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Evidence from Uranium-Series-Dated Speleothems for the Timing of the Penultimate Deglaciation of Northwestern Europe

Published online by Cambridge University Press:  20 January 2017

Isaac J. Winograd
Isaac J. Winograd*
Affiliation:
U.S. Geological Survey, 432 National Center, Reston, Virginia, 20192
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Abstract

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Type
Letter to the Editor
Information
Quaternary Research , Volume 58 , Issue 1 , July 2002 , pp. 60 - 61
Copyright
University of Washington

References

Atkinson, T.C., Lawson, T.J., Smart, P.L., Harmon, R.S., and Hess, J.W. New data on speleothem deposition and paleoclimate in Britain over the last forty thousand years. Journal of Quaternary Science 1, (1986). 67 72.Google Scholar
Baker, A., Smart, P.L., and Ford, D.C. Northwest European paleoclimate as indicated by growth frequency variations of secondary calcite deposits. Paleogeography, Paleoclimatology, Paleoecology 100, (1993). 291 301.CrossRefGoogle Scholar
Baker, A., Smart, P.L., and Edwards, R.L. Paleoclimate implications of mass spectrometric dating of a British flowstone. Geology 23, (1995). 309 312.2.3.CO;2>CrossRefGoogle Scholar
Berstad, I. M., Einevoll, S., and Lauritzen, S.-E.1997. U-series dating and stable isotope analysis of some last interglacial speleothems from north Norway. inProceedings of the 12th International Congress of Speleology, Symposium 7, pp. 53–54.Google Scholar
Gallup, C.D., Cheng, H., Taylor, F.W., and Edwards, R.L. Direct determination of the timing of sea level change during Termination II. Science 295, (2002). 310 313.Google Scholar
Gascoyne, M., Currant, A.P., and Lord, T.C. Ipswichian fauna of Victoria Cave and the marine paleoclimate record. Nature 294, (1981). 652 654.Google Scholar
Gascoyne, M., Schwarcz, H.P., and Ford, D.C. Uranium-series ages of speleothem from Northwest England: Correlation with Quaternary climate. Philosophical Transactions of the Royal Society of London, series B 301, (1983). 143 164.Google Scholar
Gascoyne, M. Paleoclimate determination from cave calcite deposits. Quaternary Science Reviews 11, (1992). 609 632.Google Scholar
Gordon, D., Smart, P.L., Ford, D.C., Andrews, J.N., Atkinson, T.C., Rowe, P.J., and Christopher, N.S.J. Dating of Late Pleistocene interglacial and interstadial periods in the United Kingdom from speleothem growth frequency. Quaternary Research 31, (1989). 14 26.CrossRefGoogle Scholar
Hamelin, B., Bard, E., Zindler, A., and Fairbanks, R.G. 234U/238U mass spectrometry of corals: How accurate is the U–Th age of the last interglacial period?. Earth and Planetary Science Letters 106, (1991). 169 180.CrossRefGoogle Scholar
Henderson, G.M., and Slowey, N.C. Evidence from U–Th dating against Northern Hemisphere forcing of the penultimate deglaciation. Nature 404, (2000). 61 66.Google Scholar
Henderson, G.M., Slowey, N.C., and Fleisher, M.Q. U–Th dating of carbonate platform and slope sediments. Geochimica et Cosmochimica Acta 65, (2001). 2757 2770.Google Scholar
Karner, D.B., and Muller, R.A. A causality problem for Milankovitch. Science 288, (2000). 2143 2144.Google Scholar
Lauritzen, S.-E. Natural environmental change in karst: The Quaternary record. Catena, Supplement 25, (1993). 21 40.Google Scholar
Lauritzen, S.-E. High resolution paleotemperature proxy record for the last interglaciation based on Norwegian speleothems. Quaternary Research 43, (1995). 133 146.Google Scholar