Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-23T19:25:01.708Z Has data issue: false hasContentIssue false
  • English
  • Français

Lake-level changes during the past 100,000 years at Lake Baikal, southern Siberia

Published online by Cambridge University Press:  20 January 2017

Atsushi Urabe ,
Masaaki Tateishi ,
Yoshio Inouchi ,
Hirokazu Matsuoka ,
Takahiko Inoue ,
Alexsander Dmytriev  and
Oleg M. Khlystov
Atsushi Urabe*
Affiliation:
Research Institute for Hazards in Snowy Areas, Niigata University, Niigata 950-2181, Japan
Masaaki Tateishi
Affiliation:
Faculty of Science, Niigata University, Niigata 950-2181, Japan
Yoshio Inouchi
Affiliation:
Center for Marine Environmental Studies, Ehime University, Matsuyama 790-8577, Japan
Hirokazu Matsuoka
Affiliation:
Kowa Consulting Office, Tokyo 202-0022, Japan
Takahiko Inoue
Affiliation:
Graduate School of Science and Engineering, Ehime University, Matsuyama 790-8577, Japan
Alexsander Dmytriev
Affiliation:
Faculty of Geology, Geological Data Processing and Geological Ecology, State Technical University, Irkutsk 664074, Russia
Oleg M. Khlystov
Affiliation:
Limnological Institute, Siberian Branch of Russian Academy of Science, Irkutsk 664033, Russia
*
*Corresponding author. Research Institute for Hazards in Snowy Areas, Niigata University, 8050 Ikarashi 2-cho Niigata 950-2181, Japan. Fax: +81 25 261 1699. E-mail address:[email protected](A. Urabe).
Get access Rights & Permissions [Opens in a new window]

Abstract

Lake-level changes inferred from seismic surveying and core sampling of the floor of Lake Baikal near the Selenga River delta can be used to constrain regional climatic history and appear to be correlated to global climate changes represented by marine oxygen isotope stages (MIS). The reflection pattern and correlation to the isotope stages indicate that the topset and progradational foreset sediments of the deltas formed during periods of stable lake levels and warm climatic conditions. During warm stages, the lake level was high, and during cold stages it was low. The drop in the lake level due to cooling from MIS 5 through MIS 4 is estimated to be 33–38 m; from MIS 3 through MIS 2, it fell an additional 11–15 m. Because the lake level is chiefly controlled by evaporation and river input, we infer that more water was supplied to Lake Baikal during warm stages.

Keywords

Seismic surveySelenga DeltaMarine oxygen isotope stageLake-level changeLake Baikal
Type
Short Paper
Information
Quaternary Research , Volume 62 , Issue 2 , September 2004 , pp. 214 - 222
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

