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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

Published online by Cambridge University Press:  20 January 2017

James L. Bischoff ,
Kirsten M. Menking ,
Jeffrey P. Fitts  and
John A. Fitzpatrick
James L. Bischoff
Affiliation:
U.S. Geological Survey, Menlo Park, California, 94025
Kirsten M. Menking
Affiliation:
U.S. Geological Survey, Menlo Park, California, 94025
Jeffrey P. Fitts
Affiliation:
U.S. Geological Survey, Menlo Park, California, 94025
John A. Fitzpatrick
Affiliation:
U.S. Geological Survey, Menlo Park, California, 94025
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Abstract

Chemical analyses of the acid-soluble and clay-size fractions of sediment samples (1500-yr resolution) reveal oscillations of lake salinity and of glacial advances in core OL-92 back to 155,000 yr B.P. Relatively saline conditions are indicated by the abundance of carbonate and smectite (both pedogenic and authigenic), reflected by Ca, Sr, and Mg in the acid-soluble suite, and by Cs2O, excess MgO, and LOI (loss on ignition) in the clay-size fraction. Rock flour produced during glacial advances is represented by the abundance of detrital plagioclase and biotite in the clay-size fraction, the ratio of which remains essentially constant over the entire time span. These phases are quantitatively represented by Na2O, TiO2, Ba, and Mn in the clay fraction. The rock-flour record indicates two major ice-advances during the penultimate glacial cycle corresponding to marine isotope stage (MIS) 6, no major advances during the last interglaciation (entire MIS 5), and three major advances during the last glacial cycle (MIS 2, 3, and 4). The ages of the latter three correspond rather well to36Cl dates reported for Sierra Nevada moraines. The onset of the last interglaciation is shown by abrupt increases in authigenic CaCO3and an abrupt decrease in rock flour, at about 118,000 yr B.P. according to our time scale. In contrast, the boundary appears to be gradual in the δ18O record in which the change from light to heavy values begins at about 140,000 yrs B.P. The exact position of the termination, therefore, may be proxy-dependent. Conditions of high carbonate and low rock flour prevailed during the entire period from 118,000 yr B.P. until the glacial advance at 53,000 yr B.P. signaled the end of this long interglaciation.

Type
Research Article
Information
Quaternary Research , Volume 48 , Issue 3 , November 1997 , pp. 313 - 325
Copyright
University of Washington

