Hostname: page-component-78c5997874-j824f Total loading time: 0 Render date: 2024-11-15T01:26:50.676Z Has data issue: false hasContentIssue false
  • English
  • Français

Marine late Saalian to Eemian environments and climatic variability in the Danish shelf area

Published online by Cambridge University Press:  01 April 2016

Marit-Solveig Seidenkrantz ,
Karen Luise Knudsen  and
Peter Kristensen
Marit-Solveig Seidenkrantz*
Affiliation:
Department of Earth Sciences, University of Aarhus, DK-8000 ÅRHUS C, Denmark
Karen Luise Knudsen
Affiliation:
Department of Earth Sciences, University of Aarhus, DK-8000 ÅRHUS C, Denmark
Peter Kristensen
Affiliation:
Department of Earth Sciences, University of Aarhus, DK-8000 ÅRHUS C, Denmark
*
1 Corresponding author
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

The marine Eemian (marine oxygen-isotope substage 5e: MIS 5e) is represented by shallow-water deposits in southern and western Denmark, while relatively deep-water environments occurred to the north and north-east, where complete interglacial successions seem to be present. We present an overview of the marine Eemian deposits in Denmark, and discuss in more detail indications of climate variability, both for the late Saalian and within the Eemian.

Keywords

coastlineEemianForaminiferamarine environmentpaleogeographypaleotemperaturestable isotopes
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 79 , Issue 2-3 , August 2000 , pp. 335 - 343
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2000