Afanasyev, A.N., (1960). The water budget of Lake Baikal: transactions of the Baikal Limnological Station. Academic Nark SSSR Vista, Siberia 18, 115–241.Google Scholar
Colman, S.M., (1998). Water-level changes in Lake Baikal, Siberia: tectonism versus climate. Geology 26, 531–534.2.3.CO;2>CrossRefGoogle Scholar
Colman, S.M., Peck, J.A., Karabanov, E.B., Carter, S.J., Bradbury, J.P., King, J.W., Williams, D.F., (1995). Continental climate response to orbital forcing from biogenic silica records in Lake Baikal, Siberia. Nature 378, 769–771.Google Scholar
Colman, S.M., Jones, G.A., Rubin, M., King, J.W., Peck, J.A., Orem, W.H., (1996). AMS radiocarbon analyses from Lake Baikal, Siberia: challenges of dating sediments from a large, oligotrophic lake. Quaternary Science Reviews 15, 669–684.Google Scholar
Colman, S.M., Peck, J.A., Hatton, J., Karabanov, E.B., King, J.W., (1999). Biogenic silica records from the BDP93 drill site and adjacent areas of the Selenga Delta, Lake Baikal, Siberia. Journal of Paleolimnology 21, 9–17.Google Scholar
Colman, S.M., Karabanov, E.B., Nelson, C.H., (2003). Quaternary sedimentation and subsidence history of Lake Baikal, Siberia, based on seismic stratigraphy and coring. Journal of Sedimentary Geology 73, 941–956.Google Scholar
Grachev, M.A., Likhoshway, Ye.V., Vorobyova, S.S., Khlystov, O.M., Bezrukova, E.V., Veinberg, E.V., Goldberg, E.L., Granina, L.Z., Koenakova, E.G., Lazo, F.I., Levina, O.V., Letunova, P.P., Otinov, P.V., Pirog, V.V., Fedotov, A.P., Yaskevich, S.A., Bobrov, V.A., Sukhorukov, F.V., Rezchikov, V.I., Fedorin, M.A., Zolotaryov, K.V., Kravchinsky, V.A., (1997). Signal of the paleoclimates of Upper Pleistocene in the sediments of Lake Baikal. Russian Geology and Geophysics 38, 957–980.Google Scholar
Grachev, M.A., Vorobyova, S.S., Likhoshway, Y.V., Goldberg, E.L., Ziborova, G.A., Levina, O.V., Khlystov, O.M., (1998). A high-resolution diatom record of the paleoclimates of east Siberia for the last 2.5 My from Lake Baikal. Quaternary Science Reviews 17, 1101–1106.CrossRefGoogle Scholar
Guiot, J., de Beaulieu, J.L., Pons, A., Reille, M., (1989). A 140,000-year continental climate reconstruction from two European pollen records. Nature 338, 309–313.Google Scholar
Harrison, S.P., (1989). Lake-levels and climatic changes in eastern North America. Climate Dynamics 3, 157–167.Google Scholar
Harrison, S.P., (1993). Late Quaternary lake-level changes and climates of Australia. Quaternary Science Reviews 12, 211–231.Google Scholar
Harrison, S.P., Digerfeldt, G., (1993). European lakes as palaeohydrological and palaeoclimatic indicators. Quaternary Science Reviews 12, 233–248.Google Scholar
Harrison, S.P., Tarasov, P.E., (1996). Late Quaternary lake-level records from northern Eurasia. Quaternary Research 45, 138–159.CrossRefGoogle Scholar
Khursevich, G.K., Karabanov, E.B., Prokopenko, A.A., Williams, D.F., Kuzmin, M.I., Fedenya, S.A., Gvozdkov, A.A., (2001). Insolation regime in Siberia as a major factor controlling diatom production in Lake Baikal during the past 800,000 years. Quaternary International 80–81, 47–58.CrossRefGoogle Scholar
Kutzubach, J.E., Street-Perrott, A.F., (1985). Milankovitch forcing of fluctuations in the level of tropical lake from 18 to 0 kyr B.P.. Nature 317, 130–134.Google Scholar
Mats, V.D., (1993). The structure and development of the Baikal rift depression. Earth Science Review 34, 81–118.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C., Shackleton, N.J., (1987). Age dating and the orbital theory of the ice ages–development of a high-resolution 0 to 300000-year. Quaternary chronostratigraphy Research 27, 1–29.Google Scholar
Mats, V.D., Fujii, S., Mashiko, K., Osipov, E.Yu., Yefrimova, I.M., Klimansky, A.V., (2000). Change in Lake Baikal water levels and runoff direction in the Quaternary Period. Minoura, K., Lake Baikal Elsevier, Amsterdam., 15–34.Google Scholar
Oda, T., Minoura, K., Fujimura, C., Nakamura, T., Kawai, T., (2000). Vegetation history of the Baikal drainage basin during the last 250,000 years. Japanese Journal of Palynology 46, 81–92.Google Scholar
Peteet, D.M., (1995). Global younger dryas?. Quaternary International 28, 93–104.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.A., King, J.W., (2001a). Biogenic silica record of the Lake Baikal response to climatic forcing during the Brunhes. Quaternary Research 55, 123–132.CrossRefGoogle Scholar
Prokopenko, A.A., Karabanov, E.B., Williams, D.F., Kuzmin, M.I., Khursevich, G.K., Gvozdkov, A.A., (2001b). The detailed record of climatic events during the past 75,000 yrs BP from the Lake Baikal drill core BDP-93-2. Quaternary International 80–81, 59–68.CrossRefGoogle Scholar
Shimaraev, M.N., Verbolov, V.I., Granin, N., Sherstayankin, P.P., (1994). Physical limnology of Lake Baikal: a review.. BICER reprint, 2, Irkutsk, 80 pp.Google Scholar
Street, F.A., Grove, A.T., (1979). Global maps of lake-level fluctuations since 30,000 yr BP. Quaternary Research 12, 83–118.Google Scholar
Street-Perrott, F.A., Harrison, S.P., (1985). Lake levels and climate reconstruction. Hecht, A.D., Paleoclimate Analysis and Modeling Wiley, New York., 291–340.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, G., van der Plicht, J., Spurk, M., (1998). INTCAL98 radiocarbon age calibration, 24,000-0 cal BP. Radiocarbon 40, 1041–1083.Google Scholar
Williams, D.F., Peck, J.A., Karabanov, E.B., Prokopenko, A.A., Kravchinsky, V., King, J., Kuzmin, M.I., (1997). Lake Baikal record of continental climate response to orbital insolation during the past 5 million years. Science 278, 1114–1117.Google Scholar