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Age and paleoclimatic significance of late Holocene lakes in the Carson Sink, NV, USA

Published online by Cambridge University Press:  20 January 2017

Kenneth D. Adams
Kenneth D. Adams*
Affiliation:
Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512
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Abstract

New dating in the Carson Sink at the termini of the Humboldt and Carson rivers in the Great Basin of the western United States indicates that lakes reached elevations of 1204 and 1198 m between 915 and 652 and between 1519 and 1308 cal yr B.P., respectively. These dates confirm Morrison's original interpretation (Lake Lahontan: Geology of the Southern Carson Desert, Professional Paper 40, U.S. Geol. Survey, 1964) that these shorelines are late Holocene features, rather than late Pleistocene as interpreted by later researchers. Paleohydrologic modeling suggests that discharge into the Carson Sink must have been increased by a factor of about four, and maintained for decades, to account for the 1204-m lake stand. The hydrologic effects of diversions of the Walker River to the Carson Sink were probably not sufficient, by themselves, to account for the late Holocene lake-level rises. The decadal-long period of increased runoff represented by the 1204-m lake is also reflected in other lake records and in tree ring records from the western United States.

Keywords

Lake LahontanGreat Basinlate HoloceneFallon Lakespaleoclimatology
Type
Research Article
Information
Quaternary Research , Volume 60 , Issue 3 , November 2003 , pp. 294 - 306
Copyright
University of Washington

