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Elevational Shifts of Coleogyne ramossissima in the Mojave Desert during the Little Ice Age

Published online by Cambridge University Press:  20 January 2017

Kimberly L. Hunter  and
Joseph R. McAuliffe
Kimberly L. Hunter
Affiliation:
Department of Biological Sciences, University of Nevada, Las Vegas, Las Vegas, Nevada 89154
Joseph R. McAuliffe
Affiliation:
Desert Botanical Garden, 1201 North Galvin Parkway, Phoenix, Arizona 85008
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Abstract

Plant macrofossils from woodrat (Neotoma) middens collected in the Mojave Desert of southern Nevada were used to reconstruct the timing and magnitude of vegetation change during the past 1000 yr. Although vegetation at the site now is dominated by the shrub Coleogyne ramossissima, this species does not occur in fossil middens prior to 600 ± 50 yr B.P. The appearance and persistence of C. ramosissima in middens was coincident with the Little Ice Age (ca. 1250 to 1850 A.D.) and was probably related to an increase in precipitation.

Type
Research Article
Information
Quaternary Research , Volume 42 , Issue 2 , September 1994 , pp. 216 - 221
Copyright
University of Washington

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References

Beatley, J. C. (1975). Climates and vegetation pattern across the Mojave/Great Basin Desert transition of southern Nevada. American Midland Naturalist 93, 53–70.Google Scholar
Benedict, J. B. (1965). Recent glacial history of an alpine area in the Colorado Front Range, U.S.A. II. Dating the glacial deposits. Journal of Glaciology 7, 77–87.Google Scholar
Benedict, J. B. (1973). Chronology of cirque glaciation, Colorado Front Range. Quaternary Research 3, 584–599.Google Scholar
Bemarbo, J. C. (1981). Quantitative estimates of temperature changes over the last 2700 years in Michigan based on pollen data. Quaternary Research 15, 143–159.Google Scholar
Bowns, J. E., and West, N. E. (1976). “Blackbrush (Coleogyne ramosissima Torn) on Southwestern Utah Rangelands.” Utah Agricultural Experimental Station Research Report 27.Google Scholar
Bradley, W. G., and Deacon, D. E. (1967). “The Biotic Communities of Southern Nevada,” Nevada State Museum Antrhopological Paper No. 13, pp. 203–295. Carson City, NV.Google Scholar
Burbank, D. W. (1981). A chronology of Late Holocene glacier fluctuations on Mount Rainier, Washington. Arctic Alpine Research 13, 369–381.Google Scholar
Cole, K. L. (1981). “Late Quaternary Vegetation of the Grand Canyon: Vegetational Gradients over the Last 25,000 Years.” Unpublished Ph.D. dissertation, University of Arizona, Tucson.Google Scholar
Cole, K. L., and Webb, R. H. (1985). Late Holocene vegetation changes in Greenwater Valley, Mojave Desert, California. Quaternary Research 23, 227–235.CrossRefGoogle Scholar
Conover, W. J. (1971). “Practical Nonparametric Statistics.” Wiley, New York.Google Scholar
Ely, L. L„ Enzel, Y. Baker, V. R„ and Cayan, D. R. (1993). A 5000year record of extreme floods and climate change in the southwestern United States. Science 262, 410–412.Google Scholar
Enzel, Y. Cayan, D. R. Anderson, R. Y., and Wells, S. G. (1989). Atmospheric circulation during Holocene lake stands in the Mojave Desert: Evidence of regional climate change. Nature 341, 44–46.Google Scholar
Finley, R. B. Jr., (1958). The wood rats of Colorado: Distribution and ecology. University of Kansas Publications, Museum of Natural History 10, 213–552.Google Scholar
