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Correlation and interpretation of paleosols and loess across European Russia and Asia over the last interglacial–glacial cycle

Published online by Cambridge University Press:  20 January 2017

Nathaniel W. Rutter ,
Dean Rokosh ,
Michael E. Evans ,
Edward C. Little ,
Jiri Chlachula  and
Andrei Velichko
Nathaniel W. Rutter*
Affiliation:
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada T6G 2E3
Dean Rokosh
Affiliation:
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada T6G 2E3
Michael E. Evans
Affiliation:
Institute for Geophysical Research, University of Alberta, Edmonton, Alberta, Canada T6E 2G1
Edward C. Little
Affiliation:
Canada-Nunavut Geoscience Office, Box 2319, Iqaluit, Nunavut, Canada X0A 0H0
Jiri Chlachula
Affiliation:
University of Zlin, Palaeoecology Laboratory, Zlin 76272, Czech Republic
Andrei Velichko
Affiliation:
Institute of Geography RAS, Laboratory of Evolutionary Geography, Staromonetny Lane 29, Moscow 109017, Russia
*
*Corresponding author. E-mail address:nat.rutter@ualberta.ca (N.W. Rutter).
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Abstract

Loess-paleosol sequences of the last interglacial-glacial cycle are correlated from European Russia to central Siberia and the Chinese Loess Plateau. During cold periods represented by marine oxygen isotope stages (OIS) 2 and 4, loess deposition dominated in the Russian Plain and the Loess Plateau. In central Siberia, loess deposition took place also, but five to seven thin, weakly developed paleosols are identified in both stages. OIS 3, in the Chinese Loess Plateau near Yangchang, consists of a loess bed that is flanked by two weakly developed paleosols. At Kurtak, Siberia, OIS 3 is represented by two distinct, stacked paleosols with no loess bed separating the paleosols. In the Russian Plain, OIS 3 consists of a single, possibly welded paleosol, representing upper and lower stage-3 climates. Brunisols and Chernozems dominate the profiles in China and Siberia, whereas Regosols, Luvisols, and Chernozems are evident in the northern and southern Russian Plain, respectively. OIS 5 is represented in China and the Russian Plain by pedo complexes in a series of welded soils, whereas in contrast, the Kurtak site consists of six paleosols with interbedded loess. The paleosols consist largely of Brunisols and Chernozems. Although the three areas examined have different climates, geographical settings, and loess source areas, they all had similar climate changes during the last interglacial-glacial cycle.

Keywords

PaleoclimateLoessPaleosolLast glacial maximumQuaternaryRussian PlainSiberiaIsotope stageChinese loess plateauStratigraphy
Type
Research Article
Information
Quaternary Research , Volume 60 , Issue 1 , July 2003 , pp. 101 - 109
Copyright
University of Washington

