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Reconstruction of climate and vegetation changes of Lake Bayanchagan (Inner Mongolia): Holocene variability of the East Asian monsoon

Published online by Cambridge University Press:  20 January 2017

Wenying Jiang*
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China CEREGE UMR 6635 CNRS, BP 80, Europôle Méditerranéen de l’Arbois, 13545 Aix-en-Provence cedex 4, France
Zhengtang Guo
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xian 710075, China
Xiangjun Sun
Affiliation:
Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China
Haibin Wu
Affiliation:
SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xian 710075, China
Guoqiang Chu
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Baoyin Yuan
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Chritine Hatté
Affiliation:
Laboratoire des Sciences du Climat et de l'Environnement, UMR 1572 CEA/CNRS, F-91198 Gif sur Yvette Cedex, France
Jöel Guiot
Affiliation:
CEREGE UMR 6635 CNRS, BP 80, Europôle Méditerranéen de l’Arbois, 13545 Aix-en-Provence cedex 4, France
*
*Corresponding author. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China. Fax: +86 10 62032495. E-mail address:wjiang@mail.igcas.ac.cn (W. Jiang).

Abstract

A high-resolution pollen and Pediastrum record, spanning 12,500 yr, is presented for Lake Bayanchagan , southern Inner Mongolia. Individual pollen taxa (PT-MAT) and the PFT affinity scores (PFT-MAT) were used for quantitative climatic reconstruction from pollen and algal data. Both techniques indicate that a cold and dry climate, similar to that of today, prevailed before 10,500 cal yr B.P. The wettest climate occurred between ∼10,500 and 6500 cal yr B.P., at which time annual precipitation was up to 30–60% higher than today. The early Holocene increases in temperature and precipitation occurred simultaneously, but mid-Holocene cooling started at approximately 8000 cal yr B.P., 1500 yr earlier than the drying. Vegetation reconstruction was based on the objective assignment of pollen taxa to the plant functional type. The results suggest that this region was dominated by steppe vegetation throughout the Holocene, except for the period ∼9200 to ∼6700 cal yr B.P., when forest patches were relatively common. Inner Mongolia is situated at the limit of the present East Asian monsoon and patterns of vegetation and climate changes in that region during the Holocene probably reflect fluctuations in the monsoon's response to solar insolation variations. The early to middle Holocene monsoon undoubtedly extended to more northern latitudes than at present.

