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Reconstruction of Holocene Precipitation Patterns in Europe Using Pollen and Lake-Level Data

Published online by Cambridge University Press:  20 January 2017

Joël Guiot ,
Sandy P. Harrison  and
I. Colin Prentice
Joël Guiot
Affiliation:
Laboratoire de Botanique Historique et Palynologie, CNRS UA 1152, Faculté de St. Jérôme F-13397 Marseille, Cedex 13, France
Sandy P. Harrison
Affiliation:
Department of Earth Sciences, Uppsala University, Box 554, S-751 22 Uppsala, Sweden
I. Colin Prentice
Affiliation:
Department of Plant Ecology, Lund University, Östra Vallgatan 14 S-223 61 Lund, Sweden
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Abstract

Lake-level data can be used to refine palaeoclimate reconstructions based on pollen data. This approach is illustrated for the European Holocene. Estimates of P-PET (precipitation minus potential evapotranspiration) were first inferred from modern pollen analogues. The pollen-based estimates were then compared with the status of lakes within a 5° radius. Analogues with P-PET anomalies inconsistent with the lake-level changes were rejected. The "constrained" sets of analogues were used to estimate continental-scale patterns of annual mean temperature and annual precipitation at 3000-yr intervals. Estimated temperature anomalies differed only slightly from the unconstrained reconstructions. Estimated precipitation anomalies, however, showed improved spatial coherence and increased regional contrast and were occasionally reversed in sign. The effect of the constraint was to impose a rational selection among almost equally similar modern pollen analogues with similar temperatures but widely varying moisture regimes. The resulting maps showed clear, spatially coherent patterns of change in precipitation as well as temperature, suitable for comparison with climate-model results. Further improvement of these maps will become possible as a more extensive coverage of lake-level data is obtained.

Type
Research Article
Information
Quaternary Research , Volume 40 , Issue 2 , September 1993 , pp. 139 - 149
Copyright
University of Washington

