Hostname: page-component-745bb68f8f-hvd4g Total loading time: 0 Render date: 2025-01-26T06:40:03.815Z Has data issue: false hasContentIssue false
  • English
  • Français

Statistical Analysis of Grain Size Distribution in Pleistocene Sediments from Lake Biwa, Japan

Published online by Cambridge University Press:  20 January 2017

Kenji Kashiwaya ,
Atsuyuki Yamamoto  and
Kaoru Fukuyama
Kenji Kashiwaya
Affiliation:
The Graduate School of Science and Technology, Kobe University, Kobe 657, Japan
Atsuyuki Yamamoto
Affiliation:
Faculty of Engineering, Osaka Electro-Communication University, Neyagawa, Osaka 572, Japan
Kaoru Fukuyama
Affiliation:
Department of Earth Sciences, Mie University, Tsu, Mie 514, Japan
Get access Rights & Permissions [Opens in a new window]

Abstract

Time series of grain-size distributions from Pleistocene sediments deposited in Lake Biwa during the past 550 millennia show dominant periods of 40,000 and 20,000 yr that are very close to those predicted by the Milankovitch theory, as well as a period of about 70,000 yr not directly predicted by this theory. The 70,000-yr period is strongest, followed by the 20,000-yr period. The sequences also show that coarser particles were deposited, in general, during strong solar insolation, whereas finer particles were deposited during weak insolation.

Type
Research Article
Information
Quaternary Research , Volume 30 , Issue 1 , July 1988 , pp. 12 - 18
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

Berger, A., (1978). Long term variations of caloric insolation resulting from the Earth's orbital elements. Quaternary Research. 9, 139-167.Google Scholar
Berger, A., Imbrie, J., Kukla, G., Saltzman, B., (1984). Milankovitch and Climate: Understanding the Response to Astronomical Forcing. Reidel, Dordrecht.Google Scholar
Boyd, R.F., Clark, D.L., Jones, G., Ruddiman, W.F., McIntyre, A., Pisias, N.G., (1984). Central Arctic Ocean response to Pleistocene earth-orbital variations. Quaternary Research. 22, 121-128.Google Scholar
Burg, J.P., (1967). Maximum Entropy Spectral Analysis. Paper presented at the 37th Meeting Soc. of Explor, Geophys., Oklahoma, Oct. 1967.Google Scholar
Hayashi, Y., (1981). Space-time cross spectral analysis using the maximum entropy method. Journal of the Meterological Society of Japan. 59, 620-624.Google Scholar
Hays, J.D., Imbrie, J., Shackleton, N.J., (1976). Variations in the Earth's orbit: Pacemaker of the Ice Ages. Science. 194, 1121-1132.Google Scholar
Imbrie, J., Hays, J.D., Martinson, D.G., McIntyre, A., Mix, A.C., Morley, J.J., Pisias, N.G., Prell, W.L., Shackleton, N.J., The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ18O record. Berger, A.L., (1984). Milankovitch and Climate: Understanding the Response to Astronomical Forcing. Reidel, Dordrecht, 269-305.Google Scholar
Inman, D.L., (1952). Measures for describing the size distribution of sediments. Journal of Sedimentary Petrology. 22, 125-145.Google Scholar
Janecek, T.R., Rea, D.K., Pleistocene fluctuations in Northern Hemisphere tradewinds and westerlies. Berger, A.L., (1984). Milankovitch and Climate: Understanding the Response to Astronomical Forcing. Reidel, Dordrecht, 331-347.Google Scholar
Kanari, S., Fuji, N., Horie, S., The paleoclimatological constituents of paleotemperature in Lake Biwa. Berger, A.L., (1984). Milankovitch and Climate: Understanding the Response to Astronomical Forcing. Reidel, Dordrecht, 405-414.Google Scholar
Kashiwaya, K., (1986). A mathematical model of the erosional process of a mountain. Transactions, Japanese Geomorphological Union. 7, 69-77.Google Scholar
Kashiwaya, K., (1987). Theoretical investigation of the time variation of drainage density. Earth Surface Processes and Landforms. 12, 39-46.Google Scholar
Kashiwaya, K., Yamamoto, A., Fukuyama, K., (1987). Time variations of erosional force and grain size in Pleistocene lake sediments. Quaternary Research. 28, 61-68.Google Scholar
Milankovitch, M., (1930). Mathematische Klimalehre und Astronomische Theorie der Klimaschwankungen. Gebruder Borntraeger, Berlin.Google Scholar
Pisias, N.G., Leinen, M., Milankovitch forcing of the oceanic system: Evidence from the northwest Pacific. Berger, A.L., (1984). Milankovitch and Climate: Understanding the Response to Astronomical Forcing. Reidel, Dodrecht, 307-330.Google Scholar
Yamamoto, A., (1976). Paleoprecipitational change estimated from the grain size variations in the 200 m-long core from Lake Biwa. Paleolimnology of Lake Biwa and the Japanese Pleistocene. 4, 179-203.Google Scholar
Yamamoto, A., Grain size variation. Horie, S., (1984). Lake Biwa. Junk, Dordrecht, 439-459.Google Scholar
Yamamoto, A., Kanari, S., Fukuo, Y., Horie, S., (1974). Consolidation and dating of sediments in the core sample from Lake Biwa. Paleolimnology of Lake Biwa and the Japanese Pleistocene. 2, 135-144.Google Scholar
Yamamoto, A., Kashiwaya, K., Fukuyama, K., (1984). Periodic variations of grain size in the 200 meter core sample from Lake Biwa. Transactions, Japanese Geomorphological Union. 5, 345-352, [In Japanese with English abstract and illustrations].Google Scholar
Yamamoto, A., Kashiwaya, K., Fukuyama, K., (1985). Periodic variations of grain size in Pleistocene sediments in Lake Biwa and earth-orbital cycles. Geophysical Research Letters. 12, 585-588.Google Scholar
Wigley, T.M., (1976). Spectral analysis and the astronomical theory of climate change. Nature. 264, 629-631, (London).Google Scholar