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Factors Affecting 14C Ages of Lacustrine Carbonates: Timing and Duration of the Last Highstand Lake in the Lahontan Basin

Published online by Cambridge University Press:  20 January 2017

Larry Benson
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Abstract

Two processes contribute to inaccurate 14C age estimates of carbonates precipitated within the Lahontan basin, NevadaCalifornia: low initial 14C/C ratios in lake water (reservoir effect) and addition of modern carbon to calcium carbonate after its precipitation. The mast reliable set of 14C ages on carbonates from elevations > 1310 m in the Pyramid and Walker Lake subbasins indicate that lakes in all seven Lahontan subbasins coalesced ∼14,200 14C yr B.P. forming Lake Lahontan. Lake Lahontan achieved its 1330-m highstand elevation by ∼13,800 14 C yr B.P. and receded to 1310 m by ∼13,700 14C yr B.P. Calculations, based on measured carbonate-accumulation rates, of the amount of time Lake Lahontan exceeded 1310 and 1330 m (500 and 50 yr) are consistent with this chronology. The timing of the Lake Lahontan highstand is of interest because of the linkage of highstand climates with proximity to the polar jet stream. The brevity of the Lahontan highstand is interpreted to indicate that the core of the southern branch of the polar jet stream remained only briefly over the Lahontan basin.

Type
Articles
Information
Quaternary Research , Volume 39 , Issue 2 , March 1993 , pp. 163 - 174
Copyright
University of Washington

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References

Benson, L. V. (1978). Fluctuation in the level of pluvial Lake Lahontan during the last 40,000 years. Quaternary Research 9, 300–318.Google Scholar
Benson, L. V. (1981). Paleoclimatic significance of lake-level fluctuations in the Lahontan Basin. Quaternary Research 16, 390–403.Google Scholar
Benson, L. V. (1984). “Hydrochemical Data for the Truckee River Drainage System, California and Nevada.” U.S. Geological Survey Open File Report 84–440.Google Scholar
Benson, L. V., and Leach, D. L. (1979). Uranium transport in the Walker River basin. Journal of Ceochemical Exploration 11, 227–248.Google Scholar
Benson, L. V., and Mifflin, M. D. (1986). “Reconnaissance Bathymetry of Basins Occupied by Pleistocene Lake Lahontan, Nevada and California.” U.S. Geological Survey Water Resources Investigation Report 85–4262.Google Scholar
Benson, L. V., and Spencer, R. J. (1983). “A Hydrochemical Reconnaissance of the Walker River Basin, California and Nevada.” U.S. Geological Survey Open File Report 83–740.Google Scholar
Benson, L. V., and Thompson, R. S. (1987). The physical record of lakes in the Great Basin. In “North America and Adjacent Oceans during the Last Deglaciation” (Ruddiman, W. F. and Wright, H. E. Jr., Eds.), Vol. K.3, pp. 241–259. Geological Society of America, Boulder, CO.Google Scholar
Benson, L. V. Meyers, P. A., and Spencer, R. J. (1991). Change in the size of Walker Lake during the past 5000 years. Palaeogeography, Palaeoclimatology, Palaeoecology 81, 189–214.CrossRefGoogle Scholar
Broecker, W. S., and Olson, E. A. (1959). Lamont Radiocarbon Measurements VI. American Journal of Science 1, 111–132.Google Scholar
Broecker, W. S., and Walton, A. F. (1959). The geochemistry of 14C in freshwater systems. Geochimica el Cosmochimica Acta 16, 15–38.Google Scholar
Dorn, R. I. Jull, A. J. T. Donahue, D. J. Linick, T. W., and Toolin, L. J. (1990). Latest Pleistocene lake shorelines and glacial chronol-ogy in the western Basin and Range Province, USA: Insights from AMS radiocarbon dating of rock varnish and paleoclimatic implica-tions. Palaeogeography, Palaeoclimatology, Palaeoecology 78, 315–332.Google Scholar
Hostetler, S. W., and Benson, L. V. (1990). Paleoclimatic implications of the high stand of Lake Lahontan derived from models of evaporation and lake level. Climate Dynamics 4, 207–217.Google Scholar
Kutzbach, J. E., and Guetter, P. J. (1986). The influence of changing orbital parameters and surface boundary conditions on climate sim-ulations for the past 18000 years. Journal of Atmospheric Science 43, 1726–1759.Google Scholar
Lao, Y., and Benson, L. V. (1988). Uranium-series age estimates and paleoclimatic significance of Pleistocene tufas from the Lahontan Basin, California and Nevada. Quaternary Research 30, 165–176.Google Scholar
Milne, W. (1987). “A Comparison of Reconstructed Lake-Level Records since the Mid-1800’s of Some Great Basin Lakes. Unpub-lished M.S. thesis, Colorado School of Mines, Golden, CO.Google Scholar
Newton, M. S., and Grossman, E. L. (1988). Late Quaternary chronology of tufa deposits, Walker Lake, Nevada. Journal of Geology 96, 417–433.Google Scholar
Peng, T.-H., and Broecker, W. S. (1980). Gas exchange rates for three closed-basin lakes. Limnology and Oceanography 25, 789–796.Google Scholar
Stuiver, M., and Quay, P. D. (1981). Atmospheric 14C changes resulting from fossil fuel CO2 release and cosmic ray flux variability. Earth and Planetary Science Letters 53, 349–362.Google Scholar
Thompson, R. S. Benson, L. V., and Hattori, E. M. (1986). A revised chronology for the last Pleistocene lake cycle in the central Lahontan basin. Quaternary Research 25, 1–9.Google Scholar
U.S. Geological Survey (1960). “Compilation of Records of Surface Water of the United States through September 1950. Part 10. The Great Basin.” U.S. Geological Survey Water Supply Paper 1314.Google Scholar
U.S. Geological Survey (1963). “Compilation of Records of Surface Water of the United States, October 1950 to September 1960. Part 10. The Great Basin.” U.S. Geological Survey Water Supply Paper 1734.Google Scholar
U.S. Geological Survey (1961-1990). “Water Resources Data for Nevada.” U.S. Geological Survey Water Data Report Series, annual volumes.Google Scholar
Wanninkhof, R. Ledwell, J. R., and Broecker, W. S. (1987). Gas exchange on Mono Lake and Crowley Lake, California. Journal of Geophysical Research 92, 14567–14580.Google Scholar