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Modeling Climate Limits of Plants Found in Sonoran Desert Packrat Middens

Published online by Cambridge University Press:  20 January 2017

Samantha Thompson Arundel
Samantha Thompson Arundel*
Affiliation:
Department of Geography and Public Planning, Northern Arizona University, Flagstaff, Arizona, 86011, E-mail: [email protected]
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Abstract

Geostatistical analyses of 35 plant species from 213 packrat middens with combined records spanning the last 40,000 yr indicate that many presumed winter precipitation-dependent taxa that existed in the Sonoran Desert during the last glaciation were expelled by increasing monsoon precipitation instead of waning cool-season moisture. The statistical influence of excessive monsoon rainfall on the distributions of many species probably reflects the simultaneous increase in the magnitude and occurrence of fire. During the early Holocene, results indicate a dramatic decrease in cool-season precipitation and an increase in monsoon rainfall. Levels of temperature and precipitation continued to change linearly until they reached modern values. These conclusions are drawn from a newly developed computer model that determines which climatic factors impede species movement into an unoccupied region. Climatic “limiters,” derived from digital versions of modern plant distributions, elevation, and meteorological data, formed the basis of the reconstructions. Particularly important distribution limiters for the Sonoran Desert include maximum warm-season precipitation and low winter temperatures. The model allows for quantitative estimates of past climatic changes with relatively detailed temporal and spatial resolutions. These results can be used to refine paleoclimatic interpretations based on coarser resolution General Circulation Models.

Keywords

paleoclimatic reconstructionclimatic limitersmacrofossilsGeographic Information SystemsSonoran Desert
Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 2 , September 2002 , pp. 112 - 121
Copyright
University of Washington