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References

Adams, K.D., and Wesnousky, S.G., (1998). Shoreline processes and the age of the Lake Lahontan highstand in the Jessup embayment, Nevada. Geological Society of America Bulletin 110, 1318–1332.2.3.CO;2>CrossRefGoogle Scholar
Benson, L., Kashgarian, M., Rye, R., Lund, S., Paillet, F., Smoot, J., Kester, C., Mensing, S., Meko, D., and Lindstrom, S., (2002). Holocene multidecadal and multicentennial droughts affecting northern California and Nevada. Quaternary Science Review 21, 659–682.CrossRefGoogle Scholar
Benson, L.V., Currey, D.R., Lao, Y., and Hostetler, S.W., (1992). Lake-size variations in the Lahontan and Bonneville basins between 13,000 and 9000 (super 14) C yr B.P.. Palaeogeogr. Palaeoclimatol. Palaeoecol. 95, 19–32.CrossRefGoogle Scholar
Benson, L. V., Mifflin, M. D., (1986). Reconnaissance bathymetry of basins occupied by Pleistocene Lake Lahontan, Nevada and California. in: U.S. Geological Survey Water Resources Investigations Report 85–4262. p. 14 Google Scholar
Benson, L.V., and Paillet, F.L., (1989). The use of total lake-surface area as an indicator of climatic change. Examples from the Lahontan Basin. Quaternary Research 32, 262–275.CrossRefGoogle Scholar
Benson, L.V., and Thompson, R.S., (1987). The physical record of lakes in the Great Basin. Ruddiman, W.F., Wright, H.E. Jr. North America and Adjacent Oceans during the Last Deglaciation. Geological Society of America, Boulder, CO. 241–260.Google Scholar
Broecker, W.S., and Kaufman, A., (1965). Radiocarbon chronology of Lake Lahontan and Lake Bonneville; Part 2, Great Basin. Geological Society of America Bulletin 76, 537–566.CrossRefGoogle Scholar
Cayan, D.R., Redmond, K.T., and Riddle, L.G., (1999). ENSO and hydrologic extremes in the western United States. Journal of Climate 12, 2881–2893.2.0.CO;2>CrossRefGoogle Scholar
Currey, D. R., (1988). Isochronism of final Pleistocene shallow lakes in the Great Salt Lake and Carson Desert regions of the Great Basin. in: Program and Abstracts of the Tenth Biennial Meeting, American Quaternary Association, . p. 117 Google Scholar
Currey, D.R., (1990). Quaternary palaeolakes in the evolution of semidesert basins, with special emphasis on Lake Bonneville and the Great Basin, U.S.A.. Palaeogeography, Palaeoclimatology, Palaeoecology 76, 189–214.CrossRefGoogle Scholar
Davis, J. O., (1978). Quaternary Tephrochronology of the Lake Lahontan Area, Nevada and California. Nevada Archeological Survey Research Paper 7. University of Nevada, Google Scholar
Davis, J. O., (1982). Bits and pieces: The last 35,000 years in the Lahontan basin. in: Madsen, D. B., O'Connell, J. F. (Eds.), Man and Environment in the Great Basin, Society of American Archeology Papers No. 2. Pp. 53–75.Google Scholar
Davis, J.O., (1983). Geology of Gatecliff shelter. Sedimentary facies and Holocene climate. Thomas, D.H. The Archaeology of Monitor Valley 2. Gatecliff Shelter. Anthropological Papers of the American Museum of Natural History, New York. 64–87.Google Scholar
Dugas, D.P., (1998). Late Quaternary variations in the level of pales-Lake Malheur, eastern Oregon. Quaternary Research 50, 276–282.CrossRefGoogle Scholar
Enzel, Y., Cayan, D.R., Anderson, R.Y., and Wells, S.G., (1989). Atmospheric circulation during Holocene lake stands in the Mojave Desert. Evidence of regional climate change. Nature 341, 44–47.CrossRefGoogle Scholar
Graumlich, L.J., (1993). A 1000-year record of temperature and precipitation in the Sierra Nevada. Quaternary Research 39, 249–255.CrossRefGoogle Scholar
Grayson, D.K., (1993). The desert's past. A natural prehistory of the Great Basin. Smithsonian Institution Press, Washington, D.C.Google Scholar
Kelly, R.L., (2001). Prehistory of the Carson Desert and Stillwater Mountains. Environment, Mobility, and Subsistence in a Great Basin wetland, Anthropological Papers, Number 123. University of Utah, Salt Lake City.Google Scholar
King, G.Q., (1993). Late Quaternary history of the lower Walker River and its implications for the Lahontan paleolake system. Physical Geography 14, 81–96.CrossRefGoogle Scholar
Lancaster, N., (1995). Geomorphology of Desert Dunes. Routledge, New York.Google Scholar
Leavitt, S.W., (1994). Major wet interval in White Mountains Medieval Warm Period evidenced in δ13C of Bristlecone Pine tree rings. Climatic Change 26, 299–307.CrossRefGoogle Scholar
Meko, D. M., Baisan, C. H., Hughes, M. K., (1999). Climatic inferences from a 1200-year tree ring reconstruction of Sacramento River flow. in: Wilson, R., Buffaloe, L. (Eds.), Proceedings of the Fifteenth Annual Pacific Climate (PACLIM) Workshop, Technical Report 64, Interagency Ecological Program for the Sacramento–San Joaquin Estuary, p. 122 Google Scholar
Meko, D.M., Therrell, M.D., Baisan, C.H., and Hughes, M.K., (2001). Sacramento river flow reconstructed to AD 869 from tree rings. Journal of the American Water Resources Association 37, 1029–1039.CrossRefGoogle Scholar
Mifflin, M.D., and Wheat, M.M., (1979). Pluvial lakes and estimated pluvial climates of Nevada, Bulletin 94. Nevada Bureau of Mines and Geology, Reno, NV.Google Scholar
Miller, C.D., (1985). Holocene eruptions at the Inyo volcanic chain. Implications for possible eruptions in Long Valley Caldera. Geology 13, 14–17.2.0.CO;2>CrossRefGoogle Scholar
Milne, W., (1987). A Comparison of Reconstructed Lake-Level Records since the Mid-1880's of Some Great Basin Lakes. Unpublished M.S. thesis, Colorado School of Mines, Google Scholar
Morrison, R. B., (1964). Lake Lahontan: Geology of the Southern Carson Desert. Professional Paper 401. United States Geological Survey, CrossRefGoogle Scholar
Morrison, R.B., (1991). Quaternary geology of the southern Basin and Range Province. Morrison, R.B. Quaternary nonglacial geology; conterminous U.S.. Geological Society of America, Boulder, CO. 353–371.Google Scholar
Redmond, K.T., and Koch, R.W., (1991). Surface climate and streamflow variability in the western United States and their relationship to large-scale circulation indices. Water Resources Research 29, 2381–2399.CrossRefGoogle Scholar
Rhode, D., (2003). Coprolites from Hidden Cave, revisited. Evidence for site occupation history, diet, and sex of occupants. Journal of Archaeological Science 30, 909–922.CrossRefGoogle Scholar
Rhode, D., Adams, K.D., and Elston, R.G., (2000). Geoarchaeology and Holocene landscape history of the Carson Desert, western Nevada. Lageson, D.R., Peters, S.G., and Lahren, M.M. Great Basin and Sierra Nevada. Geological Society of America Field Guide 2, Boulder, CO. 45–74.Google Scholar
Russell, I. C., (1885). Geological History of Lake Lahontan, a Quaternary Lake in Northwestern Nevada, Monograph 11. United States Geological Survey, Google Scholar
Sarna-Wojcicki, A.M., Lajoie, K.R., Meyer, C.E., Adam, D.P., and Rieck, H.J., (1991). Tephrochronologic correlation of upper Neogene sediments along the Pacific margin, conterminous United States. Morrison, R.B. Quaternary Nonglacial Geology. Conterminous U.S. Geological Society of America, Boulder, CO. 117–140.Google Scholar
Sieh, K., and Bursik, M., (1986). Most recent eruption of the Mono Craters, eastern central California. Journal of Geophysical Research 91, 12539–12571.CrossRefGoogle Scholar
Stine, S., (1990). Late Holocene fluctuations of Mono Lake, California. Palaeogeography, Palaeoclimatology, Palaeoecology 78, 333–381.CrossRefGoogle Scholar
Stine, S., (1994). Extreme and persistent drought in California and Patogonia during mediaeval time. Nature 369, 546–549.CrossRefGoogle Scholar
Stuiver, M., and Reimer, P.J., (1993). Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, 215–230.CrossRefGoogle Scholar
Wood, S.H., (1977). Distribution, correlation, and radiocarbon dating of late Holocene tephra, Mono and Inyo craters, eastern California. Geological Society of America Bulletin 88, 89–95.2.0.CO;2>CrossRefGoogle Scholar