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Late-Glacial and Early Holocene Vegetation and Climate Change near Owens Lake, Eastern California

Published online by Cambridge University Press:  20 January 2017

Scott A. Mensing*
Affiliation:
Department of Geography, University of Nevada, Reno, Nevada 89557

Abstract

Pollen and algae from Owens Lake in eastern California provide evidence for a series of climatic oscillations late in the last glaciation. Juniper woodland, which dominated the Owens Valley from 16,200 to 15,500 cal yr B.P., suggests much wetter conditions than today. Although still wetter and cooler than today, the area then became fairly warm and dry, with woodland being replaced by shrubs (mainly sagebrush) from 15,500 to 13,100 cal yr B.P. Next, Chenopodiaceae (shadscale) increased, woody species declined, and lake levels fell—all evidence for a brief (ca. 100–200 yr) drought about 13,000 cal yr B.P. The climate continued to oscillate between wet and dry from 13,000 to 11,000 cal yr B.P. After 11,000 cal yr B.P., low lake levels and the increased dominance of desert shrubs indicate the beginning of warm, dry Holocene conditions. The region's climate was unstable during the Younger Dryas but uncertainities in dating prevent identification of the Younger Dryas interval in the Owens Lake record. Comparison of the Owens Lake record with studies in the Sierra Nevada and Great Basin suggest that the climate was generally wetter between 13,000 and 11,000 cal yr B.P., with warmer summers, although no consistent pattern of climate change emerges.

