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Continuous Lake-Sediment Records of Glaciation in the Sierra Nevada between 52,600 and 12,50014C yr B.P

Published online by Cambridge University Press:  20 January 2017

Larry V. Benson ,
Howard M. May ,
Ronald C. Antweiler ,
Terry I. Brinton ,
Michaele Kashgarian ,
Joseph P. Smoot  and
Steve P. Lund
Larry V. Benson
Affiliation:
United States Geological Survey, 3215 Marine Street, Boulder, Colorado, 80303-1066
Howard M. May
Affiliation:
United States Geological Survey, 3215 Marine Street, Boulder, Colorado, 80303-1066
Ronald C. Antweiler
Affiliation:
United States Geological Survey, 3215 Marine Street, Boulder, Colorado, 80303-1066
Terry I. Brinton
Affiliation:
United States Geological Survey, 3215 Marine Street, Boulder, Colorado, 80303-1066
Michaele Kashgarian
Affiliation:
Lawrence Livermore National Laboratory, P.O. Box 808, Livermore, California, 94550
Joseph P. Smoot
Affiliation:
United States Geological Survey, MS 955, Reston, Virginia, 22092
Steve P. Lund
Affiliation:
Department of Earth Sciences, University of Southern California, Los Angeles, California, 90089
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Abstract

The chemistry of the carbonate-free clay-size fraction of Owens Lake sediments supports the use of total organic carbon and magnetic susceptibility as indicators of stadial–interstadial oscillations. Owens Lake records of total organic carbon, magnetic susceptibility, and chemical composition of the carbonate-free, clay-size fraction indicate that Tioga glaciation began ∼24,500 and ended by ∼13,60014C yr B.P. Many of the components of glacial rock flour (e.g., TiO2, MnO, BaO) found in Owens Lake sediments achieved maximum values during the Tioga glaciation when valley glaciers reached their greatest extent. Total organic carbon and SiO2(amorphous) concentrations reached minimum values during Tioga glaciation, resulting from decreases in productivity that accompanied the introduction of rock flour into the surface waters of Owens Lake. At least 20 stadial–interstadial oscillations occurred in the Sierra Nevada between 52,600 and 14,00014C yr B.P. Total organic carbon data from a Pyramid Lake sediment core also indicate oscillations in glacier activity between >39,500 and ∼13,60014C yr B.P. Alpine glacier oscillations occurred on a frequency of ≤1900 yr in both basins, suggesting that millennial-scale oscillations occurred in California and Nevada during most of the past 52,600 yr.

Keywords

Tioga glaciationSierra NevadaOwens LakePyramid Lake
Type
Original Articles
Information
Quaternary Research , Volume 50 , Issue 2 , September 1998 , pp. 113 - 127
Copyright
University of Washington