Type
Research Article
Copyright
University of Washington

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References

An, Z.S., Porter, S.C., Kutzbach, J.E., Wu, X.H., Wang, S.M., Liu, X.D., Li, X.Q., Zhou, W.J., (2000). Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews 19, 743762.CrossRefGoogle Scholar
Arnold, M., Bard, E., Maurice, P., Duplessy, J.-C., (1987). C-14 dating with the Gif-sur-Yvette Tandetron accelerator: status report. Nuclear Instruments and Methods in Physics Research B29, 635645.Google Scholar
Bennett, K.D., (2002). Psimpoll 4.10: computer programs for data plotting and analysis.. http://www.kv.geo.uu.se/psimpoll.html.Google Scholar
Berger, A., Loutre, M.F., (1991). Insolation values for the last 10 million years. Quaternary Science Reviews 10, 297317.CrossRefGoogle Scholar
Charney, J., Stone, P.H., Quirk, W.J., (1975). Drought in Sahara–Biogeophysical feedback mechanism. Science 187, 434435.CrossRefGoogle ScholarPubMed
Chen, C.A., Lan, H.C., Lou, J.Y., Chen, Y.C., (2003). The dry Holocene megathermal in inner mongolia. Palaeogeography, Palaeoclimatology, Palaeoecology 193, 181200.CrossRefGoogle Scholar
Cui, H.T., Wu, W.L., Wu, H.L., (1993). Holocene environmental reconstruction in Da Qing Shan region in Inner Mongolia. Zhang, L.S. Research on the Past Life–Supporting Environment Changes of China China Ocean Press, Beijing.285295.Google Scholar
Davis, B.A.S., Brewer, S., Stevenson, A.C., Guiot, J., (2003). The temperature of Europe during the Holocene reconstructed from pollen data. Quaternary Science Reviews 22, 17011716.Google Scholar
DeMenocal, P., Ortiz, J., Guilderson, T., Adkins, J., Sarnthein, M., Baker, L., Yarusinsky, M., (2000). Abrupt onset and termination of the African humid period: rapid climate responses to gradual insolation forcing. Quaternary Science Reviews 19, 347361.Google Scholar
Domrös, M., Peng, G., (1988). The Climate of China. Springer-Verlag, Berlin.Google Scholar
Ganopolski, A., Kubatzki, C., Claussen, M., Brovkin, V., Petoukhov, V., (1998). The influence of vegetation–atmosphere–ocean interaction on climate during the mid-Holocene. Science 280, 19161919.CrossRefGoogle ScholarPubMed
Gasse, F., Fontes, J.Ch., Campo, E.V., Wei, K., (1996). Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4: discussion and conclusions. Palaeogeography, Palaeoclimatology, Palaeoecology 120, 7992.CrossRefGoogle Scholar
Grimm, E.C., (1987). CONISS: a FORTRAN 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computers and Geosciences 13, 1335.CrossRefGoogle Scholar
Guiot, J., (1987). Late Quaternary climatic changes in France estimated from multivariate pollen time series. Quaternary Research 28, 100118.Google Scholar
Guiot, J., (1990). Methodology of the last climatic cycle reconstruction from pollen data. Palaeogeography, Palaeoclimatology, Palaeoecology 80, 4969.Google Scholar
Guiot, J., Goeury, C., (1996). PPPBASE, a software for statistical analysis of paleoecological and paleoclimatological data. Dendrochronologia 14, 295300.Google Scholar
Guiot, J., de Beaulieu, J.L., Cheddadi, R., David, F., Ponel, P., Reille, M., (1993a). The climate in Western Europe during the last Glacial/Interglacial cycle derived from pollen and insect remains. Palaeogeography, Palaeoclimatolology, Palaeoecology 103, 7394.CrossRefGoogle Scholar
Guiot, J., Harrison, S.P., Prentice, T.C., (1993b). Reconstruction of Holocene patterns of moisture in Europe using pollen and lake-level data. Quaternary Research 40, 139149.CrossRefGoogle Scholar
Herzschuh, U., Tarasov, P., Wünnemann, B., Hartmann, K., (2004). Holocene vegetation and climate of the Alashan Plateau, NW China, reconstructed from pollen data. Palaeogeography, Palaeoclimatology, Palaeoecology 211, 117.CrossRefGoogle Scholar
Kutzbach, J.E., (1981). Monsoon climate of the Early Holocene: climate experiment with the earth's orbital parameters for 9000 years ago. Science 214, 5961.Google Scholar
Kutzbach, J.E., Liu, Z., (1997). Response of the African monsoon to orbital forcing and ocean feedbacks in the middle Holocene. Science 278, 440443.CrossRefGoogle Scholar
Kutzbach, J.E., Bonan, G., Foley, J., Harrison, S.P., (1996). Vegetation and soil feedbacks on the response of the African monsoon to orbital forcing in the early to middle Holocene. Nature 384, 623626.Google Scholar
