Hostname: page-component-cd9895bd7-gxg78 Total loading time: 0 Render date: 2024-12-23T09:15:46.708Z Has data issue: false hasContentIssue false
  • English
  • Français

Periodic Variations in Late Pleistocene Speleothem Abundance in Britain

Published online by Cambridge University Press:  20 January 2017

Kenji Kashiwaya ,
Timothy C. Atkinson  and
Peter L. Smart
Kenji Kashiwaya
Affiliation:
The Graduate School of Science and Technology, Kobe University, Kobe 657, Japan
Timothy C. Atkinson
Affiliation:
School of Environmental Sciences, University of East Anglia, Norwich NR4 7JT, England
Peter L. Smart
Affiliation:
Department of Geography, University of Bristol, Bristol BS8 1SS, England
Get access Rights & Permissions [Opens in a new window]

Abstract

Temporal change in the growth of speleothems in the United Kingdom during the past 150,000 years is shown to be related to the insolation variation by the Milankovitch theory. The speleothem data compiled by Gordon et al. (1989. Quarternary Research 31, 14–26) have two Milanokovitch frequencies: the ca. 40,000-yr period related to change in the earth's obliquity and the ca. 20,000-yr period related to the precession of the equinoxes. The abundance of speleothem growth was, in general, large during the last interglaciation and small during the last glaciation. In both periods, however, speleothem abundance was greater during periods of strong insolation and less during weak insolation.

Type
Research Article
Information
Quaternary Research , Volume 35 , Issue 2 , March 1991 , pp. 190 - 196
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

Atkinson, T.C. Growth mechanism of speleothems in Castleguard Cave, Columbia Icefields, Alberta, Canada Arctic and Alpine Research 15 1983 523 536 Google Scholar
Atkinson, T.C. Harmon, R.S. Smart, P.L. Waltham, A.C. Paleoclimatic and geomorphic implications of 230Th/234U dates on speleothems from Britain Nature (London) 272 1978 24 28 Google Scholar
Atkinson, T.C. Lawson, T.J. Smart, P.L. Harmon, R.S. 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
Barnola, J.M. Raynaud, D. Korotkevich, Lorius, C. Vostok ice core provides 160,000-year record of atmospheric CO2 Nature (London) 329 1987 408 414 Google Scholar
Barrodale, I. Ericksson, R.E. Algorithm for least-square linear prediction and maximum entropy spectral analysis—Part 1. Theory Geophysics 45 1980 420 432 Google Scholar
Berger, A. Long term variations of caloric insolation resulting from the Earth's orbital elements Quaternary Research 9 1978 139 167 Google Scholar
Drake, J.J. Theory and model for global carbonate solution by ground water Lafleur, R.G. Groundwater as a Geomorphic Agent 1984 Allen & Unwin London 210 260 Google Scholar
Ford, D.C. Williams, P.W. Karst Ecology and Hydrology 1989 Unwin Hyman London Google Scholar
Gordon, D. Smart, P.L. Comments on “Speleothem, Travertines, and Paleoclimates” by G. J. Hennig, R. Grun, and K. Brunnacker Quaternary Research 22 1984 144 147 CrossRefGoogle Scholar
Gordon, D. Smart, P.L. Ford, D.C. Andrews, J.N. Atkinson, T.C. Rowe, P.J. 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 Google Scholar
Hennig, G.J. Grun, R. Brunnacker, K. Speleothem, travertines, and paleoclimates Quaternary Research 20 1983 1 29 Google Scholar
Hsu, H.P. Fourier Analysis 1970 Simon & Schuster New York Google Scholar
Jouzel, J. Lorius, C. Petit, J.R. Genthon, C. Barkov, N.I. Kotlyakov, V.M. Petrov, V.M. Vostok ice core: A continuous isotope temperature record over the last climatic cycle (160,000 years) Nature (London) 329 1987 403 408 Google Scholar
Kashiwaya, K. Fukuyama, K. Yamamoto, A. Erosional environment and grain size variation in Pleistocene late sediments L'anthropology 90 1990 (in press) Google Scholar
Kashiwaya, K. Yamamoto, A. Fukuyama, K. Time variations of erosional force and grain size in Pleistocene late sediments Quaternary Research 28 1987 61 68 Google Scholar
Kashiwaya, K. Yamamoto, A. Fukuyama, K. Statistical analysis of grain size distribution in Pleistocene sediments from Lake Biwa, Japan Quaternary Research 30 1988 61 68 Google Scholar
Martinson, D.G. Pisias, N.G. Hays, J.D. Imbrie, J. Moore, T.C. Jr. Shackleton, N.J. Age dating and orbital theory of the ice ages; Development of a high-resolution 0 to 300,000-year chronostratigraphy Quaternary Research 27 1987 1 29 Google Scholar
Milankovitch, M. Kanon der Erdbestrahlung und seine Andwendung auf das Eiszeitenproblem 1941 Königlich Serbische Akademie Bergrad (Translated by the Israel Program for scientific translations, Jerusalem, 1969) Google Scholar
Ormsby, J.F.A. Design of numerical filters with applications to missile data processing Journal of Association of Computer Mechanics 8 1961 440 466 Google Scholar
Prenter, P.M. Splines and Variational Methods 1975 Wiley Chichester Google Scholar
Yamamoto, A. Kashiwaya, K. Fukuyama, K. Periodic variations of grain size in the 200 meter core sample from Lake Biwa Transactions, Japanese Geomorphological Union 5 1984 345 352 [In Japanese with English abstract and illustrations] Google Scholar
Yamamoto, A. Kashiwaya, K. Fukuyama, K. Periodic variations of grain size in Pleistocene sediments in Lake Biwa and earth-orbital cycles Geophysical Research Letters 12 1985 585 588 CrossRefGoogle Scholar