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References

Berger, A., and Loutre, M.F., (1991). Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 297–317.Google Scholar
Bolikhovskaya, N.S., (1995). Evolution of Loess-Soil Formation of Northern Eurasia. Moscow State Univ. Press, Moscow. [in Russian] Google Scholar
Chichagova, O.A., and Cherkinsky, A.E., (1988). Radiocarbon Studies in Geography. Institute of Geography, Academy of Sciences of the U.S.S.R, Moscow. [in Russian] Google Scholar
Chlachula, J., (1995). Pleistocene climate history of southern Siberia. Ph.D. thesis. University of Alberta, Edmonton, Alberta, Canada.Google Scholar
Chlachula, J., Rutter, N.W., and Evans, M.E., (1997). A late Quaternary loess-paleosol record at Kurtak, southern Siberia. Canadian Journal of Earth Sciences 34, 679–686.Google Scholar
Ding, Z., Sun, J., Rutter, N.W., Rokosh, D., and Liu, T., (1999). Changes in the sand content of loess deposits along a north to south transect of the Chinese Loess Plateau and the implications for desert variations. Quaternary Research 52, 56–62. doi:ques.1999.2045 Google Scholar
Ding, Z.L., Liu, T.S., Rutter, N.W., Yu, Z.W., Guo, Z.T., and Zhu, R.X., (1995). Ice-volume forcing of East Asian winter monsoon variations in the past 800,000 years. Quaternary Research 44, 149–159.Google Scholar
Drozdov, N.I., Cheka, V.P., Laukhin, S.A., Kol’tsova, V.G., Akimova, E.V., Ermolayev, A.E., Leont’ev, V.P., Vasil’ev, S.A., Yamskikh, A.E., Demidenko, G.A., Artem’ev, E.V., Vikulov, A.A., Bokarev, A.A., Foronova, I.V., Sidoras, S.D., (1991). Chronostratigraphy of palaeolithic sites of central Siberia (the Yennisey Basin) [in Russian]. in: Excursion Guide of the International Symposium on the Chronostratigraphy of the Palaeolithic of North, Central and Eastern Asia, and America, 13th INQUA Congress, China., (1991). Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia.Google Scholar
Fang, X., Li, J., and van der Voo, R., (1999). Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800,000 years B.P. related to Tibetan uplift. Earth and Planetary Science Letters 165, 129–144.CrossRefGoogle Scholar
Geiger, R., and Pohl, W., (1954). Revision of the Köppen-Geiger Klimckarte der Erde. Erdkunde 8, 58–61.Google Scholar
Grootes, P.M., Stuiver, M., White, J.W.C., Johnsen, S., and Jouzel, J., (1993). Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores. Nature 366, 522–554.Google Scholar
Little, E.C., (2002). Sedimentology and stratigraphy for Quaternary deposits of the Russian Plain. Ph.D. thesis. University of Alberta, Edmonton, Alberta, Canada.Google Scholar
Little, E.C., Lian, O.B., Velichko, A.A., Morozova, T.D., Nechaev, V.P., Dlussky, K.G., Rutter, N.W. (in press). Quaternary stratigraphy and optical dating of loess from the East European Plain (Russia). Quaternary Science Reviews Google Scholar
Liu, J., Liu, T., and Chen, T., (1998). Loess dating progress in China. Past Global Changes (PAGES) Newsletter 6, 2 Google Scholar
Liu, J., Nie, G., Chen, T., Song, C., Zhu, G., Li, K., Gao, Z., and Qiao, Y., (1995). A preliminary high resolution time scale for the last 130,000 years at Weinan loess section. Sciencia Geologica Sinica (Overseas Edition; Supplementary Issue) 1, 9–22.Google Scholar
Liu, T.S., (1985). Loess and the Environment. China Ocean Press, Beijing.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C.J., and Shackleton, N.J., (1987). Age dating and the orbital theory of the ice ages; development of a high-resolution 0 to 300,000-year chronostratigraphy. Quaternary Research 27, 1–29.Google Scholar
Morozova, T.D., (1981). Development of Soil Cover of Europe in Late Pleistocene. Nauka Press, Moscow. [in Russian] Google Scholar
Morozova, T.D., and Nechaev, V.P., (1997). The Valdai Periglacial Zone as an Area of cryogenic Soil Formation. Quaternary International 41/42, 57–58.Google Scholar
National Oceanic Atmospheric Administration (NOAA) (1991). Climates of the World. Historical Climatology Series 6-4. First published 1986, revised 1991. United States Department of Commerce, National Oceanic Atmospheric Administration, National Environmental Satellite Data and Information Service, National Climatic Data Center, Asheville, N.C.Google Scholar
Rokosh, D., Rutter, N.W., Little, E.C., Ding, Z., and Sun, J. (in press). Lithofacies and pedofacies variations during the last glacial period in the Loess Plateau, China. Quaternary Science Reviews Google Scholar
Rutter, N.W., and Ding, Z., (1993). Paleoclimates and monsoon variations interpreted from micromorphogenic features of the Baoji paleosols, China. Quaternary Science Reviews 12, 853–862.Google Scholar
Rutter, N.W., Ding, Z., Evans, M.E., and Liu, T., (1991). Baoji-type pedostratigraphic section, Loess Plateau, North-central China. Quaternary Science Reviews 10, 1–22.Google Scholar
Soil Classification Working Group The Canadian System of Soil Classification. Agriculture and Agricultural Foods, Canada. (1998). Publication 1646, Ottawa.Google Scholar
Sudakova, N.G., (1993). Glacial Lithogenesis of Russian Plain. Moscow State Univ. Publishing House, Moscow. [in Russian] Google Scholar
Sun, J., Ding, Z., and Liu, T., (1995). The environmental evolution of the desert-loess transition zone over the last glacial-interglacial cycle. Wang, S. Quaternary Geology and Past Environmental Changes in China. Science Press, Beijing. 1–8.Google Scholar
Sun, J., Yin, G., Ding, D., Liu, T., and Chen, J., (1998). Thermoluminescence chronology of sand profiles in the Mu Us Desert, China. Palaeogeography, Palaeoclimatology, Palaeoecology 144, 25–233.CrossRefGoogle Scholar
Velichko, A.A., (1990). Loess-paleosol formation on the Russian Plain. Quaternary International 7/8, 103–114.CrossRefGoogle Scholar
Velichko, A.A., Dlussky, K.G., Morozova, T.D., Nechaev, V.P., Semenov, V.V., Rutter, N.W., and Little, E.C., (2000). The Gololobovo section. Loess-soil-cryogenic formations of Moscow-Oka plain. Paleosols and modern soils as stages of continuous soil formation. Makeev, A.O., and Velichko, A.A. Abstracts and Field Excursion Guidebook V, International Symposium on Paleopedology,. Institute of Geography, Russian Academy of Sciences, Moscow. 67–87. [in Russian] Google Scholar
Velichko, A.A., Gribchenko, , Yu, N., Gubonina, Z.P., Morozova, T.D., Nechaev, V.P., Sycheva, S.A., Timireva, S.N., Udartsev, V.P., Khalcheva, T.A., Tsatskin, A.I., Chikolini, N.I., (1997). Main features of loess-soil formation. in: Loess-Soil Formation of East-European Plain. Paleogeography and Stratigraphy, Institute of Geography, Russian Academy of Sciences, Moscow., pp. 5–24. [In Russian] Google Scholar
Velichko, A.A., and Nechaev, V.P., (1984). Late Pleistocene in European USSSR. Velichko, A.A., Wright, H.E. Jr., and Barnosky, A.D. Late Quaternary Environments of the Soviet Union. Univ. of Minnesota Press, Minneapolis. 79–86.Google Scholar
Zhang, X., Chen, Z., Zhang, G., Chen, T., and Liu, H., (1996). Remote mineral aerosols in Westerlies and their contributions to the Chinese loess. Science in China (Series D) 39, 134–143.Google Scholar
Zhao, S., (1986). Physical Geography of China. Science Press, Beijing, and J Wiley, New York.Google Scholar