Type
Research Article
Copyright
University of Washington

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References

Adam, D.P., Mehringer, P.J. Jr., (1975). Modern pollen surface samples—An analysis of subsamples. Journal of Research of the U.S. Geological Survey, 3, 733736.Google Scholar
Anderson, R.S., Smith, S.J., (1994). Paleoclimatic interpretations of meadow sediment and pollen stratigraphies from California. Geology, 22, 723726.Google Scholar
Benson, L., (1993). Factors affecting 14C ages of lacustrine carbonates: Timing and duration of the last highstand lake in the Lahontan Basin. Quaternary Research, 39, 163174.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, 746749.Google Scholar
Benson, L., Burdett, J., Lund, S., Kashgarian, M., Mensing, S., (1997). Nearly synchronous climate change in the Northern Hemisphere during the last glacial termination. Nature, 388, 263265.Google Scholar
Benson, L.V., Lund, S.P., Burdett, J.W., Kashgarian, M., Rose, T.P., Smoot, J.P., 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
Benson, L. V, Lund, S. P, Smoot, J. P, Kashgarian, M, and Burdett, J. W. (in press), Records of climate change from the Owens Lake Basin, California. In, Proceedings of the Great Basin Symposium on Glacial and Postglacial Drainage, Smithsonian Institution, Washington, DC.Google Scholar
Billings, W.D., (1949). The shadscale vegetation zone of Nevada and Eastern California in relation to climate and soils. The American Midland Naturalist, 42, 87109.Google Scholar
Birks, H.J.B., Gordon, A.D., (1985). Numerical Methods in Quaternary Pollen Analysis. Academic Press, London.Google Scholar
Bright, R.C., (1966). Pollen and seed stratigraphy of Swan Lake, Southeastern Idaho. Tibewa, 2, 147.Google Scholar
Byrne, R.A., Busby, C.I., Heizer, R.F., (1979). The Altithermal revisited: Pollen evidence from the Leonard Rockshelter. Journal of California and Great Basin Anthropology, 1, 280294.Google Scholar
Dansgaard, W., Clausen, H., Gundestrup, N., Hammer, C., Johnsen, S., Kristensdottier., P, Reeh, N., (1982). A new Greenland deep ice core. Science, 218, 12731277.Google Scholar
Davis, O.K., (1995). Climate and vegetation patterns in surface samples from arid western USA: Application to Holocene climatic reconstructions. Palynology, 19, 95117.CrossRefGoogle Scholar
Davis, O.K., (1999). Pollen analysis of a late-glacial and Holocene sediment core from Mono Lake, Mono County, California. Quaternary Research, 52, 243249.CrossRefGoogle Scholar
Davis, O.K., Anderson, R.S., Fall, P.L., O'Rourke, M.K., Thompson, R.S., (1985). Palynological evidence for early Holocene aridity in the southern Sierra Nevada, California. Quaternary Research, 24, 222252.Google Scholar
Davis, O.K., Moratto, M.J., (1988). Evidence for a warm dry early Holocene in the western Sierra Nevada of California: Pollen and plant macrofossil analysis of Dinkey and Exchequer Meadows. Madroño, 35, 132149.Google Scholar
Eicher, U., Siegenthaler, U., Wegmuller, S., (1981). Pollen and isotope analysis on late and post-glacial sediments of the Tourbiere de Chirens (Dauphine, France). Quaternary Research, 15, 160170.Google Scholar
Engstrom, D.R., Hansen, B.C.S., Wright, H.E. Jr., (1990). A possible Younger Dryas record in southeastern Alaska. Science, 250, 13831385.Google Scholar
Faegri, K., Iversen, J., (1985). Textbook of Pollen Analysis. Hafner, New York.Google Scholar
Griffin, J. R, and Critchfield, W. B. (1972). The Distribution of Forest Trees in California. U.S. Dept. of Agriculture Forest Service Research Paper PSW-82, Washington, DC.Google Scholar
Grigg, L.D., Whitlock, C., (1998). Late-glacial vegetation and climate change in Western Oregon. Quaternary Research, 49, 287298.Google Scholar
Hickman, J.C., (1993). The Jepson Manual: Higher Plants of California.. Univ. of California Press, Berkeley.Google Scholar
Hollett, K. J, Danskin, W. R, McCaffrey, W. F, and Walti, C. L. (1991). Geology and Water Resources of Owens Valley, California.. USGS Water-Supply Paper 2370.Google Scholar
Jankovská, V., Komárek, J., (1982). Das vorkommen einiger chlorokokkalalgen in bohmischen spatglazial and postglazial. Folia Geobotanica et Phytotaxonomica, Praha, 17, 165195.Google Scholar
Jennings, S.A., Elliot-Fisk, D.L., (1993). Packrat midden evidence of late Quaternary vegetation change in the White Mountains, California–Nevada. Quaternary Research, 39, 214221.Google Scholar
Kapp, R.O., (1969). How to Know Pollen and Spores.. W.C. Brown Co, Dubuque.Google Scholar
Koehler, P.A., Anderson, R.S., (1995). Thirty thousand years of vegetation change in the Alabama Hills, Owens Valley, California. Quaternary Research, 43, 238248.Google Scholar
Lehman, S.J., Keigwin, L.D., (1992). Sudden changes in North Atlantic circulation during the last deglaciation. Nature, 356, 757762.Google Scholar