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References

Antevs, E. (1938). Postpluvial climatic variations in the southwest. Bulletin of the American Meteorological Society 19, 190–193.Google Scholar
Bard, E., Arnold, M., Fairbanks, R.G., and Hamelin, B. (1993). 230 234 14 . Radiocarbon 35, 191–199.Google Scholar
Bard, E., Hamelin, B., Arnold, M., Montaggioni, L., Cabioch, G., Faure, G., and Rougerie, F. (1996). Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge. Nature 382, 241–244.Google Scholar
Bard, E., Hamelin, B., Fairbanks, R.G., and Zindler, A. (1990). Calibration of the14 . Nature 345, 405–410.Google Scholar
Bateman, P.C. (1961). Granitic formations in the East-Central Sierra Nevada near Bishop, California. Geological Society of America Bulletin 72, 1521–1538.Google Scholar
Benson, L.V., and Thompson, R.S. (1987). Lake-level variation in the Lahontan Basin for the past 50,000 years. Quaternary Research 28, 69–85.CrossRefGoogle Scholar
Benson, L.V., Burdett, J., Lund, S., Kashgarian, M., and Mensing, S. (1997). Nearly synchronous climate change in the Northern hemisphere during the last glacial termination. Nature 388, 263–265.Google Scholar
Benson, L.V., Burdett, J.W., Kashgarian, M., Lund, S.P., Phillips, F.M., and Rye, R.O. (1996). Climatic and hydrologic oscillations in the Owens Lake Basin and adjacent Sierra Nevada, California. Science 274, 746–749.Google Scholar
Benson, L.V., 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, 1–30.Google Scholar
Benson, L.V., and Klieforth, H. (1989). Stable isotopes in precipitation and ground water in the Yucca Mountain region, southern Nevada: Paleoclimatic implications. Aspects of Climate Variability in the Pacific and Western Americas p. 41–59Google Scholar
Benson, L.V., Lund, S.P., Burdett, J.W., Kashgarian, M., Rose, T.P., and Schwartz, M. (1998). Correlation of Late-Pleistocene lake-level oscillations in Mono Lake, California, with North Atlantic climate events. Quaternary Research 49, 1–10.CrossRefGoogle Scholar
Benson, L.V., Smoot, J.P., Kashgarian, M., Sarna-Wojcicki, A., and Burdett, J.W. (1997). Radiocarbon ages and environments of deposition of the Wono and Trego Hot Springs tephra layers in the Pyramid Lake subbasin, Nevada. Quaternary Research 47, 251–260.CrossRefGoogle Scholar
Bischoff, J.L., Menking, K.M., Fitts, J.P., and Fitzpatrick, J.A. (1997). Climatic oscillations 10,000–155,000 yr B.P. at Owens Lake, California, reflected in glacial rock flour abundance and lake salinity in Core OL-92. Quaternary Research 48, 313–325.Google Scholar
Bischoff, J.L., Stafford, T.W., and Rubin, M. (1997). A time–depth scale for Owens Lake sediments of core OL-92: Radiocarbon dates and constant mass-accumulation rate.Smith, G.I., Bischoff, J.L. An 800,000-year paleoclimatic record from Core OL-92, Owens Lake, Southeast California 91–98.Google Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hajdas, I., and Bonani, G. (1997). A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, 1257–1266.Google Scholar
Broecker, W.S., and Walton, A.F. (1959). The geochemistry of14 . Geochimica et Cosmochimica Acta 16, 15–38.Google Scholar
Champion, D.E., Lanphere, M., and Kuntz, M. (1988). Evidence for a new geomagnetic reversal from lava flows in Idaho: Discussion of short polarity reversals in the Brunhes and Late Matuyama polarity chrons. Journal of Geophysical Research 93, 11,667–11,680.Google Scholar
Church, M., and Ryder, J.M. (1972). Paraglacial sedimentation: A consideration of fluvial processes conditioned by glaciation. Geological Society of America Bulletin 83, 3059–3072.CrossRefGoogle Scholar
Clark, D.H. (1995). Extent, timing, and climatic significance of latest Pleistocene and Holocene glaciation in the Sierra Nevada, California.CrossRefGoogle Scholar
Dub, G. D (1947). Owens Lake, California—Source of sodium minerals. 1, 13, American Institute of Mining, Metallurgical, and Petroleum Engineers Technical Publication 2235Google Scholar
Emiliani, C. (1955). Pleistocene temperatures. Journal of Geology 63, 538–578.CrossRefGoogle Scholar
Garbarino, J.R., and Taylor, H.E. (1979). An inductively coupled plasma-atomic emission spectrometric method for routine water quality testing. Applied Spectroscopy 33, 220–226.CrossRefGoogle Scholar
Garbarino, J. R., and Taylor, H. E (1993). Inductively coupled plasma-mass spectrometric method for the determination of dissolved trace elements in water. U.S. Geological Survey Open-File Report 94–358.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.Smith, G.I., Bischoff, J.L. An 800,000-Year Paleoclimatic Record from Core OL-92, Owens Lake, Southeast California 67–78.Google Scholar