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References

Bartlein, P. J. Prentice, I. C., and Webb, T. III, (1986). Climatic re-sponse surfaces from pollen data for some eastern North American taxa. Journal of Biogeography 13, 35–57.CrossRefGoogle Scholar
Behre, K.-E. (1988). The role of man in European vegetation history. In “Vegetation History” (Huntley, B. and Webb, T. III, Eds.), pp. 633–672. Kluwer, Dordrecht.Google Scholar
Berger, A. L. (1978). Long-term variations of daily insolation and Quaternary climatic changes. Journal of Atmospheric Sciences 16, 390–403.Google Scholar
Birks, H. J. B. Line, J. M. Juggins, S. Stevenson, A. C, and Ter Braak, C. J. F. (1990). Diatoms and pH reconstruction. Philosophical Transactions of the Royal Society (London) B 327, 263–278.Google Scholar
COHMAP Members (1988). Climatic changes of the last 18,000 years: Observations and model simulations. Science 241, 1043–1052.Google Scholar
Digerfeldt, G. (1988). Reconstruction and regional correlation of Ho-locene lake-level fluctuations in Lake Bysjön, South Sweden. Boreas 17, 165–182.Google Scholar
Efron, B. (1979). Bootstrap methods: Another look at the Jackknife. The Annals of Statistics 7, 1–26.Google Scholar
Efron, B. (1983). Estimating the error rate of a prediction rule: Im-provement on cross-validation. Journal of the American Statistical Association 78, 316–331.CrossRefGoogle Scholar
Federer, C. A. (1982). Transpirational supply and demand: Plant, soil, and atmospheric effects evaluated by simulation. Water Resources Research 18, 355–362.Google Scholar
Guiot, J. (1985). A method for palaeoclimatic reconstruction in paly-nology based on multivariate time-series analysis. Géographie Physique et Quaternaire 39, 115–126.CrossRefGoogle Scholar
Guiot, J. (1987). Late Quaternary climatic change in France estimated from multivariate pollen time series. Quaternary Research 28, 100–118.CrossRefGoogle Scholar
Guiot, J. (1989). Methods of calibration. In “Methods of Dendrochronology: Application to Environmental Sciences” (Cook, E., and Kairiukstis, L., Eds), pp. 165–178. Kluwer, Dordrecht.Google Scholar
Guiot, J. (1990). Methodology of paleoclimatic reconstruction from pollen in France. Palaeogeography, Palaeoclimatology, Palaeoecology 80, 49–69.Google Scholar
Guiot, J. (1991). Structural characteristics of proxy data and methods for quantitative climate reconstruction. Paläoklimaforschung 6, 271–284.Google Scholar
Guiot, J. Pons, A. Beaulieu, J. L. de, and Reille, M. (1989). A 140,000-year climatic 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., and Digerfeldt, G. European lakes as palaeohydrolog-ical and palaeoclimatic indicators. Quarternary Science Reviews, in press.Google Scholar
Harrison, S. P., and Metcalfe, S. E. (1985). Variations in lake levels during the Holocene in North America: An indicator of changes in atmospheric circulation patterns. Géographie Physique et Quaternaire 39, 141–150.Google Scholar
Harrison, S. P. Saarse, L., and Digerfeldt, G. (1991). Holocene changes in lake levels as climate proxydata in Europe. Paläokli-maforschung 6, 285–300.Google Scholar
Harrison, S. P. Prentice, I. C., and Bartlein, P. J. (1992). Influence of insolation and glaciation on atmospheric circulation in the North At-lantic sector: Implications of general circulation models experiments for the Late Quaternary climatology of Europe. Quaternary Science Reviews 11, 283–299.CrossRefGoogle Scholar
Harrison, S. P. Prentice, I. C, and Guiot, J. Climatic controls of Ho-locene lake-level changes in Europe. Climate Dynamics 8, 189–200.CrossRefGoogle Scholar
Huntley, B. (1988). Glacial and Holocene vegetation history: Europe. In “Vegetation History” (Huntley, B. and Webb, T. III, Eds.), pp. 341–384, Kluwer, Dordrecht.CrossRefGoogle Scholar
Huntley, B. (1990a). European vegetation history: Palaeovegetation maps from pollen data—13,000 yr B.P. to present. Journal of Quaternary Science 5, 103–122.Google Scholar
Huntley, B. (1990b). Dissimilarity mapping between fossil and contemporary pollen spectra in Europe for the past 13,000 years. Quaternary Research 33, 360–376.CrossRefGoogle Scholar
Huntley, B., and Birks, H. J. B. (1983). “An Atlas of Past and Present Pollen Maps for Europe 0-13,000 Years Ago.” Cambridge Univ. Press, Cambridge.Google Scholar
Huntley, B., and Prentice, I. C. (1988). July temperatures in Europe from pollen data, 6000 years before present. Science 241, 687–690.Google Scholar
Huntley, B., and Prentice, I. C. (1992). Holocene vegetation and cli-mates of Europe. In “Global Climates since the Last Glacial Maximum” (Wright, H. E. Kutzbach, J. E. Street-Perrott, F. A. Ruddiman, W. F. Webb, T. III, Eds.). Univ. of Minnesota Press, Minneapolis, in press.Google Scholar