Liu, T.S., Ding, Z.L., (1998). Chinese loess and the paleomonsoon. Annual Review of Earth and Planetary Sciences 26, 111145.Google Scholar
Liu, K.B., Yao, Z., Thompson, L.G., (1998). A pollen record of Holocene climatic changes from the Dunde ice cap, Qinghai-Tibetan Plateau. Geology 26, 135138.Google Scholar
Liu, H.Y., Xu, L.H., Cui, H.T., (2002). Holocene history of desertification along the woodland-steppe border in northern China. Quaternary Research 57, 259270.Google Scholar
Magny, M., Guiot, J., Schoellammer, P., (2001). Quantitative reconstruction of Younger Dryas to Mid-Holocene paleoclimates at Le Locle, Swiss Jura, using pollen and lake-level data. Quaternary Research 56, 170180.Google Scholar
Members of China Quaternary Pollen Data Base(2001). Simulation of China biome reconstruction based on pollen data from surface sediment samples. Acta Botanica Sinica 43, 201209.Google Scholar
Moore, P.D., Webb, J.A., Collinson, M.E., (1991). Pollen Analysis. 2nd ed. Blackwell Science, London.Google Scholar
Nakagawa, T., Tarasov, P.E., Nishida, K., Gotanda, K., Yasuda, Y., (2002). Quantitative pollen-based climate reconstruction in central Japan: application to surface and Late Quaternary spectra. Quaternary Science Reviews 21, 20992113.Google Scholar
Olsson, I.U., (1986). Radiometric dating. Berglund, B.E. Handbook of Holocene Palaeoecology and Palaeohydrology John Wiley and Sons, Chichester.273312.Google Scholar
Prentice, I.C., Guiot, J., Huntley, B., Jolly, D., Cheddadi, R., (1996). Reconstructing biomes from palaeoecological data: a general method and its application to European pollen data at 0 and 6 ka. Climate Dynamics 12, 185194.CrossRefGoogle Scholar
Ritchie, J.C., Haynes, C.V., (1987). Holocene vegetation zonation in the eastern Sahara. Nature 330, 645647.Google Scholar
Song, C.Q., Wang, F.Y., Sun, X.J., (1996). Implication of paleovegetational changes in Diaojiao Lake, Inner Mongolia. Acta Botanica Sinica 38, 568575.Google Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C data base and revised 3.0 14C age calibration program. Radiocarbon 35, 215230.Google Scholar
Tarasov, P.E., Webb, T. III, Andreev, A.A., Afanas'eva, N.B., Berezina, N.A., Bezusko, L.G., Blyakharchuk, T.A., Bolikhovskaya, N.S., Cheddadi, R., Chernavskaya, M.M., Chernova, G.M., Dorofeyuk, N.I., Dirksen, V.G., Elina, G.A., Filimonova, L.V., Glebov, F.Z., Guiot, J., Gunova, V.S., Harrison, S.P., Jolly, D., Khomutova, V.I., Kvavadze, E.V., Osipova, I.M., Panova, N.K., Prentice, I.C., Saarse, L., (1998). Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia. Journal of Biogeography 25, 10291053.Google Scholar
Tarasov, P.E., Guiot, J., Cheddadi, R., Andreev, A.A., Bezusko, L.G., Blyakharchuk, T.A., Dorofeyuk, N.I., Filimonova, L.V., Volkova, V.S., Zernitskaya, V.P., (1999). Climate in northern Eurasia 6000 years ago reconstructed from pollen data. Earth and Planetary Science Letters 171, 635645.Google Scholar
Tarasov, P., Dorofeyuk, N., Metel'tseva, E., (2000). Holocene vegetation and climate changes in Hoton-Nur basin, northwest Mongolia. Boreas 29, 117126.Google Scholar
Tao, S.Y., Chen, L.X., (1987). A review of recent research on the East Asian Summer Monsoon. Chang, C.P., Krishnamurti, T.N. Monsoon Meteorology Oxford Univ. Press, Oxford.6092.Google Scholar
Wu, N.Q., Liu, T.S., Liu, X.P., Gu, Z.Y., (2002). Mollusk record of millennial climate variability in the Loess Plateau during the Last Glacial Maximum. Boreas 31, 2027.Google Scholar
Xiao, J.L., Nakamura, T., Lu, H.Y., Zhang, G.Y., (2002). Holocene climate changes over the desert/loess transition of north-central China. Earth and Planetary Science Letters 197, 1118.CrossRefGoogle Scholar
Yu, G., Chen, X., Ni, J., Cheddadi, R., Guiot, J., Han, H., Harrison, S.P., Huang, C., Ke, M., Kong, Z., Li, S., Li, W., Liew, P., Liu, G., Liu, Q., Liu, K-B., Prentice, I.C., Qui, W., Ren, G., Song, C., Sugita, S., Sun, X., Tang, L., Van Campo, E., Xia, Y., Xu, Q., (2000). Palaeovegetation of China: a pollen data-based synthesis for the mid-Holocene and last glacial maximum. Journal of Biogeography 27, 635664.CrossRefGoogle Scholar
Zhou, W.J., Head, M.J., Deng, L., (2001). Climate changes in northern China since the late Pleistocene and its response to global change. Quaternary International 83–85, 285292.CrossRefGoogle Scholar