Hostname: page-component-848d4c4894-mwx4w Total loading time: 0 Render date: 2024-06-26T23:52:33.642Z Has data issue: false hasContentIssue false

Paleomagnetic Investigation of the Bonneville Alloformation, Lake Bonneville, Utah

Published online by Cambridge University Press:  20 January 2017

Joseph C. Liddicoat
Affiliation:
Department of Environmental Science, Barnard College, Columbia University, New York, New York, 10027
Robert S. Coe
Affiliation:
Earth Science Department, University of California, Santa Cruz, Santa Cruz, California, 95064

Abstract

Paleomagnetic secular variation in a portion of the Bonneville Alloformation is compared with secular variation in lacustrine sediments in the Mono Basin, California, and with secular variation in Lake Lahontan sediments in the northwestern Great Basin. The comparison places an age of about 18,000 yr B.P., and a span of 1000 to 3000 yr, on part of a transgressive stage of Lake Bonneville near Delta, Utah, that is coeval with a wet period in the Lahontan Basin.

Type
Original 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

Benson, L., Kashgarian, M., and Rubin, M. (1995). Carbonate deposition, Pyramid Lake subbasin, Nevada. 2. Lake levels and polar jet stream positions reconstructed from radiocarbon ages and elevations of carbonates (tufas) deposited in the Lahontan Basin. Palaeogeography, Palaeoclimatology, Palaeoecology 117, 130.Google Scholar
Benson, L.V., Lund, S.P., Burdett, J.W., Kashgarian, M., Rose, T.P., Smoot, J.P., and Schwartz, M. (1998). Correlation of late-Pleistocene lake-level oscillations in Mono Lake, California, with North Atlantic climate events. Quaternary Research 49, 110.Google Scholar
Broecker, W.S., and Kaufman, A. (1965). Radiocarbon chronology of Lake Lahontan and Lake Bonneville. II. Great Basin. Bulletin of Geological Society of America 76, 537566.Google Scholar
Coe, R.S., and Liddicoat, J.C. (1994). Overprinting of natural magnetic remanence in lake sediments by a subsequent high-intensity field. Nature 367, 5759.Google Scholar
Denham, C.R., and Cox, A. (1971). Evidence that the Laschamp polarity event did not occur 13 300–30 400 years ago. Earth and Planetary Science Letters 13, 181190.Google Scholar
Doh, S.J., and Steele, W.K. (1983). The late Pleistocene geomagnetic field as recorded by sediments from Fargher Lake, Washington, U.S.A. Earth and Planetary Science Letters 63, 385398.Google Scholar
Gilbert, G. K (1890). Lake Bonneville. 1, 438.Google Scholar
Glen, J. M., and Coe, R. S (1997). Paleomagnetism and Magnetic Susceptibility of Pleistocene Sediments from Drill Hole OL-92. Owens Lake, California., 67, 78.Google Scholar
Kaufman, A., and Broecker, W. (1965). Comparison of Th230 14 . Journal of Geophysical Research 70, 40394054.Google Scholar
King, R.F. (1955). The remanent magnetism of artificially deposited sediments. Monthly Notices of the Royal Astronomical Society Geophysical Supplement 7, 115134.Google Scholar
Liddicoat, J. C (1976). A Paleomagnetic Study of Late Quaternary Dry Lake Deposits from the Western United States and Basin of Mexico.Google Scholar
Liddicoat, J.C. (1992). Mono Lake excursion in Mono Basin, California, and at Carson Sink and Pyramid Lake, Nevada. Geophysical Journal International 108, 442452.Google Scholar
Liddicoat, J.C. (1996). Mono Lake excursion in the Lahontan Basin, Nevada. Geophysical Journal International 125, 630635.CrossRefGoogle Scholar
Liddicoat, J.C., and Coe, R.S. (1979). Mono Lake geomagnetic excursion. Journal of Geophysical Research 84, 261271.Google Scholar
Liddicoat, J.C., and Coe, R.S. (1997). Paleomagnetic investigation of Lake Lahontan sediments and its application for dating pluvial events in the northwestern Great Basin. Quaternary Research 47, 4553.Google Scholar
Lund, S.P., Liddicoat, J.C., Lajoie, K.R., Henyey, T.L., and Robinson, S.W. (1988). Paleomagnetic evidence for long-term (104 . Geophysical Research Letters 10, 11011104.CrossRefGoogle 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., Geological Society of America Decade of North America Geology 283320.Google Scholar
Negrini, R.M., and Davis, J.O. (1992). Dating late Pleistocene pluvial events and tephras by correlating paleomagnetic secular variation records from the western Great Basin. Quaternary Research 38, 4659.Google Scholar
Oviatt, C.G. (1997). Lake Bonneville fluctuations and global climate change. Geology 25, 155158.Google Scholar
Oviatt, C.G., Currey, D.R., and Sack, D. (1992). Radiocarbon chronology of Lake Bonneville, eastern Great Basin, U.S.A. Palaeogeography, Palaeoclimatology, Palaeoecology 99, 225241.Google Scholar
Oviatt, C.G., McCoy, W.D., and Nash, W.P. (1994). Sequence stratigraphy of lacustrine deposits, a Quaternary example from the Bonneville Basin, Utah. Geological Society of America Bulletin 106, 133144.Google Scholar
Scott, W.E., McCoy, W.D., Shroba, R.R., and Rubin, M. (1983). Reinterpretation of the exposed record of the last two cycles of Lake Bonneville, western United States. Quaternary Research 20, 261285.Google Scholar
Tarling, D.H. (1983). Palaeomagnetism: Principles and Applications in Geology, Geophysics and Archaeology. Chapman and Hall, London.Google Scholar
Thompson, R.S., Toolin, L.J., Forester, R.M., and Spencer, R.J. (1990). Accelerator-mass spectrometer (AMS) radiocarbon dating of Pleistocene lake sediments in the Great Basin. Palaeogeography, Palaeoclimatology, Palaeoecology 78, 301313.Google Scholar
Varnes, D. J., and Van Horn, R (1991). Surficial Geologic Map of the Oak City Area. Millard County, Utah.Google Scholar
Verosub, K.L., Davis, J.O., and Valastro, S. (1980). A paleomagnetic record from Pyramid Lake, Nevada, and its implications for proposed geomagnetic excursions. Earth and Planetary Science Letters 49, 141148.Google Scholar