Hostname: page-component-586b7cd67f-dsjbd Total loading time: 0 Render date: 2024-11-24T04:34:40.471Z Has data issue: false hasContentIssue false
  • English
  • Français

Formal Status and Vegetational Development of the Eemian Interglacial in Northwestern and Southern Europe

Published online by Cambridge University Press:  20 January 2017

Charles Turner
Charles Turner*
Affiliation:
Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, United Kingdom
*
1To whom correspondence should be addressed. [email protected].
Get access Rights & Permissions [Opens in a new window]

Abstract

The terms Eem and Eemian have been applied to lithostratigraphic, chronostratigraphic, and biostratigraphic aspects of the last interglacial in western Europe. Eemian vegetational successions show strong uniformity at sites from western France across the North European Plain to Poland, suggesting, by comparison with the Holocene, that major pollen zones are broadly synchronous. South of the Alps and Pyrenees, a different vegetational succession is observed with no evidence for a substage of post-temperate cooling.

Keywords

Eemianlast interglacialstratotypevegetational development
Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 1 , July 2002 , pp. 41 - 44
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Behre, K.E., and Lade, U. Eine Folge von Eem und 4 Weichsel-Interstadialen in Oerel/Niedersachsen und ihr Vegetationsablauf. Eiszeitalter und Gegenwart 36, (1986). 11 36.Google Scholar
Caspers, G. Die eem- und weichselzeitliche Hohlform von Gross Todtshorn (Kr. Harburg; Niedersachsen)—Geologische und palynologische Untersuchungen zu Vegetation und Klimaverlauf der letzten Kaltzeit. Freund, H., and Caspers, G. Vegetation und Paläoklima der Weichsel-Kaltzeit im nordlichen Mitteleuropa—Ergebnisse paläobotanischer, -faunistischer und geologischer Untersuchungen. (1997). 7 59.Google Scholar
Cheddadi, R., Mamakowa, K., Guiot, J., de Beaulieu, J.-L., Reille, M., Andrieu, V., Granoszewski, W., and Peyron, O. Was the climate of the Eemian stable? A quantitative climate reconstruction from seven European pollen records. Palaeogeography, Palaeoclimatology, Palaeoecology 143, (1998). 73 85.Google Scholar
de Beaulieu, J.L., and Reille, M. A long Upper Pleistocene pollen record from Les Echets, near Lyon, France. Boreas 13, (1984). 111 132.Google Scholar
de Beaulieu, J.L., and Reille, M. The last climatic cycle at La Grande Pile (Vosges). A new pollen profile. Quaternary Science Reviews 11, (1992). 431 438.Google Scholar
de Beaulieu, J.L., and Reille, M. Long Pleistocene pollen sequences from the Velay Plateau (Massif Central, France). I Ribains maar. Vegetation History and Archaeobotany 1, (1992). 233 242.Google Scholar
Follieri, M., Magri, D., and Sadori, L. 250,000 year pollen record from Valle di Castiglione (Roma). Pollen et Spores 30, (1988). 329 356.Google Scholar
Frenzel, B., and Bludau, W. On the duration of the interglacial to glacial transition at the end of the Eemian Interglacial (deep sea stage 5 E): Botanical and sedimentological evidence. Berger, W.H., and Labeyrie, L.D. Abrupt Climate Change. (1987). Reidel, Dordrecht. 151 162.Google Scholar
Frogley, M.R., Tzedakis, P.C., and Heaton, T.H.E. Climate variability in northwest Greece during the Last Interglacial. Science 285, (1999). 1886 1889.CrossRefGoogle ScholarPubMed
Grüger, E. Die Seeablagerungen vom Samerberg Obb, und ihre Stellung im Jungpleistozän. Eiszeitalter und Gegenwart 29, (1979). 23 34.Google Scholar
Grüger, E. Palynostratigraphy of the last Interglacial cycle in Germany. Quaternary International 3–4, (1989). 69 79.Google Scholar
Hahne, J., Kemle, S., Merkt, J., and Meyer, K.-D. Eem-, weichsel- und saalezeitliche Ablagerungen der Bohrung “Quakenbrück GE 2”. Geologisches Jahrbuch A 134, (1994). 9 69.Google Scholar
Harting, P. De bodem van het Eemdal. Verslagen en Mededelingen van de Koninklijke Akademie van Wetenschappen, afdeling. Natuurkunde II 8, (1874). 282 290.Google Scholar
Huntley, B., and Birks, H.J.B. An atlas of past and present pollen maps for Europe: 0-13,000 years ago. (1983). Cambridge Univ. Press, Cambridge.Google Scholar
Menke, B., and Tynni, R. Das Eeminterglazial und das Weichselfrühglazial von Rederstall/Dittmarschen und ihre Bedeutung für die mitteleuropäische Jungpleistozängliederung. Geologisches Jahrbuch A 76, (1984). 3 120.Google Scholar
