Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-10T09:56:45.815Z Has data issue: false hasContentIssue false
  • English
  • Français

The Stability and the Abrupt Ending of the Last Interglaciation in Southeastern Siberia

Published online by Cambridge University Press:  20 January 2017

Alexander A. Prokopenko ,
Eugene B. Karabanov ,
Douglas F. Williams  and
Galina K. Khursevich
Alexander A. Prokopenko*
Affiliation:
Baikal Drilling Project, Department of Geological Sciences, University of South Carolina, Columbia, South Carolina, 29208 United Institute of Geology, Geophysics and Mineralogy, Russian Academy of Sciences, Novosibirsk, 630090, Russia
Eugene B. Karabanov
Affiliation:
Baikal Drilling Project, Department of Geological Sciences, University of South Carolina, Columbia, South Carolina, 29208 Institute of Geochemistry, Russian Academy of Sciences, Irkutsk, 664033, Russia
Douglas F. Williams
Affiliation:
Baikal Drilling Project, Department of Geological Sciences, University of South Carolina, Columbia, South Carolina, 29208
Galina K. Khursevich
Affiliation:
Institute of Geological Sciences, National Academy of Sciences of Belarus, Minsk, 220141 Baikal Drilling Project, Department of Geological Sciences, University of South Carolina, Columbia, South Carolina, 29208, USA
*
1To whom correspondence should be addressed. E-mail: sasha@geol.sc.edu.
Get access Rights & Permissions [Opens in a new window]

Abstract

Paleoproductivity records from Lake Baikal indicate that the last interglaciation in southeastern Siberia lasted ca. 12,000 yr from 127,000 to 115,000 yr B.P., was punctuated by a climatic oscillation about 120,000 yr ago, and ended abruptly with a rapid onset of regional glaciation during marine isotope substage (MIS) 5d. The Siberian equivalent of the MIS 5e–5d transition appears to lead the post-Eemian cold pulses in Europe and in the central North Atlantic by 5000 to 8000 yr. The Baikal record also registers a pronounced cold event during early MIS 5c, which correlates with the Montaigu event in pollen records from France. In Siberia, the climatic deterioration during the MIS 5d was a full-scale glacial pulse unlike the short, moderate cooling during the Montaigu event.

Keywords

Lake Baikaldiatomsbiogenic silicaEemianclimate changeSiberia
Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 1 , July 2002 , pp. 56 - 59
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

Arkhipov, S.A., and Volkova, V.S. Geological history, Pleistocene landscapes and climate in West Sibera. (1994). SB RAS, UIGGM, Novosibirsk.Google Scholar
Arkhipov, S.A., Isaeva, L.L., Bespaly, V.G., and Glushkova, O.Y. Glaciation of Siberia and north-east USSR. Quaternary Science Reviews 5, (1986). 463 474.CrossRefGoogle Scholar
EOS American Geophyiscal Union, Transactions 78, (1997). 597 604.Google Scholar
Russian Geology and Geophysics 41, (2000). 3 32.Google Scholar
Karabanov, E.B., Prokopenko, A.A., Williams, D.F., and Colman, S.M. Evidence from Lake Baikal for Siberian glaciation during Oxygen-Isotope Substage 5d. Quaternary Research 50, (1998). 46 55.CrossRefGoogle Scholar
Karabanov, E.B., Prokopenko, A.A., Williams, D.F., and Khursevich, G.K. Evidence for mid-Eemian cooling in continental climatic record from Lake Baikal. Journal of Paleolimnology 23, (2000). 365 371.CrossRefGoogle Scholar
Kukla, G. The last interglacial. Science 287, (2000). 987 988.CrossRefGoogle Scholar
Mangerud, J., Astakhov, V.I., Murray, A., and Svendsen, J.I. The chronology of a large ice-dammed lake and the Barents–Kara Ice Sheet advances, Northern Russia. Global and Planetary Change 31, (2001). 321 336.CrossRefGoogle Scholar
McManus, J.F., Bond, G.C., Broecker, W.S., Johnsen, S., Laberie, L., and Higgins, S. High-resolution climate records from the North Atlantic during the last interglacial. Nature 371, (1994). 326 329.CrossRefGoogle Scholar
Mortlock, R.A., and Froelich, P.N. A simple method for the rapid determination of biogenic opal in pelagic marine sediments. Deep-Sea Research 36, (1989). 1415 1426.CrossRefGoogle Scholar
Prokopenko, A.A., Karabanov, E.B., Williams, D.F., Kuzmin, M.I., Shackleton, N.J., Crowhurst, S.J., Peck, J.A., Gvozdkov, A.N., and King, J.W. Biogenic silica record of the Lake Baikal response to climatic forcing during the Brunhes chron. Quaternary Research 55, (2001). 123 132.CrossRefGoogle Scholar
Reille, M., Guiot, J., and Beaulieu, J.-L. The Montaigu Event: An abrupt climatic change during the early Wurm in Europe. Kukla, G.J., and Went, E. Start of a Glacial. NATO ASI Series (1992). Springer-Verlag, Berlin. 85 95.Google Scholar
Ruddiman, W.F., and McIntyre, A. Warmth of the subpolar North Atlantic Ocean during northern hemisphere ice-sheet growth. Science 204, (1979). 173 175.CrossRefGoogle ScholarPubMed
Shackleton, N.J., Berger, A., and Peltier, W.R. An alternative astronomical calibration of the lower Pelistocene timescale based on ODP site 677. Trans. R. Soc. Edinburg Earth Sciences 81, (1990). 251 261.CrossRefGoogle Scholar
Velichko, A. A. (1984). Late Pleistocene spatial paleoclimatic reconstructions. in Late Quaternary Environments of Soviet Union Velichko, A. A., Ed., pp. 261–285. Univ. of Minnesota Press, Minneapolis.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.CrossRefGoogle Scholar