Hallet, B., Hunter, L., and Bogen, J. (1996). Rates of erosion and sediment evacuation by glaciers: A review of field data and their implications. Global and Planetary Change 12, 213–235.Google Scholar
Hinkley, T. (1974). Alkali and alkaline earth metals: Distribution and loss in a High Sierra Nevada watershed. Geological Society of America Bulletin 85, 1333–1338.Google Scholar
Hollett, K.J., Danskin, W.R., McCaffrey, W.F., and Walti, C.L. (1991). Geology and water resources of Owens Valley, California. U.S. Geological Survey Water-Supply Paper 2370. Google Scholar
Horn, L.H., and Bryson, R.A. (1960). Harmonic analysis of the annual march of precipitation over the United States. Annals of the Association of American Geographers 50, 157–171.Google Scholar
Jackson, M.L. Soil Chemical Analysis-Advanced Course.(1969). University of WisconsinDept. of Soil Science, Madison.Google Scholar
Keigwin, L., Rio, D., and Acton, G (1997). Initial reports of the ocean drilling project 172. College Station, TX.Google Scholar
Kitagawa, H., and van der Plicht, J. (1998). Atmospheric radiocarbon calibration to 45,000 yr B.P.: Late glacial fluctuations and cosmogenic isotope production. Science 279, 1187–1190.CrossRefGoogle Scholar
Kukla, G.J. (1981). Pleistocene Climates on Land.Berger, A. Climatic Variations and Variability: Facts and Theories Reidel, Dordrecht.207–232.CrossRefGoogle Scholar
Kutzbach, J.E., and Guetter, P.J. (1986). The influence of changing orbital parameters and surface boundary conditions of climate simulations for the past 18,000 years. Journal of Atmospheric Science 43, 1726–1759.Google Scholar
Lund, S.P. (1993). Paleomagnitic secular variation. Trends in Geophysical Research Council of Scientific Research Integration, Trivandrum.p. 143–155Google 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 15, 1101–1104.Google Scholar
Manabe, S., and Broccoli, A.J. (1985). The influence of continental ice sheets on the climate of an ice age. Journal of Geophysical Research 90, 2167–2190.Google Scholar
Menking, K. M (1997). Climatic signals in clay mineralogy and grain-size variations in Owens Lake core OL-92. Southeast California. An 800,000-year paleoclimatic record from Core OL-92, Owens Lake, Southeast California, Geological Society of America Special Paper 317 Google Scholar
Newton, M (1991). Holecene stratigraphy and magnetostratigraphy of Owens and Mono Lakes. eastern California, Google Scholar
Phillips, F.M., Zreda, M.G., Benson, L.V., Plummer, M.A., Elmore, D., Sharma, P. Chronology for fluctuations in Late Pleistocene Sierra Nevada glaciers and lakes Science 274, (1996). 749–751.Google Scholar
Phillips, F.M., Zreda, M.G., Gosse, J.C., Klein, J., Evenson, E.B., Hall, R.D., Chadwick, O.A., and Sharma, P. (1997). Cosmogenic36 10 . Geological Society of America Bulletin 109, 1453–1463.Google Scholar
Pyke, C. B (1972). Some meteorological aspects of the seasonal distribution of precipitation in the Western United States and Baja California. University of California Water Resources Center Contribution, 139 Google Scholar
Riehl, H., Alaka, M.A., Jordan, C.L., and Renard, R.J. (1954). The jet stream. Meteorology and Monograph 2, 23–47.Google Scholar
Sarna-Wojcicki, A.M., and Pringle, M.S. (1992). LaserOfusion 40Ar/39Ar ages of the tuff of Taylor Canyon and Bishop ash bed. California, E., Nevada, W., Nevada. Transactions, American Geophysical Union 73, 146 Google Scholar
Smith, G.I., Friedman, I., and McLaughlin, R.J. (1987). Studies of quaternary saline lakes—III. Mineral, chemical, and isotopic evidence of salt solution and crystallization process in Owens Lake, California, 1969–1971. Geochimica et Cosmochimica Acta 51, 811–827.Google Scholar
Starrett, L.G. (1949). The relation of precipitation patterns in North America to certain types of jet streams at the 300-millibar level. Journal of Meteorology 6, 347–352.Google Scholar
Stuiver, M., and Becker, B. (1993). High-precision decadal calibration of the radiocarbon time scale, AD 1950–6000 BC. Radiocarbon 35, 35–65.Google Scholar
Wahrhaftig, C., and Birm, J.H. (1956). The Quaternary of the Pacific Mountain system in California.Morrison, R., Wright, H.E. Jr. Means of Correlation of Quaternary Successions. Vol. 8, Proceedings, VII Congress International Association for Quaternary Research University of Utah Press, Salt Lake City.293 Google Scholar
Williams, D.F., Thunell, R.C., Tappa, E., Rio, D., and Raffi, I. (1988). Chronology of the Pleistocene oxygen isotope record: 0–1.88 m.y. B.P. Palaeogeography, Palaeoclimatology, Palaeoecology 64, 221–240.CrossRefGoogle Scholar