Müller, H. Pollenanalytische Untersuchungen und Jahresschichten-zählungen an der eemzeitlichen Kieselgur von Bispingen/Luhe. Geologisches Jahrbuch A 21, (1974). 149 169.Google Scholar
Müller, U. Die Vegetations- und Klimaentwicklung im jüngeren Quartär anhand ausgewählter Profile aus dem südwestdeutschen Alpenvorland. Tübinger geowissenschaftliche Arbeiten D No. 7, (2001). 118 Google Scholar
Reille, M., de Beaulieu, J.-L., Andrieu, V., Guenet, P., and Goeury, C. A long pollen record from Lac du Bouchet, Massif, central France: For the period ca. 325 to 100 ka BP (OIS 9c to OIS 5e). Quaternary Science Reviews 17, (1998). 1107 1124.Google Scholar
Salvador, A. International Stratigraphic Guide. (1994). The International Union of Geological Sciences and the Geological Society of America Inc, p. 214 Google Scholar
Sánchez Goñi, M.F., Eynaud, F., Turon, J.-L., and Shackleton, N.J. High resolution palynological record off the Iberian margin: Direct land-sea correlation for the Last Interglacial complex. Earth and Planetary Science Letters 171, (1999). 123 137.CrossRefGoogle Scholar
Sánchez Goñi, M.F., Turon, J.-L., Eynaud, F., and Shackleton, N.J. Direct land/sea correlation of the Eemian, and its comparison with the Holocene: a high-resolution palynological record off the Iberian margin. Geologie en Mijnbouw/Netherlands Journal of Geosciences 79, (2000). 345 354.Google Scholar
Simpson, I.M., and West, R.G. On the stratigraphy and palaeobotany of a late-Pleistocene organic deposit at Chelford, Cheshire. New Phytologist 57, (1958). 239 250.CrossRefGoogle Scholar
Turner, C. The Eemian Interglacial in the North European Plain and adjacent areas. Geologie en Mijnbouw/Netherlands Journal of Geosciences 79, (2000). 217 231.Google Scholar
Turon, J.-L. Direct land/sea correlations in last interglacial complex. Nature 309, (1984). 673 676.CrossRefGoogle Scholar
Tzedakis, P.C. Vegetation change through glacial-interglacial cycles: A long pollen sequence perspective. Philosophical Transactions of the Royal Society of London B 345, (1994). 403 432.Google Scholar
van der Heide, S., and Zagwijn, W.H. Stratigraphical Nomenclature of the Quaternary deposits in the Netherlands. Mededelingen Geologische Stichting NS 18, (1967). 23 28.Google Scholar
van der Vlerk, I.M., and Florschütz, F. The palaeontological base of the subdivision of the Pleistocene in the Netherlands. Verhandelingen Koninklijke Nederlandse Akademie van Wetenschappen, Afdeling Natuurkunde 20, (1953). 1 58.Google Scholar
van Leeuwen, R.J.W., Beets, D.J., Bosch, J.H.A., Burger, A.W., Cleveringa, P., van Harten, D., Herngreen, G.F.W., Kruk, R.W., Langereis, C.G., Meijer, T., Pouwer, R., and de Wolf, H. Stratigraphy and integrated facies analysis of the Saalian and Eemian sediments in the Amsterdam-Terminal borehole, the Netherlands. Geologie en Mijnbouw/Netherlands Journal of Geosciences 79, (2000). 161 196.CrossRefGoogle Scholar
Wijmstra, T.A. Palynology of the first 30 metres of a 120 m deep section in Northern Greece. Acta Botanica Neerlandica 18, (1969). 511 527.CrossRefGoogle Scholar
Wijmstra, T.A., and Smit, A. Palynology of the middle part (30–78 metres) of the 120 m deep section in Northern Greece (Macedonia). Acta Botanica Neerlandica 25, (1976). 297 312.Google Scholar
Woillard, G.M. Grande Pile peat bog: A continuous pollen record from the last 140,000 years. Quaternary Research 9, (1978). 1 21.Google Scholar
Woillard, G.M. Abrupt end of the last interglacial s.s. in north-east France. Nature 281, (1979). 558 562.CrossRefGoogle Scholar
Zagwijn, W.H. Vegetation, climate and radiocarbon datings in the Late Pleistocene of the Netherlands. Part 1: Eemian and Early Weichselian. Mededelingen Geologische Stichting NS 14, (1961). 15 45.Google Scholar
Zagwijn, W.H. Indeling van het Kwartair op grond van veranderingen in vegetatie en klimaat [Subdivision of the Quaternary based upon changes in vegetation and climate]. Zagwijn, W.H., and van Staalduinen, C.J. Toelichting bij Geologische overzichtskaarten van Nederland. (1975). Rijks Geologische Dienst, Haarlem. 109 114.Google Scholar
Zagwijn, W.H. An analysis of Eemian climate in Western and Central Europe. Quaternary Science Reviews 15, (1996). 451 469.Google Scholar