Hostname: page-component-76fb5796d-wq484 Total loading time: 0 Render date: 2024-04-28T08:28:57.111Z Has data issue: false hasContentIssue false

Pollen Analysis of Fossil Packrat Middens from the Sonoran Desert

Published online by Cambridge University Press:  20 January 2017

James E. King
Affiliation:
Quaternary Studies Center, Illinois State Museum, Springfield, Illinois 62706
Thomas R. Van Devender
Affiliation:
Department of Geosciences, University of Arizona, Tucson, Arizona 85721

Abstract

Pollen contained in 22 fossil packrat middens from the Sonoran Desert provides a complementary, but differing, view of the paleoenvironment from that derived by analysis of the associated plant macrofossils. The regional component of the pollen data is in sharp contrast to the locally oriented macrofossils. A total of 84 macrofossil taxa and 47 pollen taxa were identified; only 18 taxa were common to both. The low Index of Similarity, 0.4, indicates that the two sources of fossil information are providing different sets of paleobotanical data. When combined with plant macrofossils and good radiocarbon dating control, the pollen spectra derived from fossil middens are compatable with other paleoenvironmental sequences.

Type
Research Article
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Adam, D.P., Mehringer, P.J. Jr., (1975). Modern pollen surface samples—an analysis of subsamples. Journal of Research, U. S. Geological Survey. 3, 733-736.Google Scholar
Bartos, F.M., (1972). Pollen in Fecal Pellets as an Environmental Indicator. M.S. Thesis. University of Arizona. Google Scholar
Curtis, J.T., (1959) The Vegetation of Wisconsin. Univ. of Wisconsin Press, Madison. Google Scholar
Finley, R.B. Jr., (1958). The wood rats of Colorado: Distribution and ecology. University of Kansas, Publications of the Museum of Natural History. 10, 213-552.Google Scholar
Hevly, R.H., Mehringer, P.J. Jr., Yocum, H.G., (1965). Modern pollen rain in the Sonoran Desert. Journal of the Arizona Academy of Science. 3, 123-135.Google Scholar
King, J.E., Sigleo, W.R., (1973). Modern pollen in the Grand Canyon, Arizona. Geosciences and Man. 7, 73-81.Google Scholar
Lanner, R.M., Van Devender, T.R., (1974). Morphology of pinyon pine needles from fossil packrat middens in Arizona. Forest Science. 20, 207-211.Google Scholar
Leskinen, P.H., (1970). Late Pleistocene Vegetation Change in the Christmas Tree Pass Area, Newberry Mountains, Nevada. M.S. Thesis. University of Arizona. Google Scholar
Leskinen, P.H., (1975). Occurrence of oaks in the late Pleistocene vegetation in the Mohave Desert of Nevada. Madroño. 23, 234-235.Google Scholar
Madsen, D.B., (1973). Late Quaternary Paleoecology in the Southeastern Great Basin. Ph.D. Dissertation. University of Missouri. Google Scholar
Martin, P.S., 1963a. Geochronology of pluvial Lake Cochise, southern Arizona. II. Pollen analysis of a 42-meter core. Ecology. 44, 436-444.Google Scholar
Martin, P.S., 1963b The Last 10,000 Years, a Fossil Pollen Record of the American Southwest. Univ. of Arizona Press, Tucson. Google Scholar
Martin, P.S., Mehringer, P.J. Jr., (1965). Pleistocene pollen analysis and biogeography of the southwest. Wright, H.E. Jr., Frey, D.G., The Quaternary of the United States. Princeton Univ. Press, Princeton, N. J, 433-451.Google Scholar
Mehringer, P.J. Jr., (1967). Pollen analysis of the Tule Springs site, Nevada. Wormington, H.M., Ellis, D., Pleistocene Studies in Southern Nevada. Nevada State Museum Anthropological Papers. 129-200 No. 13.Google Scholar
Mehringer, P.J. Jr., Ferguson, C.W., (1969). Pluvial occurrence of bristlecone pine (Pinus aristata) in a Mohave Desert mountain range. Journal of the Arizona Academy of Science. 5, 284-292.Google Scholar
Phillips, A.M. III, (1976). Packrats, plants and the Pleistocene in the lower Grand Canyon of Arizona. American Quaternary Association Abstracts of Fourth Biennial Meeting. 70-71.Google Scholar
Phillips, A.M. III, Van Devender, T.R., (1974). Pleistocene packrat middens from the lower Grand Canyon of Arizona. Journal of the Arizona Academy of Science. 9, 117-119.Google Scholar
Shreve, F., (1964). Vegetation of the Sonoran Desert. Vegetation and Flora of the Sonoran Desert. Stanford Univ. Press, Stanford, Calif, 1-186 by F. Shreve and I. L. Wiggins.Google Scholar
Spaulding, W.G., (1974). Pollen Analysis of Fossil Dung of Ovis canadensis from Southern Nevada. M.S. Thesis. University of Arizona. 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. Ph.D. Dissertation. University of Arizona. Google Scholar
Van Devender, T.R., (1976). The biota of the hot deserts of North America during the last glaciation: The packrat midden record. American Quaternary Association Abstracts of Fourth Biennial Meeting. 62-67.Google Scholar
Van Devender, T.R., King, J.E., (1971). Late Pleistocene vegetational records in western Arizona. Journal of the Arizona Academy of Science. 6, 240-244.Google Scholar
Van Devender, T.R., Mead, J.I., (1976). Late Pleistocene and modern plant communities of Shinumo Creek and Peach Springs Wash, lower Grand Canyon, Arizona. Journal of the Arizona Academy of Science. 11, 16-22.Google Scholar
Wells, P.V., (1966). Late Pleistocene vegetation and degree of pluvial climatic change in the Chihuahuan Desert. Science. 153, 970-975.Google Scholar
Wells, P.V., (1976). Macrofossil analysis of wood rat (Neotoma) middens as a key to the Quaternary vegetational history of arid America. Quaternary Research. 6, 223-248.CrossRefGoogle Scholar
Wells, P.V., Berger, R., (1967). Late Pleistocene history of coniferous woodland in the Mohave Desert. Science. 155, 1640-1647.Google Scholar
Wells, P.V., Jorgensen, C.D., (1964). Pleistocene wood rat middens and climatic change in the Mohave Desert: A record of juniper woodlands. Science. 143, 1171-1173.Google Scholar