References

Adkins, J.F., Boyle, E.A., Keigwin, L. & Cortijo, E., 1997. Variability of the North Atlantic thermohaline circulation during the last interglacial period. Nature 390: 154–156.CrossRefGoogle Scholar
Bauch, H.A., Erlenkeuser, H., Fahl, K., Spielhagen, R.F., Weinelt, M.S., Andruleit, H. & Henrich, R., 1999. Evidence for a steeper Eemian than Holocene sea surface temperature gradient between Arctic and sub-Arctic regions. Palaeogeography Palaeoclimatology Palaeoecology 144: 95–117.Google Scholar
Behre, K.-E., Menke, B. & Streif, H., 1979. The Quaternary geological development of the German part of the North Sea. In: Oele, E., Schüttenhelm, R.T.E. & Wiggers, A.J. (eds.): The Quaternary history of the North Sea. Acta Universitatis Upsaliensis, Symposia Universitatis Upsaliensis Annum Quingentesimum Celebrantis (Uppsala) 2: 85–113.Google Scholar
Björck, S., Noe-Nygaard, N., Wollin, J., Houmark-Nielsen, M., Hansen, H.J. & Snowball, I., 2000. Eemian lake development, hydrology and climate – a multi-stratigraphic study of the Hollerup site in Denmark. Quaternary Science Reviews 19: 509–536.Google Scholar
Chapell, J. & Shackleton, N.J., 1986. Oxygen isotopes and sea level. Nature 324: 137–140.CrossRefGoogle Scholar
CPM (CLIMAP Project Members), 1984. The last interglacial ocean. Quaternary Research 21: 123–224.CrossRefGoogle Scholar
Craig, H. & Gordon, L.I., 1965. Deuterium and oxygen 18 variations in the ocean and the marine atmosphere. In: Tongiorgi, E. (ed.): Stable isotopes in océanographie studies and Paleotemperatures. Consigilo Nazionale Delle Ricerche, Laboratorio di Geologia Nucleare (Pisa): 9–130.Google Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N.S., Hammer, CU., Hvidbjerg, C.S., Steffensen, J.R., Sveinbjörnsdóttir, A.E., Jouzel, J. & Bond, G., 1993. Evidence for general instability of past climate from a 250-kyr ice core record. Nature 364: 218–220.CrossRefGoogle Scholar
Donner, J., 1995. The Quaternary history of Scandinavia. Cambridge University Press (Cambridge): 200 pp.Google Scholar
Feyling-Hanssen, R.W., 1955. Stratigraphy of the marine Late-Pleistocene of Billefjorden, Vestspitsbergen. Norsk Polarinstitutt Skrifterl 07: 1–186.Google Scholar
Field, M.H., Huntley, B. & Müller, H., 1994. Eemian climate fluctuations observed in a European pollen record. Nature 371: 779–783.CrossRefGoogle Scholar
Forsström, L., Aalto, M., Eronen, M. & Grönlund, T., 1988. Strati-graphical evidence for Eemian crustal movements and relative sea-level changes in eastern Fennoscandia. Palaeogeography Palaeoclimatology Palaeoecology 68: 317–335.Google Scholar
Fronval, T. & Jansen, E., 1996. Rapid changes in ocean circulation and heat flux in the Nordic seas during the last interglacial period. Nature 383: 806–810.CrossRefGoogle Scholar
Fronval, T. & Jansen, E., 1997. Eemian and early Weichselian (140-60 ka) paleoceanography and paleoclimate in the Nordic seas with comparisons to Holocene conditions. Paleoceanography 12: 443–462.Google Scholar
Fronval, T, Jansen, E., Haflidason, H. & Sejrup, H.P., 1998. Variability in surface and deep water conditions in the Nordic seas during the Last Interglacial period. Quaternary Science Reviews 17:963–985.Google Scholar
Gallup, CD., Edwards, R.L. & Johnson, R.G., 1994. The timing of high sea levels over the past 200,000 years. Science 263: 796–800.CrossRefGoogle ScholarPubMed
Glaister, C.G. & Gibbard, P.L., 1998. Pollen stratigraphy of Late Pleistocene marine sediments at Norre Lyngby and Skagen, North Denmark. Quaternary Science Reviews 17: 839–854.Google Scholar
GRIP Members 1993. Climate instability during the last inter-glacial period recorded in the GRIP ice core. Nature 364: 203–207.Google Scholar
Jessen, K. & Milthers, V., 1928. Stratigraphical and paleontological studies of interglacial fresh-water deposits in Jutland and Northwest Germany. Geological Survey of Denmark, II Series 48: 1–379.Google Scholar
Johnsen, S.J., Clausen, H.B., Dansgaard, W., Gundestrup, N.S., Hammer, C.U. & Tauber, H., 1995. The Eem stable isotope record along the GRIP ice core and its interpretation. Quaternary Research 43: 117–124.Google Scholar
Knudsen, K.L., 1984. Foraminiferal stratigraphy in a marine Eemian-Weichselian sequence at Apholm, North Jutland. Bulletin of the Geological Society of Denmark 32: 169–180.CrossRefGoogle Scholar
Knudsen, K.L., 1985. Foraminiferal faunas in Eemian deposits of the Oldenbüttel area, Nord-Ostsee-Kanal (Kiel Canal). Geologisches Jahrbuch A 86: 27–47.Google Scholar
Knudsen, K.L., 1992. A long marine Eemian-Weichselian shelf record in North Denmark, Scandinavia. In: Kukla, G.J. & Went, E. (eds.): Start of a glacial. NATO ASI Series I 3. Springer-Ver-lag (Berlin-Heidelberg): 157–171.Google Scholar
Knudsen, K.L., Conradsen, K., Heier-Nielsen, S. & Seidenkrantz, M.-S., 1996. Palaeoenvironments in the Skagerrak-Kattegat basin in the eastern North Sea during the déglaciation. Boreas 25: 65–77.Google Scholar
Knudsen, K.L. & Lykke-Andersen, A.-L., 1982. Foraminifera in Late Saalian, Eemian, Early and Middle Weichselian of the Skaerumhede I boring. Bulletin of the Geological Society of Denmark 30: 97–109.CrossRefGoogle Scholar
Knudsen, K.L., Seidenkrantz, M.-S. & Kristensen, P. (in press). The northern North Atlantic circulation during the last inter-glacial and Early Glacial. Quaternary Research.Google Scholar
Konradi, P.B., 1976. Foraminifera in Eemian deposits at Sten-sigmose, southern Jutland. Geological Survey of Denmark, II Series 105: 1–57.Google Scholar
Kosack, B. & Lange, W., 1985. Das Eem-Vorkommen von Offen-büttel/Schmttlohe und die Ausbreitung des Eem-Meeres zwis-chen Nord-und Ostsee. Geologisches Jahrbuch A 86: 3–17.Google Scholar
