Editorial Type:
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Article Type:
Research Article

Pollen-Based Quantitative Reconstruction of Holocene Climate Changes in the Daihai Lake Area, Inner Mongolia, China

Qinghai Xu College of Resources and Environment Science, and Hebei Key Laboratory of Environmental Change and Ecological Construction, Hebei Normal University, Shijiazhuang, and Key Laboratory of Western China’s Environmental System (Ministry of Education), Lanzhou University, Lanzhou, China

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Jule Xiao Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China

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Yuecong Li College of Resources and Environment Science, and Hebei Key Laboratory of Environmental Change and Ecological Construction, Hebei Normal University, Shijiazhuang, China

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Fang Tian College of Resources and Environment Science, and Hebei Key Laboratory of Environmental Change and Ecological Construction, Hebei Normal University, Shijiazhuang, China

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Takeshi Nakagawa Department of Geography, University of Newcastle, Newcastle upon Tyne, United Kingdom

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Print Publication:
01 Jun 2010
DOI:
https://doi.org/10.1175/2009JCLI3155.1
Page(s):
2856–2868
Restricted access

Abstract

Vegetation around the Daihai Lake, northern China, is very sensitive to climate changes. In this paper, pollen-based quantitative climate reconstructions using three methods [weighted averaging partial least squares method (WAPLS), modern analog technique (MAT), and pollen response surface method (PRS)] were conducted to obtain robust reconstructions of Holocene climate changes in the Daihai Lake area. The result obtained by the three methods all consistently show the annual precipitation to have been 50–100 mm lower in the early Holocene, 100–200 mm higher in the Mid-Holocene, and 50–100 mm lower again in the late Holocene than at present. The WAPLS and the MAT methods also show quasi-synchronous oscillations of the mean annual temperature (Ta); 1°–2°C lower in the Early Holocene and 1°–3°C higher in the Mid-Holocene than today. The time period from 6200 to 5100 cal yr BP was the wettest and the warmest interval, with an annual precipitation (Pa) greater than 550 mm and mean annual temperature Ta higher than 6.5°C. Several cold and dry events can be identified to occur about 8200, 6000, and 4400 cal yr BP, with an annual precipitation less than 400 mm and a mean annual temperature colder than 4.5°C, respectively. The mean temperature of the warmest month (Tw) as reconstructed using both WAPLS and MAT methods was relatively stable during the Holocene, fluctuating about ±2°C relative to the present level, but the PRS method suggests more varied Tw values in both amplitude and frequency. After 1500 cal yr BP, no consistent pattern can be observed from these three different analyses, probably because of the impact of intensified human disturbances on the natural vegetation. The fluctuations of annual precipitation (Pa) correspond to that observed in Dongge Cave in southern China. The differences might be linked to Indian monsoon and East Asia monsoon climates or caused by the different degree of dating precision, different temporal resolution, and different sensitive response of climate proxies to the climate variations.

Corresponding author address: Qinghai Xu, College of Resources and Environment Science, Hebei Normal University, Shijiazhuang 050016, China. Email: xuqinghai@mail.hebtu.edu.cn

Abstract

Vegetation around the Daihai Lake, northern China, is very sensitive to climate changes. In this paper, pollen-based quantitative climate reconstructions using three methods [weighted averaging partial least squares method (WAPLS), modern analog technique (MAT), and pollen response surface method (PRS)] were conducted to obtain robust reconstructions of Holocene climate changes in the Daihai Lake area. The result obtained by the three methods all consistently show the annual precipitation to have been 50–100 mm lower in the early Holocene, 100–200 mm higher in the Mid-Holocene, and 50–100 mm lower again in the late Holocene than at present. The WAPLS and the MAT methods also show quasi-synchronous oscillations of the mean annual temperature (Ta); 1°–2°C lower in the Early Holocene and 1°–3°C higher in the Mid-Holocene than today. The time period from 6200 to 5100 cal yr BP was the wettest and the warmest interval, with an annual precipitation (Pa) greater than 550 mm and mean annual temperature Ta higher than 6.5°C. Several cold and dry events can be identified to occur about 8200, 6000, and 4400 cal yr BP, with an annual precipitation less than 400 mm and a mean annual temperature colder than 4.5°C, respectively. The mean temperature of the warmest month (Tw) as reconstructed using both WAPLS and MAT methods was relatively stable during the Holocene, fluctuating about ±2°C relative to the present level, but the PRS method suggests more varied Tw values in both amplitude and frequency. After 1500 cal yr BP, no consistent pattern can be observed from these three different analyses, probably because of the impact of intensified human disturbances on the natural vegetation. The fluctuations of annual precipitation (Pa) correspond to that observed in Dongge Cave in southern China. The differences might be linked to Indian monsoon and East Asia monsoon climates or caused by the different degree of dating precision, different temporal resolution, and different sensitive response of climate proxies to the climate variations.