Finley, R. B. Jr., (1990). Woodrat ecology and behavior and the interpretation of paleomiddens. In “Packrat Middens: The Last 40,00 Years of Biotic Change in the Desert Southwest” (Martin, P. S. Van Devender, T. R., and Betancourt, J. L., Eds.), pp. 28–42. Univ. of Arizona Press, Tucson.Google Scholar
Grove, J. M. (1985). The timing of the Little Ice Age in Scandinavia. In“The Climatic Scene” (Tooley, M. J. and Sheail, C. M., Eds.), pp. 132–153. Hemel Hemps ted, Allen and Unwin.Google Scholar
Grove, J. M. (1988). “The Little Ice Age.” Routledge, London and New York.Google Scholar
Kearney, T. H., and Peebles, R. H. (1960). “Arizona Flora.” Univ. of California Press, Berkeley.Google Scholar
Lamb, H. H. (1966). The early Medieval warm epoch and its sequel. Palaeogeography, Palaeoclimatology, Palaeoecology 1, 13–37.Google Scholar
Lamb, H. H. (1982). “Climate History and the Modem World.” London, Methuen.Google Scholar
Matthes, F. E. (1939). Report of Committee on Glaciers, April 1939. Transactions of the American Geophysical Union 20, 518–523.Google Scholar
McAuliffe, J. R. (1990). A rapid survey method for determination of density and cover in open shrubland communities. Journal of Vegetation Science 1, 653–656.Google Scholar
Munz, P. A. (1974). “A Flora of Southern California.” Univ. of California Press, Stanford.Google Scholar
Reyes, S., and Cadet, D. L. (1988). The southwestern branch of the North American monsoon during summer 1979. Monthly Weather Review 116, 1175–1187.Google Scholar
Rowlands, P. (1980). Regional bioclimatology of the California desert. In “The California Desert: An Introduction to Its Resources and Man’s Impact” (Latting, J., Ed.), California Native Plant Society Special Publication No. 5. Berkeley, CA.Google Scholar
Spaulding, W. G. (1985). “Vegetation and Climates of the Last 45,000 Years in the Vicinity of the Nevada Test Site, South-Central Nevada.” U.S. Geological Survey Professional Paper No. 1329.Google Scholar
Spaulding, W. G. Betancourt, J. L. Cole, K. L., and Croft, L. K. (1990). Packrat middens: Observations about composition, analytical methods, and nature of the data. In “Packrat Middens: The Last 40,00 Years of Biotic Change in the Desert Southwest” (Martin, P. S. Van Devender, T. R., and Betancourt, J. L., Eds,), pp. 59–84. Univ. of Arizona Press, TUcson.Google Scholar
Stine, S. (1990). Past climate at Mono Lake. Nature 345, 391.Google Scholar
Thompson, L. G. Mosley-Thompson, E. Dansgaard, W., and Groster, P. M. (1986). The Little Ice Age as recorded in the stratigraphy of the tropical Quelccaya Ice Cap. Science 234, 361–364.Google Scholar
Turner, R. M. (1982). Mohave Desertscrub. In “Biotic Communities of the American Southwest—United States and Mexico” (Brown, D. E., Ed.), pp. 157–168.Google Scholar
Van Devender, T. R. (1973). “Late Pleistocene Plants and Animals of the Sonoran Desert: A Survey of Ancient Packrat Middens in Southwestern Arizona.” Unpublished Ph.D. dissertation, University of Arizona, TUcson.Google Scholar
Van Devender, T. R. (1987). Holocene vegetation and climate in the Puerto Blanco Mountains, Southwestern Arizona. Quaternary Research 27, 51–72.Google Scholar
Van De vender, T. R., and Spaulding, W. G. (1979). Development of vegetation and climate in the southwestern United States. Science 204, 701–710.Google Scholar
Webb, R. H. Steiger, J. W., and Tiimer, R. M. (1987). Dynamics of Mojave Desert shrub assemblages in the Panamint Mountains, California. Ecology 68(3), 478–490.Google Scholar
Yeaton, R. I. Yeaton, R. W. Waggoner, J. P. III, and Horenstein, J. E. (1985), The ecology of Yucca (Agavaceae) over an environmental gradient in the Mojave Desert: Distribution and interspecific interactions. Journal of Arid Environments 8, 33–44.Google Scholar