Kristensen, P., Gibbard, P., Knudsen, K.L. & Ehlers, J. (in press). Last interglacial stratigraphy at Ristinge Klint, South Denmark. Boreas 29.Google Scholar
Kristensen, P., Knudsen, K.L., Lykke-Andersen, H., Nørmark, E., Peacock, J.D. & Sinnoth, A., 1998. Interglacial and glacial climate oscillations in a marine shelf sequence from northern Denmark – a multidisciplinary study. Quaternary Science Reviews 17:813–837.CrossRefGoogle Scholar
Krog, H., 1979. Late Pleistocene and Holocene shorelines in western Denmark. In: Oele, E., Schüttenhelm, R.T.E. & Wiggers, A. J. (eds.): The Quaternary history of the North Sea. Acta Universi-tatis Upsaliensis, Symposia Universitatis Upsaliensis Annum Quingentesimum Celebrantis (Uppsala) 2: 75–83.Google Scholar
Larsen, E,. Sejrup, H.P., Johnsen, S.J. & Knudsen, K.L., 1995. Do Greenland ice cores reflect NW European interglacial climate variations? Quaternary Research 43: 125–132.Google Scholar
Lykke-Andersen, H., 1987. Thickness of Quaternary deposits and their relation to the pre-Quaternary in the Fennoscandian border zone in Kattegat andVendsyssel. Boreas 16: 369–371.CrossRefGoogle Scholar
Lykke-Andersen, H., Knudsen, K.L. & Christensen, C., 1993. The Quaternary of the Kattegat area, Scandinavia: a review. Boreas 22:269–281.CrossRefGoogle Scholar
McManus, J.F., Bond, G.C., Broecker, W.S., Johnsen, S., Labeyrie, L. & Higgins, S., 1994. High-resolution climate records from the North Atlantic during the last interglacial. Nature 371: 326–329.Google Scholar
Nordmann, V., 1928. La position stratigraphique des dépots d’Eem. Geological Survey of Denmark, II Series 47: 1–81.Google Scholar
Penney, D.N., 1989. Microfossils (Foraminifera, Ostracoda) from an Eemian (last interglacial) tidal flat in south-west Denmark. Quaternary International 3/4: 85–91.Google Scholar
Pisias, N.G., Martinson, D.G., Moore, T.C. Jr., Shackleton, N.J., Prell, W., Hays, J. & Boden, G., 1984. High resolution strati-graphic correlation of benthic oxygen isotope records spanning the last 300,000 years. Marine Geology 56: 119–136.Google Scholar
Poole, D.A.R., 1994. Neogene and Quaternary palaeoenvironment on the north Norwegian shelf. Unpublished Ph.D. thesis University of Tromso: 141 pp.Google Scholar
Raukas, A., 1991. Eemian interglacial record in the northwestern European part of the Soviet Union. Quaternary International 10/12: 183–189.Google Scholar
Rohde, J., 1987. The large-scale circulation in the Skagerrak; interpretation of some observations. Tellus 39A: 245–253.Google Scholar
Seidenkrantz, M.-S., 1993a. Benthic foraminiferal and stable isotope evidence for a “Younger Dryas-style” cold spell at the Saalian-Eemian transition, Denmark. Palaeogeography Palaeoclimatology Palaeoecology 102: 103–120.Google Scholar
Seidenkrantz, M.-S., 1993b. Subrecent changes in the foraminiferal distribution in the Kattegat and the Skagerrak, Scandinavia: anthropogenic influence and natural causes. Boreas 22: 383–395.Google Scholar
Seidenkrantz, M.-S., Bornmalm, L., Johnsen, S.J., Knudsen, K.L., Kuijpers, A., Lauritzen, S.-E., Leroy, S.A.G., Mergeal, I., Schwegeer, C. & Van Vliet-Lanoë, B., 1996. Two-step déglaciation at the oxygen isotope stage 6/5e transition: the Zeifen-Kat-tekat climate oscillation. Quaternary Science Reviews 15: 63–75.CrossRefGoogle Scholar
Seidenkrantz, M.-S. & Knudsen, K.L., 1994. Marine high resolution records of the last interglacial in Northwest Europe: a review. Géographie Physique et Quaternaire 48: 157–168.Google Scholar
Seidenkrantz, M.-S. & Knudsen, K.L., 1997. Eemian climatic and hydrographical instability on a marine shelf in Northern Denmark. Quaternary Research 47: 218–234.Google Scholar
Seidenkrantz, M.-S., Kristensen, P. & Knudsen, K.L., 1995. Marine evidence for climatic instability during the last interglacial in shelf records from northwest Europe. Journal of Quaternary Science 10:77–82.Google Scholar
Sejrup, J.P. & Knudsen, K.L., 1999. Geochronology and palaeoenvironment of marine Quaternary deposits in Denmark; new evidence from northern Jutland. Geological Magazine 136: 561–578.Google Scholar
Sejrup, H.P. & Larsen, E., 1991. Eemian-Early Weichselian N-S temperature gradients; North Atlantic-NW Europe. Quaternary International 10/12: 161–166.Google Scholar
Shackleton, N.J., 1974. Attainment of isotopie equilibrium between ocean water and the benthonic Foraminifera genus Uvigerina: isotopie changes in the ocean during the last glacial. In: Labeyrie, L. (ed.): Variation du climat au cours duj Pleistocène. Colloques Internationaux du Centre Nationale de la Recherche Scientifique 219: 203–209.Google Scholar
Shackleton, N.J., 1987. Oxygen isotopes, ice volume aád sea level. Quaternary Science Reviews 6: 183–190.CrossRefGoogle Scholar
Svansson, A., 1975. Physical and chemical oceanography of the Skagerrak and the Kattegat I: Open sea conditions. Fishery Board of Sweden, Institute of Marine Research Report 1: 88 pp.Google Scholar
Van Voorthuysen, J.H., 1957. Foraminiferen aus dem Eemian (Riss-Würm Interglacial) in der Bohrung Amersfoort I (locus typicus). Mededelingen van de Geologische Stichting, Nieuwe Serie 11:27–39.Google Scholar
Weaver, A.J. & Hughes, T.M.C., 1994. Rapid interglacial climate fluctuation driven by North Atlantic ocean circulation. Nature 367: 447–450.CrossRefGoogle Scholar
Zagwijn, W.H., 1986. The Pleistocene of The Netherlands with special reference to glaciation and terrace formation. Quaternary Science Reviews 5: 341–345.CrossRefGoogle Scholar
Zagwijn, W.H., 1996. An analysis of Eemian climate in Western and central Europe. Quaternary Science Reviews 15: 451–469.Google Scholar
Zans, V, 1936. Das letztinterglaziale Portlandia-Meer des Balti-cums. Bulletin de la Commission Géologique de Finlande 115: 231–250.Google Scholar