Corresponding author address: Qinghai Xu, College of Resources and Environment Science, Hebei Normal University, Shijiazhuang 050016, China. Email: xuqinghai@mail.hebtu.edu.cn

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  • Bartlein, P. J., T. Webb III, and E. Fleri, 1984: Holocene climatic change in the northern Midwest: Pollen derived estimates. Quat. Res., 22 , 361–374.

    • Search Google Scholar
    • Export Citation

  • Bartlein, P. J., I. C. Prentice, and T. Webb III, 1986: Climate response surfaces from pollen data for some eastern North American taxa. J. Biogeogr., 13 , 35–57.

    • Search Google Scholar
    • Export Citation

  • Birks, H. J. B., 1995: Quantitative paleoenvironmental reconstructions. Statistical Modeling of Quaternary Science Data, D. Maddy and J. S. Brew, Eds., Quaternary Research Association, 161–254.

    • Search Google Scholar
    • Export Citation

  • Birks, H. J. B., 1998: Numerical tools in paleolimnology—Progress, potentialities, and problems. J. Paleolimnol., 20 , 307–332.

  • Birks, H. J. B., J. M. Line, S. Juggins, A. C. Stevenson, and C. J. F. ter Braak, 1990: Diatoms and pH reconstruction. Philos. Trans. Roy. Soc. London, B327 , 263–278.

    • Search Google Scholar
    • Export Citation

  • Bond, G., and Coauthors, 2001: Persistent solar influence on North Atlantic climate during the Holocene. Science, 294 , 2130–2136.

  • Bonnefille, R., and F. Chalie, 2000: Pollen-inferred precipitation time-series from equatorial mountains, Africa, the last 40 kyr B. P. Global Planet. Change, 26 , 25–50.

    • Search Google Scholar
    • Export Citation

  • Cheddadi, R., H. F. Lamb, J. Guit, and S. van der Kaars, 1998: Holocene climatic change in Morocco: A quantitative reconstruction from pollen data. Climate Dyn., 14 , 883–890.

    • Search Google Scholar
    • Export Citation

  • Chinese Academy of Sciences (Compilatory Commission of Physical Geography of China), 1984: Physical Geography of China: Climate (in Chinese). Science Press, 161 pp.

    • Search Google Scholar
    • Export Citation

  • Conolly, A. P., 1961: Some climatic and edaphic indications from the late-glacial flora. Proc. Linn. Soc. London, 172 , 55–62.

  • Faegri, K., and J. Iversen, 1989: Textbook of Pollen Analysis. 4th ed. John Wiley, 328 pp.

  • Gao, Y. X., and S. Y. Xu, 1962: Some Issues of East Asian Monsoon (in Chinese). Science Press, 106 pp.

  • Guiot, J. P., 1990: Methodology of the last climatic cycle reconstruction in France from pollen data. Palaeogeogr. Palaeoclimatol. Palaeoecol., 80 , 49–69.

    • Search Google Scholar
    • Export Citation

  • Guiot, J. P., A. Pons, J. L. de Beaulieu, and M. Reille, 1989: A 140,000 year continental climate reconstruction from two European pollen records. Nature, 338 , 309–313.

    • Search Google Scholar
    • Export Citation

  • Hou, H. Y., 1983: Vegetation of China with reference to its geographical distribution (in Chinese). Ann. Mo. Bot. Gard., 70 , 509–549.

  • Huntley, B., and I. C. Prentice, 1988: July temperature in Europe from pollen data, 6000 years before present. Science, 241 , 687–690.

  • Imbrie, J., and N. G. Kipp, 1971: A new micropaleontological method for quantitative paleoclimatology: Application to a late Pleistocene Caribbean Core. The Late Cenozoic Glacial Ages, K. K. Turekian, Ed., Yale University Press, 71–181.

    • Search Google Scholar
    • Export Citation

  • Jackson, S. T., and J. W. Williams, 2004: Modern analogs in Quaternary paleoecology: Here today, gone yesterday, gone tomorrow? Annu. Rev. Earth Planet. Sci., 32 , 495–537.

    • Search Google Scholar
    • Export Citation

  • Jiao, B. C., 1984: Atlas of Chinese Natural Geography (in Chinese). Beijing Atlas Press, 200 pp.