Huntley, B. Bartlein, P. J., and Prentice, 1. C. (1989). Climatic control of the distribution and abundance of beech in Europe and North America. Journal of Biogeography 16, 551–560.CrossRefGoogle Scholar
Jarvis, P. G., and MacNaughton, K. G. (1986). Stomatal control of transpiration: Scaling up from leaf to region. Advances in Ecological Research 15, 1–49.Google Scholar
Klimanov, V. (1987). About climatic changes in the northern part of the east-European plain. In “Palaeohydrology of the Temperate Zone III, Mine and Lakes” (Raukas, A. and Saarse, L., Eds.), pp. 23–37. Academy of Sciences of the Estonian S.S.R. Google Scholar
Korff, H. C., and Flohn, H. (1969). Zusammenhang zwischen den Tem-peratur-Gefälle Äquator-Pol und den plantetarischen Luftdruck-gurteln. Annaien der Meteorologie NF 4, 163–164.Google Scholar
Kutzbach, J. E., and Guetter, P. J. (1986). The influence of changing orbital parameters and surface boundary conditions on climate simulations for the past 18,000 years. Journal of the Atmospheric Sciences 43, 1726–1759.Google Scholar
Leemans, R., and Cramer, W. (1991). “The IIASA Data Base for Mean Monthly Values of Temperature, Precipitation and Cloudiness on a Global Terrestrial Grid.” RR-91-18. International Institute for Applied Systems Analysis, Laxenburg.Google Scholar
Mitchell, J. F. B. Grahame, N. S., and Needham, K. J. (1988). Climate simulations for 9000 years before present: Seasonal variations and effects of the Laurentide ice sheet. Journal of Geophysical Research 93, 8283–8303.Google Scholar
Overpeck, J. T. Prentice, I. C, and Webb, T. (1985). Quantitative interpretation of fossil pollen spectra: Dissimilarity coefficients and the method of modern analogs. Quaternary Research 23, 87–108.CrossRefGoogle Scholar
Peterson, G. M. (1983). “Holocene Vegetation and Climate in the Western USSR.” Ph.D. thesis, University of Wisconsin, Madison.Google Scholar
Piggott, C. D., and Huntley, J. P. (1981). Factors controlling the distribution of Tilia cordata at the northern limits of its geographical range. I. Distribution in north-west England. New Phytologist 87, 817–839.Google Scholar
Prentice, I. C Bartlein, P. J., and Webb, T. III, (1991). Vegetation and climate change in eastern North America since the last glacial maximum. Ecology 72, 2038–2056.Google Scholar
Prentice, I. C. Cramer, W. Harrison, S. P. Leemans, R. Monsemd, R. A., and Solomon, A. M. (1992). A global biome model based on plant physiology and dominance, soil properties and climate. Journal of Biogeography 19, 117–134.CrossRefGoogle Scholar
Prentice, I. C Sykes, M. T., and Cramer, W. (1993). A simulation model for the transient effects of climate change on forest landscapes. Ecological Modelling, 65, 51–70.Google Scholar
Saarse, L., and Harrison, S. P. (1992). Holocene lake-level changes in the eastern Baltic region. In “Special Volume for the International Geographical Congress.” Estonian Academy of Sciences, Tallinn, 6–20.Google Scholar
Seret, G. Guiot, J. Wansard, G. Beaulieu, J.-L., and Reille, M. (1992). Tentative paleoclimatic reconstruction linking pollen and sedimentol-ogy in La Grande Pile (Vosges, France), Quaternary Science Reviews 11, 425–430.CrossRefGoogle Scholar
Street, F. A., and Grove, A. T. (1979). Global maps of lake-level fluctuations since 30,000 yr B.P. Quaternary Research 12, 83–118.Google Scholar
Street-Perrott, F. A., and Harrison, S. P. (1985). Lake-levels and climate reconstruction. In “Paleoclimate Analysis and Modeling” (Hecht, A. D., Ed.), pp. 291–340. Wiley, New York.Google Scholar
Street-Perrott, F. A. Marchand, D. S. Roberts, N., and Harrison, S. P. (1989). “Global Lake-Level Variations from 18,000 to 0 Years Ago: A Palaeoclimatic Analysis.” DOE/ER/60304-H1 TR046, U.S. Department of Energy, Washington.CrossRefGoogle Scholar
Till, C, and Guiot, J. (1990). Reconstruction of precipitation in Morocco since AD. 1100 based on Cedrus Atlantica tree-ring widths. Quaternary Research 33, 337–351.Google Scholar
Tuhkanan, S. (1984). A circumboreal system of climate-phytogeographical regions. Acta Botanica Fennica 127, 1–50.Google Scholar
Walter, H. (1979). “Vegetation of the Earth and Ecological Systems of the Geo-biosphere,” 2nd edition. Springer, New York.Google Scholar
Winkler, M. G. Swain, A. M., and Kutzbach, J. E. (1986). Middle Holocene dry period in the northern Midwestern United States: lake levels and pollen stratigraphy. Quaternary Research 25, 235–250.Google Scholar
Woodward, F. I. (1987). “Climate and Plant Distribution.” Cambridge Univ. Press, Cambridge.Google Scholar
Woodward, F. 1. (1988). Temperature and the distribution of plant species. Symposia of the Society for Experimental Biology 42, 59–75.Google ScholarPubMed