Lin, J.C., Broecker, W.S., Hemming, S.R., Hajdas, I., Anderson, R.F., Smith, G.I., Kelley, M., Bonani, G., (1998). A reassessment of U–Th and 14C ages for late-glacial high-frequency hydrological events at Searles Lake, California. Quaternary Research, 49, 1123.Google Scholar
Litwin, R.J., Adam, D.P., Frederiksen, N.O., Woolfenden, W.B., (1997). An 800,000-year pollen record from Owens Lake, California: Preliminary analyses.Smith, G.I., Bischoff, J.L. An 800,000-Year Paleoclimatic Record from Owens Lake, California, Geological Society of America, Boulder.127142.Google Scholar
Lund, D.C., Mix, A.C., (1998). Millennial-scale deep water oscillations: Reflections of the North Atlantic in the deep Pacific from 10 to 60 ka. Paleoceanography, 13, 1019.CrossRefGoogle Scholar
Mathewes, R.W., (1993). Evidence for Younger-Dryas-age cooling on the North Pacific coast of America. Quaternary Science Reviews, 12, 321331.Google Scholar
McCarten, N., VanDevender, T.R., (1988). Late Wisconsin vegetation of Robber's Roost in the Western Mojave Desert, California. Madroño, 35, 226237.Google Scholar
Mikolajewicz, U., Crowley, T.J., Schiller, A., Voss, R., (1997). Modelling teleconnections between the North Atlantic and North Pacific during the Younger Dryas. Nature, 387, 384387.Google Scholar
Moore, P.D., Webb, J.A., (1978). An Illustrated Guide to Pollen Analysis.. Wiley, New York.Google Scholar
Mozingo, H.N., (1987). Shrubs of the Great Basin. Univ. of Nevada Press, Reno.Google Scholar
Overpeck, J.T., Webb, T. III, Prentice, I.C., (1985). Quantitative interpretation of fossil pollen spectra: Dissimilarity coefficients and the method of modern analogs. Quaternary Research, 23, 87108.Google Scholar
Oviatt, C.G., (1997). Lake Bonneville fluctuations and global climate change. Geology, 25, 155158.Google Scholar
Oviatt, C.G., Currey, D.R., Sack, D., (1992). Radiocarbon chronology of Lake Bonneville, Eastern Great Basin, USA. Palaeogeography, Palaeoclimatology, Palaeoecology, 99, 225241.Google Scholar
Peltier, W.R., (1994). Ice age paleotopography. Science, 265, 195201.Google Scholar
Peteet, D., (1995). Global Younger Dryas?. Quaternary International, 28, 93104.CrossRefGoogle Scholar
Quade, J., Forester, R.M., Pratt, W.L., Carter, C., (1998). Black mats, spring-fed streams, and late-glacial-age recharge in the southern Great Basin. Quaternary Research, 49, 129148.Google Scholar
Rind, D., Peteet, D., Broecker, W., McIntyre, A., Ruddiman, W., (1986). The impact of cold North Atlantic sea surface temperatures on climate: Implications for the Younger Dryas cooling (11–10k). Climate Dynamics, 1, 333.Google Scholar
Ruddiman, W.F., McIntyre, A., (1981). The North Atlantic Ocean during the last glaciation. Palaeogeography, Palaeoclimatology, Palaeoecology, 35, 145214.Google Scholar
Solomon, A.M., Silkworth, A.B., (1986). Spatial patterns of atmospheric pollen transport in a montane region. Quaternary Research, 25, 150162.Google Scholar
Smith, S.J., Anderson, R.S., (1992). Late Wisconsin paleoecologic record from Swamp Lake, Yosemite National Park, California. Quaternary Research, 38, 91102.Google Scholar
Spaulding, W. G. (1985). Vegetation and Climate of the Last 45,000 Years in the Vicinity of the Nevada Test Site, South-Central Nevada.. USGS Professional Paper 1329.Google Scholar
Stockmarr, J., (1971). Tablets with spores used in absolute pollen analysis. Pollen et Spores, 13, 615621.Google Scholar
Stuiver, M., Grootes, P.M., Brasiunas, T.F., (1995). The GISP2 δ18O climate record of the past 16,500 years and the role of the sun, ocean, and volcanoes. Quaternary Research, 44, 341354.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C databases and revised CALIB radiocarbon calibration program. Radiocarbon, 28, 10221030.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., van der Plicht, J., Spurk, M., (1998). INTCAL98 Radiocarbon age calibration 24,000–0 cal B.P. Radiocarbon, 40, 10411083.Google Scholar
Stuiver, M., Reimer, P.J., Braziunas, T., (1998). High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon, 40, 11271151.CrossRefGoogle Scholar
Thompson, R.S., (1984). Late Pleistocene and Holocene Environments in the Great Basin. Univ. of Arizona, .Google Scholar
Thompson, R.S., (1988). Western North America—Vegetation dynamics in the western United States: Modes of response to climatic fluctuations.Huntley, B., Webb, T. III Vegetation History, Kluwer Academic, Dordrecht.415458.Google Scholar
Thompson, R.S., (1992). Late Quaternary environments in Ruby Valley, Nevada. Quaternary Research, 37, 115.Google Scholar
Wigand, P.E., (1987). Diamond Pond, Harney County, Oregon: Vegetation history and water table in the eastern Oregon desert. Great Basin Naturalist, 47, 427458.Google Scholar
Woolfenden, W.B., (1995). Fine resolution pollen analysis of Core OL-92, Owens Lake, California.Adam, D.P., Bradbury, J.P., Dean, W.E., Gardner, J.V., Sarna-Wojcicki, A.M. Report of 1994 Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western United States, U.S. Geological Survey, Menlo Park.Google Scholar