  • Jin, Z. D., F. H. Li, J. J. Cao, S. M. Wang, and J. M. Yu, 2006: Geochemistry of Daihai Lake sediments, Inner Mongolia, North China: Implications for provenance, sedimentary sorting, and catchment weathering. Geomorphology, 80 , 147–163.

    • Search Google Scholar
    • Export Citation

  • Jongman, R. H. G., C. J. F. ter Braak, and O. F. R. Van Tongeren, 1995: Data Analysis in Community and Landscape Ecology. Cambridge University Press, 299 pp.

    • Search Google Scholar
    • Export Citation

  • Li, H. Z., 1979: Formation of Daihai Lake basin and characteristics of the landform evolution (in Chinese). J. Nat. Sci. Beijing Norm. Univ., 1 , 98–110.

    • Search Google Scholar
    • Export Citation

  • Li, X. Q., J. Zhou, J. Shen, C. Y. Weng, H. L. Zhao, and Q. L. Sun, 2004: Vegetation history and climatic variations during the last 14ka BP inferred from a pollen record at Daihai Lake, north-central China. Rev. Palaeobot. Palynol., 132 , 195–205.

    • Search Google Scholar
    • Export Citation

  • Li, Y. C., Q. H. Xu, J. S. Liu, X. L. Yang, and T. Nakagawa, 2007: A transfer-function model developed from an extensive surface-pollen data set in northern China and its potential for palaecoclimate reconstructions. Holocene, 17 , 897–905.

    • Search Google Scholar
    • Export Citation

  • Liu, H. Y., H. T. Cui, Y. H. Tian, and L. H. Xu, 2002: Temporal spatial variances of Holocene precipitation at the marginal area of the East Asian monsoon influences from pollen evidence (in Chinese). Acta Bot. Sin., 44 , 864–871.

    • Search Google Scholar
    • Export Citation

  • Markgraf, V., R. S. Webb, K. H. Anderson, and L. Anderson, 2002: Modern pollen/climate calibration for southern South America. Palaeogeogr. Palaeoclimatol. Palaeoecol., 181 , 375–397.

    • Search Google Scholar
    • Export Citation

  • Nakagawa, T., P. E. Tarasov, K. Nishida, K. Gotanda, and Y. Yasuda, 2002: Quantitative pollen-based climate reconstruction in central Japan: Application to surface and Late Quaternary spectra. Quat. Sci. Rev., 21 , 2099–2113.

    • Search Google Scholar
    • Export Citation

  • Overpeck, J. T., T. Webb III, and I. C. Prentice, 1985: Quantitative interpretation of fossil pollen spectra: Dissimilarity coefficients and the method of modern analogs. Quat. Res., 23 , 87–108.

    • Search Google Scholar
    • Export Citation

  • Peng, Y. J., J. L. Xiao, T. Nakamura, B. L. Liu, and Y. Inouchi, 2005: Holocene East Asian monsoonal precipitation pattern revealed by grain-size distribution of core sediments of Daihai Lake in Inner Mongolia of north-central China. Earth Planet. Sci. Lett., 233 , 467–479.

    • Search Google Scholar
    • Export Citation

  • Prentice, I. C., R. W. Parsons, and T. Webb III, 1986: Pollen percentages, tree abundances and the Fagerlind effect. J. Quat. Sci., 1 , 35–42.

    • Search Google Scholar
    • Export Citation

  • Prentice, I. C., P. J. Bartlein, and T. Webb III, 1991: Vegetation and climate change in eastern North America since the last glacier maximum. Ecology, 72 , 2038–2056.

    • Search Google Scholar
    • Export Citation

  • Seppä, H., H. J. B. Birks, A. Odland, A. Poska, and S. Veski, 2004: A modern pollen-climate calibration set from northern Europe: Developing and testing a tool for palaeoclimatological reconstructions. J. Biogeogr., 31 , 251–267.

    • Search Google Scholar
    • Export Citation

  • Shen, J., R. Matsumoto, S. M. Wang, and Y. X. Zhu, 2002: Quantitative reconstruction of the lake water paleotemperature of Daihai Lake, Inner Mongolia, China and its significance in paleoclimate (in Chinese). Sci. China Ser. D, 45 , 792–800.

    • Search Google Scholar
    • Export Citation

  • Song, C. Q., and X. J. Sun, 1997: Establishment of transfer functions of the pollen-climatic factors in northern China and the quantitative climatic reconstruction at DJ core. Acta Bot. Sin., 39 , 814–821.

    • Search Google Scholar
    • Export Citation

  • Stuiver, M., and Coauthors, 1998: INTCAL98 radiocarbon age calibration, 24000-0 cal BP. Radiocarbon, 40 , 1041–1083.

