Hostname: page-component-cd9895bd7-7cvxr Total loading time: 0 Render date: 2024-12-23T01:35:01.842Z Has data issue: false hasContentIssue false

Optical Dating of Holocene Dune Sands in the Ferris Dune Field, Wyoming

Published online by Cambridge University Press:  20 January 2017

Stephen Stokes
Affiliation:
Research Laboratory for Archaeology and the History of Art, and School of Geography, Oxford University, 6 Keble Road, Oxford OXI 3QJ, England
David R. Gaylord
Affiliation:
Department of Geology, Washington State University, Pullman, Washington, 99164-2812

Abstract

Optical dating of late Quaternary quartz dune sands from the Clear Creek portion of Ferris dune field, Wyoming, demonstrates the considerable potential of the technique as a chronostratigraphic tool. A sequence of radiocarbon-dated Holocene interdune strata permit optical dating of the intercalated dune sand to be tested; the concordance is good. The optical dates for the aeolian deposits not datable by radiocarbon suggest that aeolian sedimentation at Clear Creek peaked during two relatively short phases at ca. 8500 and 4000 yr B.P. The dates indicate that aeolian accumulation maxima (at least in the Clear Creek area) may not be synchronous with previously defined phases of marked aridity.

Type
Articles
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

Ahlbrandt, T. S. (1973). “Sand Dunes, Geomorphology and Geology, Killpecker Creek Area, Northern Sweetwater County, Wyoming.” Unpublished Ph.D. dissertation, University of Wyoming, Laramie.Google Scholar
Ahlbrandt, T. S. (1974). Dune stratigraphy, and the chronology of the Killpecker dune field. In “Applied Geology and Archaeology: The Holocene History of Wyoming” (Wilson, M., Ed.), Vol. 10, pp. 5160. Wyoming Geological Survey, Rept. Invest.Google Scholar
Ahlbrandt, T. S. Swinehart, J. B., and Maroney, D. G. (1983). The dynamic Holocene dune fields of the Great Plains and Rocky Moun-tain basins, U.S.A. In “Eolian Sediments and Processes: Developments in Sedimentology 38” (Brookfield, M. E. and Ahlbrandt, T. S., Eds.), pp. 379406. Elsevier, Rotterdam.Google Scholar
Aitken, M. J. (1985). “Thermoluminescence Dating.” Academic Press, London.Google Scholar
Aitken, M. J. (1992). Optical dating. Quaternary Science Reviews 11, 127131.CrossRefGoogle Scholar
Aitken, M. J., and Alldred, J. C. (1972). The assessment of error limits in thermoluminescent dating. Archaeometry 14(2), 257267.CrossRefGoogle Scholar
Aitken, M. J., and Smith, B. W. (1988). Optical dating: Recuperation after bleaching. Quaternary Science Reviews 7, 387393.CrossRefGoogle Scholar
Albanese, J. P. (1974). Geology of the Casper archaeological site, Natrona County, Wyoming. In “Applied Geology and Archaeology: The Holocene History of Wyoming” (Wilson, M., Ed.), Vol. 10, pp. 4650. Wyoming Geological Survey, Rept. Invest.Google Scholar
Benedict, , (1979). “Getting Away from It All: A Study of Man, Mountains and the Two Drought Altithermal.” Annual Meeting Plains Anthropological Association, Denver, CO.Google Scholar
Berger, G. W. (1988). Dating Quaternary events by luminescence. In “Dating Quaternary Sediments” (Easterbrook, D. J., Ed.), pp. 1350. Geological Society of America Special Paper 227.Google Scholar
Bluszcz, A., and Pazdur, M. F. (1985). Comparison of TL and 14C dates of young eolian sediments—A check of the zeroing assumption. Nuclear Tracks and Radiation Measurements 10, 703710.Google Scholar
Dawson, P. J., and Marwitz, J. D. (1982). Wave structures and turbulent features of the winter airflow in southern Wyoming. Geological Society of America Special Paper 192, 5564.Google Scholar
Dijkmans, J. W. A. Wintle, A. G., and Mejdahl, V. (1988). Some ther-moluminescence properties and dating of eolian sands from the Netherlands. Quaternary Science Reviews 7, 349355.Google Scholar
de Jong, A. F. M. Becker, B., and Mook, W. G. (1986). High precision calibration of the radiocarbon time scale, 3930-3230 Cal BC. Radiocarbon 28(2B), 939942.CrossRefGoogle Scholar
Fleming, S. J. (1970). Thermoluminescent dating: Refinement of the quartz inclusion method. Archaeometry 12, 133145.CrossRefGoogle Scholar
Gaylord, D. R. (1982). Geologic history of the Ferris Dune Field, south central Wyoming. Geological Society of America Special Paper 192, 6582.CrossRefGoogle Scholar
Gaylord, D. R. (1983). “Recent Eolian Activity and Palaeoclimate Fluctuations in the Ferris Lost Soldier Area. South Central Wyo-ming.” Unpublished Ph.D. thesis, University of Wyoming, Laramie, WY.Google Scholar
Gaylord, D. R. (1987). Airflow-terrain and hydrological controls on eolian sedimentation and Holocene paleoclimatic fluctuations in Wyoming. Contributions to Geology 25, 157165.Google Scholar
Gaylord, D. R. (1990). Holocene palaeoclimalic fluctuations revealed from dune and interdune strata in Wyoming. Journal of Arid Environments 18, 123138.Google Scholar
Geyh, M. A. Roeschmann, G. Wijmstra, T. A., and Middeldorp, A. A. (1983). The unreliability of 14C dates obtained from buried sandy podzols. Radiocarbon 25, 409416.Google Scholar
