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Reinterpretation of the Burmester Core, Bonneville Basin, Utah

Published online by Cambridge University Press:  20 January 2017

Charles G. Oviatt ,
Robert S. Thompson ,
Darrell S. Kaufman ,
Jordon Bright  and
Richard M. Forester
Charles G. Oviatt
Affiliation:
Department of Geology, Kansas State University, Manhattan, Kansas, 66506
Robert S. Thompson
Affiliation:
Box 25046, MS 980, United States Geological Survey, Denver, Colorado, 80225
Darrell S. Kaufman
Affiliation:
Departments of Geology and Environmental Sciences, Northern Arizona University, Flagstaff, Arizona, 86011-4099
Jordon Bright
Affiliation:
Departments of Geology and Environmental Sciences, Northern Arizona University, Flagstaff, Arizona, 86011-4099
Richard M. Forester
Affiliation:
Box 25046, MS 980, United States Geological Survey, Denver, Colorado, 80225
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Abstract

Initial interpretation of the sediments from the Burmester core (Eardley et al. (1973). Geological Society of America Bulletin 84, 211–216) indicated that 17 deep-lake cycles, separated by shallow-lake and soil-forming intervals, occurred in the Bonneville basin during the Brunhes Chron (the last 780 × 103 yr). Our re-examination of the core, along with new sedimentological, geochronological, and paleontological data, indicate that only four deep-lake cycles occurred during this period, apparently correlative with marine oxygen-isotope stages 2, 6, 12, and 16. This interpretation suggests that large lakes formed in the Bonneville basin only during the most extensive of the Northern Hemisphere glaciations.

Type
Research Article
Information
Quaternary Research , Volume 52 , Issue 2 , September 1999 , pp. 180 - 184
Copyright
University of Washington

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References

Aber, J.S. (1991). The glaciation of northeastern Kansas. Boreas. 20, 297–314.Google Scholar
Eardley, A.J., Shuey, R.T., Gvosdetsky, V., Nash, W.P., Picard, M.D., Grey, D.C., Kukla, G.J. (1973). Lake cycles in the Bonneville basin, Utah. Geological Society of America Bulletin. 84, 211–216.Google Scholar
Forester, R.M., Colman, S.M., Reynolds, R.L., Keigwin, L.D. (1994). Lake Michigan's late Quaternary limnological and climate history from ostracodes, oxygen isotopes, and magnetic susceptibility. Journal of Great Lakes Research. 20, 93–107.Google Scholar
Gansecki, C.A., Mahood, G.A., McWilliams, M. (1998). New ages for the climatic eruptions at Yellowstone: Single-crystal 40Ar/39Ar dating identifies contamination. Geology. 26, 343–346.Google Scholar
Imbrie, J., Hays, J.D., Martinson, D.G., McIntyre, A., Mix, A.C., Morley, J.J., Pisias, N.G., Prell, W.L., Shackleton, N.J. (1984). The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ18O record. Berger, L. Milankovitch and Climate, Part 1. Reidel, Norwell., 269–305.Google Scholar
Izett, G. A and Wilcox, R. E.(1982). Map Showing Localities and Inferred Distributions of the Huckleberry Ridge. Meas Falls, and Lava Creek Ash Beds (Pearlette Family Ash Beds) of Pliocene and Pleistocene Age in the Western United States and Southern Canada. U.S. Geological Survey Miscellaneous Investigations Series Map I-1325, scale 1:4,000,000.Google Scholar
Izett, G.A., Pierce, K.L., Naeser, N.D., Jaworowski, C. (1992). Isotopic dating of Lava Creek B tephra in terrace deposits along the Wind River, Wyoming—Implications for post 0.6 Ma uplift of the Yellowstone hotspot. Geological Society of America Abstracts with Programs. 24, A102.Google Scholar
Kaufman, D.S., Manley, W.F. (1998). A new procedure for determining enantiomeric (D/L) amino acid ratios in fossils using reverse phase liquid chromatography. Quaternary Science Reviews (Quaternary Geochronology). 17, 987–1000.Google Scholar
McCoy, W. D. (1981). Quaternary Aminostratigraphy of the Bonneville and Lahontan Basins, Western U. A, with Paleoclimatic Implications. Unpublished Ph.D. dissertation, University of Colorado.Google Scholar
McCoy, W.D. (1987). Quaternary aminostratigraphy of the Bonneville basin, western United States. Geological Society of America Bulletin. 98, 99–112.Google Scholar
Mitterer, R.M., Kriausakul, N. (1989). Calculation of amino acid racemization ages based upon apparent parabolic kinetics. Quaternary Science Reviews. 8, 853–857.Google Scholar
Morrison, R.B. (1991). Quaternary stratigraphic, hydrologic, and climatic history of the Great Basin, with emphasis on Lakes Lahontan, Bonneville, and Tecopa. Morrison, R.B. Quaternary Nonglacial Geology: Conterminous U.S., “The Geology of North America, Vol. K-2. Geological Society of America, Boulder., 283–320.Google Scholar
Oviatt, C.G., Currey, D.R., Sack, D. (1992). Radiocarbon chronology of Lake Bonneville, eastern Great Basin, USA. Palaeogeography, Palaeoclimatology, Palaeoecology. 99, 225–241.Google Scholar
Oviatt, C.G., McCoy, W.D., Reider, R.G. (1987). Evidence for a shallow early or middle Wisconsin lake in the Bonneville basin Utah. Quaternary Research. 27, 248–262.Google Scholar
Oviatt, C.G., Miller, D.M. (1997). New explorations along the northern shores of Lake Bonneville. Link, P.K., Kowallis, B.J. Mesozoic to Recent Geology of Utah. 345–371.Google Scholar
Scott, W.E., McCoy, W.D., Shroba, R.R., Rubin, M. (1983). Reinterpretation of the exposed record of the last two cycles of Lake Bonneville, western United States. Quaternary Research. 20, 261–285.Google Scholar
Spielhagen, R.F., Bonani, G., Eisenhaur, A., Frank, M., Frederichs, T., Kassens, H., Kubik, P.W., Mangini, A., Nørgaard-Pedersen, N., Schäper, S., Stein, R., Thiede, J., Tiedemann, R., Wahsner, M. (1997). Arctic Ocean evidence for late Quaternary initiation of northern Eurasian ice sheets. Geology. 25, 783–786.Google Scholar
Thompson, R.S., Whitlock, C., Bartlein, P.J., Harrison, S.P., Spaulding, W.G. (1993). Climatic changes in the western United States since 18,000 yr B.P. Wright, H.E. Jr., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J. Global Climates since the Last Glacial Maximum. University of Minnesota Press, Minneapolis., 468–513.Google Scholar
Williams, S.K. (1994). Late Cenozoic tephrochronology of deep sediment cores from the Bonneville basin, northwest Utah. Geological Society of America Bulletin. 105, 1517–1530.Google Scholar