  • Sun, Q. L., J. Zhou, J. Shen, P. Chen, F. Wu, and X. P. Xie, 2006: Environmental characteristics of Mid-Holocene recorded by lacustrine sediments from Lake Daihai, north environment sensitive zone, China. Sci. China Ser. D, 49 , 968–981.

    • Search Google Scholar
    • Export Citation

  • Sun, X. J., F. Y. Wang, and C. Q. Song, 1996: Pollen-climate response surfaces of selected taxa from northern China. Sci. China Ser. D, 39 , 486–493.

    • Search Google Scholar
    • Export Citation

  • Telford, R. J., and H. J. B. Birks, 2005: The secret assumption of transfer functions: Problems with spatial autocorrelation in evaluating model performance. Quat. Sci. Rev., 24 , 2173–2179.

    • Search Google Scholar
    • Export Citation

  • ter Braak, C. J. F., 1995: Non-linear methods for multivariate statistical calibration and their use in paleoecology: A comparison of inverse and classical approaches. Chemom. Intell. Lab. Syst., 28 , 165–180.

    • Search Google Scholar
    • Export Citation

  • ter Braak, C. J. F., and S. Juggins, 1993: Weighted averaging partial least squares regression (WA-PLS): An improved method for reconstruction environmental variables from species assemblages. Hydrobiologia, 269 , 485–502.

    • Search Google Scholar
    • Export Citation

  • Wang, S. M., Y. S. Yu, R. J. Wu, and M. Feng, 1990: The Daihai Lake: Environment Evolution and Climate Change (in Chinese). University of Science and Technology of China Press, 191 pp.

    • Search Google Scholar
    • Export Citation

  • Wang, Y. J., and Coauthors, 2005: The Holocene Asian monsoon: Links to solar changes and North Atlantic climate. Science, 308 , 854–857.

    • Search Google Scholar
    • Export Citation

  • Webb, R. S., K. H. Anderson, and T. Webb III, 1993: Pollen response-surface estimates of late Quaternary changes in the moisture balance of the northeastern United States. Quat. Res., 40 , 213–227.

    • Search Google Scholar
    • Export Citation

  • Webb III, T., and R. A. Bryson, 1972: Late- and postglacical climatic change in the northern Midwest, USA: Quantitative estimates from fossil pollen spectra by multivariate statistical analysis. Quat. Res., 2 , 70–115.

    • Search Google Scholar
    • Export Citation

  • Williams, J. W., and B. Shuman, 2008: Obtaining accurate and precise environmental reconstructions from the modern analog technique and North American surface pollen dataset. Quat. Sci. Rev., 27 , 669–687.

    • Search Google Scholar
    • Export Citation

  • Wu, Z. Y., 1980: China Vegetation (in Chinese). Science Press, 1375 pp.

  • Xiao, J. L., Q. H. Xu, T. Nakamura, X. L. Yang, W. D. Liang, and Y. Inouchi, 2004: Holocene vegetation variation in the Daihai Lake region of north-central China: A direct indication of the Asian monsoon climatic history. Quat. Sci. Rev., 23 , 1669–1679.

    • Search Google Scholar
    • Export Citation

  • Xu, Q. H., J. L. Xiao, T. Nakamura, X. L. Yang, Z. J. Yang, W. D. Liang, Y. Inouchi, and X. Y. Yang, 2003: Quantitative reconstructed climatic changes of Daihai basin by pollen data (in Chinese). Mar. Geol. Quat. Geol., 23 , 99–108.

    • Search Google Scholar
    • Export Citation

  • Xu, Q. H., Y. C. Li, X. L. Yang, J. L. Xiao, W. D. Liang, and Y. J. Peng, 2005: Source and distribution of pollen in the surface sediment of Daihai Lake, Inner Mongolia. Quat. Int., 136 , 33–45.

    • Search Google Scholar
    • Export Citation

  • Zagwijn, W. H., 1960: Aspects of the Pliocene and Early Pleistocene vegetation in the Netherlands. Meded. Geol. Sticht., 5 , 1–78.

  • Zagwijn, W. H., 1994: Reconstruction of climate change during the Holocene in western and central Europe based on pollen records of indicator species. Veg. Hist. Archaeobot., 3 , 65–88.

    • Search Google Scholar
    • Export Citation

  • Zhang, J. C., and Z. G. Lin, 1992: Climate of China. Wiley, 376 pp.

  • Zhang, Y. T., 1937: Changes of Daihai Lake shorelines and the climatic significance (in Chinese). Geol. Rev., 2 , 263–266.

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