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References

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
Beetem, W.A., Janzer, V.J., Wahlberg, J.S., (1962). Use of cesium-137 in the determination of cation exchange capacity. U.S. Geological Survey Bulletin. 1140-B, B1–B8.Google Scholar
Benson, L.V., Burdett, J.W., Kashgarian, M., Lund, S.P., Phillips, F.M., Rye, R.O., (1996). Climatic and hydrologic oscillations in the Owens Lake Basin and adjacent Sierra Nevada, California. Science. 274, 746–749.CrossRefGoogle Scholar
Berner, R.A., (1970). Sedimentary pyrite formation. American Journal of Science. 268, 1–23.CrossRefGoogle Scholar
Bischoff, J.L., Fitts, J.P., Fitzpatrick, J.A., (1997). Responses of sediment geochemistry to climate change in Owens Lake sediment: An 800 ky record of saline/fresh cycles. An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper 317, p. 37–47.Google Scholar
Bischoff, J.L., Stafford, T.W. Jr., 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., An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper 317, 91–98.Google Scholar
Bischoff, J.L., Rosenbauer, R.J., Smith, G.I., (1985). Uranium-series dating of sediments from Searles Lake, California: differences between continental and marine climate records. Science. 227, 1221–1222.Google Scholar
Bradbury, J. P., (1997). A diatom-based paleohydrologic record of climate change for the past 800 ky from Owens Lake, California, An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Smith, G. I., Bischoff, J., Geological Society of America Special Paper. 317,, 99, 112.Google Scholar
Carter, C., (1997). Ostracodes in Owens Lake sediments of core OL-92: Alternation of saline and fresh water forms through time. Smith, G.I., Bischoff, J., An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper, 317, 113–120.Google Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N.S., Hammer, C.U., Hvidberg, C.S., Steffensen, J.P., Sveinbjörnsdottir, A.E., Jouzel, J., Bond, G., (1993). Evidence for general instability of past climate from a 250-kyr ice-core record. Nature. 364, 21–220.Google Scholar
Deer, W.A., Howie, R.A., Zussman, J., (1962). Rock Forming Minerals. Longmans, London. Google Scholar
Galehouse, J.S., (1971). Sedimentation analysis. Carver, R., Procedures in Sedimentary Petrology. Wiley–Interscience, New York, 69–94.Google Scholar
Garrels, R.M., Mackenzie, F.T., (1967). Origin of the chemical compositions of some springs and lakes. Equilibrium Concepts in Natural Water Systems. Advances in Chemistry Series. 67, p. 222–242.Google Scholar
Glen, J.M., Coe, R.S., (1997). Paleomagnetism and magnetic susceptibility of Pleistocene sediments from drill hole OL-92, Owens Lake, CA. Smith, G.I., Bischoff, J., An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper 317, 67–78.Google Scholar
Jackson, M.L., (1969). Soil Chemical Analysis-Advanced Course: 2nd Edition. M. L. Jackson, Madison. Google Scholar
Jones, B.F., (1986). Clay mineral diagenesis in lacustrine sediments. Mumpton, F., Studies in Diagenesis. U.S. Geological Survey Bulletin, 1578, 291–300.Google Scholar
Hallberg, G.R., Lucas, J.R., Goodmen, C.M., (1978). Semi-quantitative analysis of clay mineralogy. Hallberg, G.R., Standard Procedures for Evaluation of Quaternary Materials in Iowa. Iowa Geological Survey Technical Information Series 8, 5–21.Google Scholar
Hay, R.L., Guldman, S.G., Matthews, J.C., Lander, R.H., Duffin, M.E., Kyser, T.K., (1991). Clay mineral diagenesis in core KM-3 of Searles Lake, California. Clays and Clay Minerals. 39, 84–96.Google Scholar
Litwin, R., Adam, D.P., Frederiksen, N.O., Woolfenden, W.B., (1997). A palynomorph record of Owens Lake sediments of core OL-92: Preliminary analyses. Smith, G.I., Bischoff, J., An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper 317, 127–142.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C. Jr., Shackleton, N.J., (1987). Age dating and the orbital theory of the ice ages; development of a high-resolution 0 to 300,000-year chronostratigraphy. Quaternary Research. 27, 1–29.Google Scholar
Menking, K.M., (1997). Climatic signals in clay mineralogy and grain-size variations in Owens Lake core OL-92, eastern California. Smith, G.I., Bischoff, J., An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper 317, 25–36.Google Scholar
Menking, K.M., Bischoff, J.L., Fitzpatrick, J.A., Burdette, J.W., Rye, R.O., (1997). Climatic/hydrologic oscillations since 155,000 yr B.P. at Owens Lake, CA, reflected in abundance and stable isotope composition of sediment carbonate. Quaternary Research. 48, 58–68.Google Scholar
Moore, D.M., Reynolds, R.C., (1989). Clay Minerals and Their X-Ray Identification. Oxford Univ. Press, New York. Google Scholar
Muhs, D. R., (1992). The last interglacial-glacial transition in North America: evidence from uranium-series dating of coastal deposits, The Last Interglacial–Glacial Transition in North America. Clark, P., Lea, P., Geological Society of America Special Paper. 270,, 31, 51.CrossRefGoogle Scholar
Müller, G., Irion, G., Forstner, U., (1972). Formation and diagenesis of inorganic Ca–Mg carbonates in the lacustrine environment. Naturwissenschaften. 59, 158–164.CrossRefGoogle Scholar
Newton, M., (1991). Holocene Stratigraphy and Magnetostratigraphy of Owens and Mono Lakes, Eastern California. University of Southern California. Google Scholar
Phillips, F.M., Zreda, M.G., Benson, L.V., Plummer, M.A., Elmore, D., Sharma, P., (1996). Chronology for fluctuations in Late Plesitocene Sierra Nevada glaciers and lakes. Science. 274, 749–751.Google Scholar
Sarna-Wojcicki, A.M., Pringle, M.S., (1992). Laser-fusion40 39 . EOS. 73, 146.Google Scholar
Smith, G.I., (1991). Continental paleoclimate records and their significance. Morrison, R.B., The Geology of North America, Volume K-2, Quaternary Nonglacial Geology: Conterminous U.S.. Geological Society of America, Boulder, 35–41.Google Scholar
Smith, G.I., (1983). Core KM-3, a Surface-to-Bedrock Record of Late Cenozoic Sedimentation in Searles Valley, California. U.S. Geological Survey Professional Paper. 1256, p. 1–24.Google Scholar
Smith, G.I., Bischoff, J.L., (1997). Core OL-92 from Owens Lake: Project rationale, geologic setting, drilling procedures, and summary. Smith, G.I., Bischoff, J., An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper 317, 1–8.Google Scholar
Smith, G.I., Bischoff, J.L., Bradbury, J.P., (1997). Synthesis of the paleoclimate record from Owens Lake core OL-92. Smith, G.I., Bischoff, J., An 800,000-Year Geologic and Climatic Record from Owens Lake, California: Core OL-92. Geological Society of America Special Paper 317, 143–160.Google Scholar
Smith, G.I., Street-Perrott, F.A., (1983). Pluvial Lakes in the Western United States. Wright, H.E. Jr., Late Quaternary Environments of the United States. University of Minnesota Press, Minneapolis, 190–211.Google Scholar
Weaver, C.E., Pollard, L.D., (1975). The Chemistry of Clay Minerals. Elsevier, New York. Google Scholar
Winograd, I.J., Coplen, T.B., Landwehr, J.M., Riggs, A.C., Ludwig, K.L., Szabo, B.J., Kolesar, P.T., Revesz, K.M., (1992). Continuous 500,000-year climate record from vein calcite in Devils Hole, Nevada. Science. 258, 255–260.Google Scholar