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References

Bartlein, P.J., Prentice, I.C., Webb, T. III Climatic response surfaces from pollen data for some eastern North American taxa. Journal of Biogeography 13, (1986). 35 57.CrossRefGoogle Scholar
Betancourt, J.L., and Van Devender, T.R. Holocene vegetation in Chaco Canyon, New Mexico. Science 214, (1981). 656 658.CrossRefGoogle ScholarPubMed
Chang, C. P, and Krishnamurti, T. N. 1987, Monsoon Meteorology, Oxford Univ. Press, New York.Google Scholar
Science 241, (1988). 1043 1052.CrossRefGoogle Scholar
Delfiner, P., and Delhomme, J. P. (1975). Optimum interpolation by kriging.. In Display and Analysis of Spatial DataJ. D. Davis and M. J. McCullagh, Eds., pp. 96–114. Wiley, New York.Google Scholar
Dimmitt, M. Arizona Upland: The land of five seasons. Sonorensis 12, (1991). 2 4.Google Scholar
Dwyer, D.D., and Pieper, R.D. Fire effects on blue gramma-pinyon-juniper rangeland in New Mexico. Journal of Range Management 30, (1967). 359 362.CrossRefGoogle Scholar
Griffith, D. A, and Amrhein, C. G. 1991, Statistical Analysis for Geographers, Prentice Hall, New York.Google Scholar
Hastings, J. R, Turner, R. M, and Warren, D. K. 1972, An Atlas of Some Plant Distributions in the Sonoran Desert. Technical Reports on the Meteorology and Climatology of Arid Regions No. 21, Univ. of Arizona, Institute of Atmospheric Physics, Tucson.Google Scholar
Huntley, B., Bartlein, P.J., and Prentice, I.C. Climatic control of the distribution and abundance of beech (Fagus L.) in Europe and North America. Journal of Biogeography 16, (1989). 551 560.CrossRefGoogle Scholar
Hutchinson, M.F. A new objective method for spatial interpolation of meteorological variables from irregular networks applied to the estimation of monthly mean solar radiation, temperature, precipitation and windrun. CSIRO, Australia, Division of Water Resources Technical Memorandum 89, (1989). 95 104.Google Scholar
Hutchinson, M. F. (1991). Climatic analyses in data sparse regions.. In Climatic Risk in Crop ProductionR. C. Muchow and J. A. Bellamy, Eds., pp. 55–71. CAB International, Wallingford.Google Scholar
Hutchinson, M.F., and Bischof, R.J. A new method for estimating the spatial distribution of mean seasonal and annual rainfall applied to the Hunter Valley, New South Wales. Australian Meteorological Magazine 3, (1983). 179 184.Google Scholar
Koniak, S. Succession in pinyon-juniper woodlands following wildfire in the Great Basin. Great Basin Naturalist 45, (1985). 556 566.Google Scholar
Little, E. L. Jr, 1971, Conifers and Important Hardwoods, U.S. Department of Agriculture Forest Service Miscellaneous Publication, No. 1146, Government Printing Office, Washington, DC.Google Scholar
Little, E. L. Jr, 1974, Minor Western Hardwoods, U.S. Department of Agriculture Forest Service Miscellaneous Publication, No. 1314, Government Printing Office, Washington, DC.Google Scholar
Nowak, R.S., Nowak, C.L., and Tausch, R.J. Probability that a fossil absent from a sample is also absent from the paleolandscape. Quaternary Research 54, (2000). 144 154.CrossRefGoogle Scholar
Prentice, I. C. (1988). Records of vegetation in time and space: The principles of pollen analysis.. In Vegetation History, Handbook of Vegetation Science, Vol. 7B. Huntley and T. Webb, III, Eds., pp. 17–42. Kluwer Academic, Dordrecht.Google Scholar
Spaulding, W.G. Late Wisconsin macrofossil records of desert vegetation in the American southwest. Quaternary Research 19, (1983). 256 264.CrossRefGoogle Scholar
Spaulding, W.G., and Graumlich, L.J. The last pluvial climate episodes in the deserts of southwestern North America. Nature 320, (1986). 441 444.CrossRefGoogle Scholar
Steenburgh, W.F., and Lowe, C.H. Critical factors during the first years of life of the saguaro (Cereus giganteus) at Saguaro National Monument, Arizona. Ecology 50, (1969). 826 834.Google Scholar
Swetnam, T.W., and Betancourt, J.L. Fire-southern oscillation relations in the southwestern United States. Science 249, (1990). 1017 1020.CrossRefGoogle ScholarPubMed
Turner, R.M. Growth in four species of Sonoran Desert trees. Ecology 44, (1963). 760 765.CrossRefGoogle Scholar
Turner, R. M, Bowers, J. E, and Burgess, T. L. 1995, Sonoran Desert Plants, An Ecological Atlas, Univ. of Arizona Press, Tucson.Google Scholar
Van Devender, T. R. (1990). Late Quaternary vegetation and climate of the Sonoran Desert, United States and Mexico.. In Packrat Middens: The Last 40,000 Years of Biotic ChangeJ. L. Betancourt, T. R. Van Devender, and P. S. Martin, Eds., pp. 134–165. Univ. of Arizona Press, Tucson.Google Scholar
Van Devender, T.R., and Spaulding, W.G. Development of vegetation and climate in the southwestern United States. Science 204, (1979). 701 710.CrossRefGoogle ScholarPubMed
Van Devender, T. R., Thompson, R. S., and Betancourt, J. L. (1987). Vegetation history in the Southwest: The nature and timing of the late Wisconsin-Holocene transition.. In North America and Adjacent Oceans during the Last DeglaciationW. F. Ruddiman and H. E. Wright, Jr., Eds., pp. 323–352. Geol. Soc. Am. Boulder, Co.Google Scholar
Wangler, M.J., and Minnich, R.A. Fire and succession in pinyon-juniper woodlands of the San Bernardino Mountains, California. Madroño 4, (1996). 493 514.Google Scholar
Warren, D. K. 1979, Precipitation and Temperature As Climatic Determinants of the Distribution of Fouquieria columnaris, Walden Univ. Massachusetts.Google Scholar
Webb, T. III, and Bartlein, P.J. Late Quaternary climatic change in eastern North America: The role of modeling experiments and empirical studies. Bulletin of the Buffalo Society of Natural Sciences 33, (1988). 3 13.Google Scholar
Webb, T. III, Kutzbach, J., and Street-Perrott, F. A. (1985). 20,000 years of global climatic change: Paleoclimatic research plan.. In Global Change, ICSU Press Symposium 5T. F. Maline and J. G. Roeder, Eds., pp. 182–218. Cambridge Univ. Press, Cambridge, UK.Google Scholar