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When did the Last Interglacial end?

Published online by Cambridge University Press:  20 January 2017

R.P. Suggate
R.P. Suggate*
Affiliation:
New Zealand Geological Survey, P.O. Box 30368, Lower Hutt, New Zealand.
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Abstract

Disagreement on the time of the end of the Last Interglacial stems from lack of an agreed definition of an Interglacial. Although strictly a climatic episode, “Interglacial” as commonly used is essentially a chronologic unit equivalent to an Age, corresponding in time range to the chronostratigraphic unit Stage.

The name “Last Interglacial” has gained a global connotation so that its definition must take into account global rather than local effects of temperature fluctuations. An Interglacial begins with a warming to full interglacial warmth (as warm as the present day). It continues until a cooling of full glacial severity occurs, and includes any lesser coolings within a period of fluctuating climate. Such lesser coolings are recorded, particularly in deep-sea cores, following a period of warmth about 125,000 y.a. The cooling that led to the next full glacial cold began about 50,000 yr later. The Last Interglacial lasted from about 128,000 to 73,000 yr BP, equivalent to stage 5 of Shackleton and Opdyke.

Type
Original Articles
Information
Quaternary Research , Volume 4 , Issue 3 , September 1974 , pp. 246 - 252
Copyright
University of Washington

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References

Broecker, W.S., Van Donk, J., (1970). Insolation changes, ice volume, and the 18O record in deep sea cores. Reviews of Geophysics and Space Physics 8, 169–198.CrossRefGoogle Scholar
Butzer, K.W., Cuerda, J., (1962). Coastal stratigraphy of southern Mallorca and its implication for the Pleistocene chronology of the Mediterranean Sea. Journal of Geology 70, 398–416.CrossRefGoogle Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Langway, C.C., (1972). Speculation about the next glaciation. Quaternary Research 2, 396–398.Google Scholar
Emiliani, C., (1955). Pleistocene temperatures. Journal of Geology 63, 538–578.CrossRefGoogle Scholar
Emiliani, C., (1972). Quaternary hypisthermals. Quaternary Research 2, 270–273.Google Scholar
Ericson, D.B., Ewing, M., Wollin, G., Heezen, B.C., (1961). Atlantic deep-sea sediment cores. Geological Society of America Bulletin 72, 173–286.CrossRefGoogle Scholar
Fairbridge, R.W., (1972). Climatology of a glacial cycle. Quaternary Research 2, 283–302.CrossRefGoogle Scholar
Hayes, J.D., Perruza, A., (1972). The significance of calcium carbonate oscillations in eastern equatorial Atlantic deep sea sediments for the end of the Holocene warm interval. Quaternary Research 2, 355–362.Google Scholar
Jessen, K., Milthers, V., (1928). Stratigraphic and paleontological studies of interglacial freshwater deposits in Jutland and northwest Germany. Danmarks Geologiske Undersögelse 2, 48.Google Scholar
Kennett, J.P., Huddlestun, P., (1972). Abrupt climatic change at 90,000 yr BP: Faunal evidence from Gulf of Mexico cores. Quaternary Research 2, 384–395.Google Scholar
Kukla, G.J., Kočí, A., (1972). End of the last interglacial in the loess record. Quaternary Research 2, 374–383.CrossRefGoogle Scholar
Kukla, G.J., Kukla, H.J., (1972). Insolation regime of interglacials. Quaternary Research 2, 412–424.CrossRefGoogle Scholar
Kukla, G.J., Matthews, R.K., Mitchell, J.M., (1972). The end of the present interglacial. Quaternary Research 2, 261–269.Google Scholar
Kukla, J., (1961). Quaternary sedimentation cycle. Survey of Czechoslovak Quarternary. Cwartorzed Europy Srodkowej i Wschodniej. VI INQUA Congress. Institut Geologiczny, Prace 34, 145–154(Warszawa).Google Scholar
McIntyre, A., Ruddiman, W.F., (1972). Northeast Atlantic post-Eemian paleoceanography: a predictive analog of the future. Quaternary Research 2, 350–354.CrossRefGoogle Scholar
Matthews, R.K., (1972). Dynamics of the oceancryosphere system: Barbados data. Quaternary Research 2, 368–373.CrossRefGoogle Scholar
Mesolella, K.J., Matthews, R.K., Broecker, W.S., Thurber, D.L., (1969). The astronomical theory of climatic changes: Barbados data. Journal of Geology 77, 250–274.CrossRefGoogle Scholar
Mörner, N-A., (1972). When will the present interglacial end?. Quaternary Research 2, 341–349.Google Scholar
Richmond, G.M., (1972). Appraisal of the future climate of the Holocene in the Rocky Mountains. Quaternary Research 2, 315–322.CrossRefGoogle Scholar
Sancetta, C., Imbrie, J., Kipp, N.G., McIntyre, A., Ruddiman, W.F., (1972). Climatic record in North Atlantic deep sea core V23-82: Comparison of the last and present interglacials based on quantitative time series. Quaternary Research 2, 363–367.Google Scholar
Shackleton, N.J., (1969). The last interglacial in the marine and terrestrial records. Proceedings of the Royal Society of London B 174, 135–154.Google Scholar
Shackleton, N.J., Opdyke, N.D., (1973). Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238: Oxygen isotope temperatures and ice volumes on a year and a 106 year 105 scale. Quaternary Research 3, 39–55.Google Scholar
Suggate, R.P., (1962). Time-stratigraphic subdivision of the Quaternary as viewed from New Zealand. Quaternaria 5, 5–17.Google Scholar
Suggate, R.P., (1965). The definition of “Interglacial”. Journal of Geology 73, 619–626.Google Scholar
Wright, H.E. Jr., (1972). Interglacial and postglacial climates. The pollen record. Quaternary Research 2, 274–282.CrossRefGoogle Scholar