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Last Interglacial and Early Glacial Circulation in the Northern North Atlantic Ocean

Published online by Cambridge University Press:  20 January 2017

Karen-Luise Knudsen ,
Marit-Solveig Seidenkrantz  and
Peter Kristensen
Karen-Luise Knudsen*
Affiliation:
Department of Earth Sciences, University of Aarhus, DK-8000, Aarhus C, Denmark
Marit-Solveig Seidenkrantz
Affiliation:
Department of Earth Sciences, University of Aarhus, DK-8000, Aarhus C, Denmark
Peter Kristensen
Affiliation:
Department of Earth Sciences, University of Aarhus, DK-8000, Aarhus C, Denmark
*
1To whom correspondence should be addressed. [email protected].
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Abstract

Studies of marine records from the northwestern European shelf and the northern North Atlantic suggest that last interglacial environments were less stable in this area than in the mid-latitude Atlantic. The influx of Atlantic water masses to the northern North Atlantic was generally higher, and the meridional temperature gradient was steeper, during the last interglaciation than during the Holocene. Strong north–south sea-surface-temperature gradients during the early Weichselian indicate a generally low influx of Atlantic water to the northern North Atlantic, even during interstades.

Keywords

Last interglacialNordic seasclimate oscillationsforaminifera
Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 1 , July 2002 , pp. 22 - 26
Copyright
University of Washington

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References

Bauch, H.A., Erlenkeuser, H., Fahl, K., Spielhagen, R.F., Weinelt, M.S., Andruleit, H., and Henrich, R. Evidence for a steeper Eemian than Holocene sea surface temperature gradient between Arctic and sub-Arctic regions. Palaeogeography, Palaeoclimatology, Palaeoecology 145, (1999). 95 117.CrossRefGoogle Scholar
Chappell, J., and Shackleton, N.J. Oxygen isotopes and sea level. Nature 324, (1986). 137 140.Google Scholar
Quaternary Research 21, (1984). 123 224.Google Scholar
Cortijo, E., Duplessy, J.-C., Labeyrie, L., Leclaire, H., Duprat, J., and Weering, T.C.E.van Eemian cooling in the Norwegian Sea and North Atlantic Ocean preceeding continental ice-sheet growth. Nature 372, (1994). 446 449.CrossRefGoogle Scholar
Fronval, T., and Jansen, E. Rapid changes in ocean circulation and heat flux in the Nordic seas during the last interglacial period. Nature 383, (1996). 806 810.Google Scholar
Fronval, T., and Jansen, E. Eemian and early Weichselian (140-60 ka) paleoceanography and paleoclimate in the Nordic seas with comparisons to Holocene conditions. Paleoceanography 12, (1997). 443 462.CrossRefGoogle Scholar
Fronval, T., Jansen, E., Haflidason, H., and Sejrup, H.P. Variability in surface and deep water conditions in the Nordic seas during the Last Interglacial period. Quaternary Science Reviews 17, (1998). 963 985.Google Scholar
Funder, S, Demidov, I, and Yelovicheva, Y. (In press), Hydrography and mollusc faunas of the Baltic and the White Sea-North Sea seaway in the Eemian, Palaeogeography, Palaeoclimatology, Palaeoecology.Google Scholar
Johnsen, S.J., Clausen, H.B., Dansgaard, W., Gundestrup, N.S., Hammer, C.U., and Tauber, H. The Eem stable isotope record along the GRIP ice core and its interpretation. Quaternary Research 43, (1995). 117 124.Google Scholar
Kellogg, T.B. Paleoclimatology and paleo-oceanography of the Norwegian and Greenland seas: Glacial-interglacial contrasts. Boreas 9, (1980). 115 137.Google Scholar
Kristensen, P., Knudsen, K.L., Lykke-Andersen, H., Nørmark, E., Peacock, J.D., and Sinnoth, A. Interglacial and glacial climate oscillations in a marine shelf sequence from northern Denmark—A multidisciplinary study. Quaternary Science Reviews 17, (1998). 813 837.Google Scholar
Kristensen, P., Gibbard, P.L., Knudsen, K.L., and Ehlers, J. Late Pleistocene interglacial and glacial deposits at Ristinge Klint, Langeland, Denmark. Boreas 29, (2000). 103 116.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C., and Shackleton, N.J. Age dating and orbital theory of the Ice Ages: Development of a high-resolution 0 to 300,000-year chronostratigraphy. Quaternary Research 27, (1987). 1 29.Google Scholar
McManus, J.F., Bond, G.C., Broecker, W.S., Johnsen, S., Labeyrie, L., and Higgins, S. High-resolution climate records from the North Atlantic during the last interglacial. Nature 371, (1994). 326 329.Google Scholar
Müller, H. Pollenanalytische Untersuchungen und Jahresschichten- zählungen an der eem-zeitlichen Kieselgur von Bispingen/Luhe. Geologisches Jahrbuch A21, (1974). 149 169.Google Scholar
Seidenkrantz, M.-S., and Knudsen, K.L. Eemian climatic and hydrographical instability on a marine shelf in Northern Denmark. Quaternary Research 47, (1997). 218 234.Google Scholar
Seidenkrantz, M.-S., Kristensen, P., and Knudsen, K.L. Marine evidence for climatic instability during the last interglacial in shelf records from northwest Europe. Journal of Quaternary Science 10, (1995). 77 82.Google Scholar
Seidenkrantz, M.-S., Knudsen, K.L., and Kristensen, P. Marine Late Saalian to Eemian environments and climatic variability in the Danish area. Geologie en Mijnbouw/The Netherlands Journal of Geosciences 79, (2000). 335 343.Google Scholar
Sejrup, H.P., and Larsen, E. Eemian-Early Weichselian N-S temperature gradients; North Atlantic-northwestern Europe. Quaternary International 10–12, (1991). 161 166.Google Scholar
Sejrup, H.P., Haflidason, H., Kristensen, D.K., and Johnsen, S.J. Last interglacial and Holocene climatic development in the Norwegian Sea Region: Ocean front movements and ice-core data. Journal of Quaternary Science 10, (1995). 385 390.Google Scholar
Weaver, A.J., and Hughes, T.M.C. Rapid interglacial climate fluctuation driven by North Atlantic ocean circulation. Nature 367, (1994). 447 450.Google Scholar
Woillard, G.M. Grande Pile peat bog: A continuous pollen record for the last 140,000 years. Quaternary Research 9, (1978). 1 21.Google Scholar
Zagwijn, W.H. The Pleistocene of The Netherlands with special reference to glaciation and terrace formation. Quaternary Science Reviews 5, (1996). 341 345.Google Scholar
Zans, V. Das letztinterglaziale Portlandia-Meer des Balticums. Bulletin de la Commision géologique de Finlande 115, (1936). 231 250.Google Scholar