014.
  • National Oceanographic Data Center (1998), NODC (Levitus) World Ocean Atlas 1998, NOAA-CIRES Clim. Diagn. Cent., Boulder, Colo. (Available at http://www.cdc.noaa.gov/cdc/data.nodc.woa98.html).
  • Nürnberg, D. (1995), Magnesium in tests of Neogloboquadrina pachyderma sinistral from high northern and southern latitudes, J. Foraminiferal Res., 25(4), 350368.
  • Nürnberg, D., J. Bijam, and C. Hemleben (1996), Assessing the reliability of magnesium in foraminiferal calcite as a proxy for water mass temperatures, Geochim. Cosmochim. Acta, 60(5), 803814.
  • O'Neil, J. R., R. N. Slayton, and T. K. Mayeda (1969), Oxygen isotope fractionation in divalent metal carbonates, J. Chem. Phys., 51, 55475558.
  • Orvik, K. A., Ø. Skagseth, and M. Mork (2001), Atlantic inflow to the Nordic Seas: Current structure and volume fluxes from moored current meters, VM-ADCP and SeaSoar-CTD observations, 1995–1999, Deep Sea Res., Part I, 48, 937957.
  • Østerhus, S., T. Gammesrød, and R. Hogstad (1996), Ocean Weather Station (66°N, 2°E): The longest existing homogenous time series from the deep ocean, WOCE Newsl. 24/96, Southampton Oceanogr. Cent., Univ. of Southampton, Southampton, England, U. K.
  • Pak, D. K., and J. P. Kennett (2002), A foraminiferal isotopic proxy for upper water mass stratification, J. Foraminiferal Res., 32(3), 319327.
  • Pak, D. K., D. W. Lea, and J. P. Kennett (2004), Seasonal and interannual variation in Santa Barbara Basin water temperatures observed in sediment trap foraminiferal Mg/Ca, Geochem. Geophys. Geosyst., 5, Q12008, doi:10.1029/2004GC000760.
  • Pflaumann, U., J. Duprat, C. Pujol, and L. D. Labeyrie (1996), SIMMAX: A modern analog technique to deduce Atlantic sea surface temperatures from planktonic foraminifera in deep-sea sediments, Paleoceanography, 11, 1535.
  • Risebrobakken, B., E. Jansen, C. Andersson, E. Mjelde, and K. Hevrøy (2003), A high-resolution study of Holocene paleoclimatic and paleoceanographic changes in the Nordic Seas, Paleoceanography, 18(1), 1017, doi:10.1029/2002PA000764.
  • Schmidt, G. A., G. R. Bigg, and E. J. Rohling (1999), Global Seawater Oxygen-18 Database, Goddard Inst. for Space Stud., New York. (Available at http://data.giss.nasa.gov/o18data/).
  • 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, Coll. Int. Cent. Natl. Rec. Sci., 219, 203209.
  • 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.
  • Skinner, L. C., and H. Elderfield (2005), Constraining ecological and biological bias in planktonic foraminiferal Mg/Ca and δ18OC: An inter-species approach to proxy calibration testing, Paleoceanography, 20, PA1015, doi:10.1029/2004PA001058.
  • Smith, L. M., J. Andrews, I. S. Castaneda, G. B. Kristjánsdottir, A. E. Jennings, and Á. E. Sveinbjørnsdottir (2005), Temperature reconstructions for SW and N Iceland waters over the last 10 cal ka based on δ18O records from planktic and benthic foraminifera, Quat. Sci. Rev., 24, 17231740, doi:10.1016/j.quascirev.2004.07.025.
  • Stangeew, E. (2001), Distribution and istotopic compostion of living planktonic foraminifera N. pachyderma (sinistral) and T. quinqueloba in the high latitude North Atlantic, thesis, 90 pp., Christian-Albrechts-Univ., Kiel, Germany.
  • Stuvier, M., P. J. Reimer, E. Bard, J. W. Beck, G. S. Burr, K. A. Hughen, B. Kromer, G. McCormac, J. van der Plicht, and M. Spurk (1998), INTCAL98 radiocarbon age calibration, 24,000–0 cal BP, Radiocarbon, 40, 10411083.
  • Swift, J. H. (1986), The Arctic waters, in The Nordic Seas, edited by B. G. Hurdell, pp. 129153, Springer, New York.
  • Széréméta, N., F. Bassinot, Y. Balut, L. Labyrie, and M. Pagel (2004), Oversampling of sedimentary series collected by giant piston corer: Evidence and corrections based on 3. 5–kHz chirp profiles, Paleoceanography, 19, PA1005, doi:10.1029/2002PA000795.
  • Volkmann, R., and M. Mensch (2001), Stable isotope composition (delta O-18, delta C-13) of living planktic foraminifers in the outer Laptev Sea and the Fram Strait, Mar. Micropaleontol., 42(3–4), 163188.
  • von Langen, P. J., D. K. Pak, H. J. Spero, and D. W. Lea (2005), Effects of temperature on Mg/Ca in neogloboquadrined shells determined by live culturing, Geochem. Geophys. Geosyst., 6(10), Q10P03, doi:10.1029/2005GC000989.
  • von Storch, H., E. Zorita, J. M. Jones, Y. Dimitriev, F. Gonzalez-Rouco, and S. F. B. Tett (2004), Reconstructing past climate from noisy data, Science, 306, 679682.