Godfrey-Smith, D. I. Huntley, D. J., and Chen, W.-H. (1988). Optical dating studies of quartz and feldspar sediment extracts. Quaternary Science Reviews 7, 373380.Google Scholar
Goodfriend, G. A., and Stipp, J. J. (1983). Limestone and the problem of radiocarbon dating of land-snail shell carbonate. Geology 11, 575577.Google Scholar
Guyton, J. W. (1960). “Geology of the Lost Soldier Area, Sweetwater, Fremont, and Carbon Counties.” Unpublished M.S. dissertation, University of Wyoming, Laramie.Google Scholar
Huntley, D. J. Godfrey-Smith, D. I., and Thewalt, M. L. W. (1985). Optical dating of sediments. Nature 313, 105107.Google Scholar
Koster, E. A. (1988). Ancient and modern cold-climate aeolian sand deposition: A review. Journal of Quaternary Science 3, 6983.CrossRefGoogle Scholar
Kromer, B. Rhein, M. Bruns, M. Schoch-Fischer, H. Munnich, K. O. Stuvier, M., and Becker, B. (1986). Radiocarbon calibration data for the 6th to 8th millenia BC. Radiocarbon 28(2B), 954960.Google Scholar
Lancaster, N. (1988). Development of linear dunes in the southwestern Kalahari, Southern Africa. Journal of Arid Environments 14, 233244.Google Scholar
Linnick, T. W. Long, A. Damon, P. E., and Ferguson, C. W. (1986). High precision radiocarbon dating of bristlecone pine from 6554 to 5350 BC. Radiocarbon 28(2B), 943953.Google Scholar
Martner, B. E. (1985). “Wyoming Climate Atlas.” Univ. of Nebraska Press.Google Scholar
Martner, B. E., and Marwitz, J. D. (1982). Wind characteristics in southern Wyoming. Journal of Applied Meteorology 21, 18151827.Google Scholar
McKee, E. D. (Ed.). (1979). “A Study of Global Sand Seas.” U.S. Geological Survey Professional Paper 1052.Google Scholar
Mears, B. Jr. (1981). Periglacial wedges and the late Pleistocene environment of Wyoming’s intermontane basins. Quaternary Research 15, 171198.Google Scholar
Miller, M. E. (1986). Preliminary investigations at the Seminoe Beach site, Carbon County, Wyoming. Wyoming Archaeologist 29, 8396.Google Scholar
Nambi, K. S. V., and Aitken, M. J. (1986). Annual dose conversion factors for TL and ESR dating. Archaeometry 28, 202205.Google Scholar
Nissen, T. C. (1985). “Field and Laboratory Studies of Selected Periglacial Wedge-Polygons in Southern Wyoming.” Unpublished M.S. dissertation. University of Wyoming, Laramie.Google Scholar
Nissen, T. C. (1990). Pleistocene periglacial wedges: Indicators of a former steppe-tundra environment in Wyoming basins. In “Geological Society of America Abstracts with Programs” (Rocky Mountain Section Meeting, Jackson, Wyoming), Vol. 22 (6), p. 41.Google Scholar
Pearson, G. W. Pilcher, J. R. Bailie, M. G. L. Corbett, D. M., and Qua, F. (1986). High-precision 14C measurement of Irish oaks to show the natural 14C variations from AD 1480-5210 BC. Radiocarbon 28(2B), 911934.Google Scholar
Pipiringos, G. N. (1955). “Tertiary Rocks in the Central Part of the Great Divide Basin, Sweetwater County, Wyoming.” Wyoming Geo-logical Association 10th Annual Field Conference Guidebook, Green River Basin.Google Scholar
Prescott, J. R. (1983). Thermoluminescence dating of sand dunes at Roonka, South Australia. PACT 9, 505512.Google Scholar
Prescott, J. R., and Hutton, J. T. (1988). Cosmic ray and gamma ray dosimetry for TL and ESR. Nuclear Tracks and Radiation Measurements 14(1/2), 223230.Google Scholar
Rhodes, E. J. (1990). “Optical Dating of Sediment.” Unpublished D.Phil. thesis, Oxford University.Google Scholar
Singhvi, A. K. Sharma, Y. P., and Agrawal, D. P. (1982). Thermoluminescence dating of sand dunes in Rajasthan, India. Nature 295, 313315.CrossRefGoogle Scholar
Singhvi, A. K. Deraniyagala, S. U., and Sengupta, D. (1986). Ther-moluminescence dating of Quaternary red-sand beds: A case study of coastal dunes in Sri Lanka. Earth and Planetary Science Letters 80, 139144.Google Scholar
Smith, B. W. Aitken, M. J. Rhodes, E. J. Robinson, P. D., and Gel-dard, D. M. (1986). Optical dating: Methodological aspects. Radiation Protection Dosimetry 17, 229233.Google Scholar
Smith, B. W. Rhodes, E. J. Stokes, S., and Spooner, N. A. (1991). Optical Dating of Quartz. Radiation Protection Dosimetry 34(14), 7578.Google Scholar
Stokes, S. (1991). Quartz-based optical dating of Weichselian cover sands from the eastern Netherlands. Geologic en Mtjnbouw 70, 327337.Google Scholar
Stokes, S. (1992). Optical dating of young (modern) sediments using quartz: Results from a selection of depositional environments. Quaternary Science Reviews 11, 153159.Google Scholar
Stokes, S. Breed, C. S., and Elder, D. (1991). Holocene maintenance of Pleistocene sand dunes in northeastern Arizona: Climatic implications of quartz optical dating. Geological Society of America Abstracts with Programs (Annual Meeting San Diego). p. 354.Google Scholar
Thomas, D. S. G., and Shaw, P. A. (1991). ‘Relict’ desert dune systems: interpretations and problems. Journal of Arid Environments 20, 114.Google Scholar