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Terminal Pleistocene/Early Holocene Environmental Change at the Sunshine Locality, North-Central Nevada, U.S.A.

Published online by Cambridge University Press:  20 January 2017

Gary Huckleberry ,
Charlotte Beck ,
George T. Jones ,
Amy Holmes ,
Michael Cannon ,
Stephanie Livingston  and
Jack M. Broughton
Gary Huckleberry
Affiliation:
Department of Anthropology, Washington State University, Pullman, Washington
Charlotte Beck
Affiliation:
Department of Anthropology, Hamilton College, Clinton, New York
George T. Jones
Affiliation:
Department of Anthropology, Hamilton College, Clinton, New York
Amy Holmes
Affiliation:
Department of Anthropology, Washington State University, Pullman, Washington
Michael Cannon
Affiliation:
Department of Anthropology, University of Washington, Seattle, Washington
Stephanie Livingston
Affiliation:
Desert Research, Inc. and Department of Anthropology, University of Nevada-Reno, Reno, Nevada
Jack M. Broughton
Affiliation:
Department of Anthropology, University of Utah, Salt Lake City, Utah
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Abstract

Sedimentological, faunal, and archaeological investigations at the Sunshine Locality, Long Valley, Nevada reveal a history of human adaptation and environmental change at the last glacial–interglacial transition in North America's north-central Great Basin. The locality contains a suite of lacustrine, alluvial, and eolian deposits associated with fluvially reworked faunal remains and Paleoindian artifacts. Radiocarbon-dated stratigraphy indicates a history of receding pluvial lake levels followed by alluvial downcutting and subsequent valley filling with marsh-like conditions at the end of the Pleistocene. A period of alluvial deposition and shallow water tables (9,800 to 11,000 14C yr B.P.) correlates to the Younger Dryas. Subsequent drier conditions and reduced surface runoff mark the early Holocene; sand dunes replace wetlands by 8,000 14C yr B.P. The stratigraphy at Sunshine is similar to sites located 400 km south and supports regional climatic synchroneity in the central and southern Great Basin during the terminal Pleistocene/early Holocene. Given regional climate change and recurrent geomorphic settings comparable to Sunshine, we believe that there is a high potential for buried Paleoindian features in primary association with extinct fauna elsewhere in the region yet to be discovered due to limited stratigraphic exposure and consequent low visibility.

Keywords

stratigraphyfaunaPaleoindianYounger DryasGreat Basin
Type
Research Article
Information
Quaternary Research , Volume 55 , Issue 3 , May 2001 , pp. 303 - 312
Copyright
University of Washington

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References

Antevs, E., (1948). Climatic changes and pre-white man.. The Great Basin with Emphasis on Glacial and Postglacial Time.. University of Utah Bulletin, Salt Lake City.p. 168–191.Google Scholar
Beck, C., Jones, G.T., (1997). The terminal Pleistocene/early Holocene archaeology of the Great Basin.. Journal of World Prehistory, 11, 161–236.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, 263–265.Google Scholar
Benson, L.V., Thompson, R.S., (1987). Lake-level variation in the Lahontan Basin for the past 50,000 years.. Quaternary Research, 28, 69–85.Google Scholar
Broecker, W., (1994). Massive iceberg discharges as triggers for global climate change.. Nature, 372, 421–424.Google Scholar
Clark, P.U., Bartlein, P.J., (1995). Correlation of the Pleistocene glaciation in the western United States with Atlantic Heinrich events.. Geology, 23, 483–486.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
Dansie, A. J., (1990)., Taphonomy and Taxonomy of Large and Small Fauna from the Sunshine Wells Locality.. Paper presented at the 22nd biennial, Great Basin Anthropological Conference, Reno, NV.Google Scholar
Denton, G.H., Hendy, C.H., (1994). Younger Dryas age advance of Franz Josef Glacier in the Southern Alps of New Zealand.. Science, 264, 1434–1437.Google Scholar
Grayson, D.K., (1993). The Desert's Past: A Natural Prehistory of the Great Basin.. Smithsonian Institution Press, Washington.Google Scholar
Grayson, D.K., Livingston, S.D., Rickart, E., Shaver, M.W. III., (1996). Biogeographic significance of low-elevation records for Neotoma cinerea from the northern Bonneville Basin, Utah.. The Great Basin Naturalist, 56, 191–196.Google Scholar
Hall, E.R., (1946). Mammals of Nevada.. University of Nevada Press, Reno.Google Scholar
Harden, J.W., Taylor, E.M., McFadden, L.D., Reheis, M.C., (1991). Calcic, gypsic, and siliceous soil chronosequences in arid and semiarid environments.. Nettleton, W.D., Occurrence, Characteristics, and Genesis of Carbonate, gypsum, and Silica Accumulations in Soils, 1–16.Google Scholar
Haynes, C.V. Jr., (1967). Quaternary geology of the Tule Springs area, Clark County, Nevada.. Wormington, M., Ellis, D., Pleistocene Studies in Southern Nevada, 15–104.Google Scholar
Hicks, P., (1990)., Lithics from the Sunshine Wells Geological Test Trenches.. Paper presented at the 22nd biennial Great Basin Anthropological Conference, Reno, NV.Google Scholar
Holmes, A.M., (1998). Geoarchaeology and Paleoenvironments of the Sunshine Locality, East-Central Nevada.. Washington State UniversityDepartment of Anthropology, Pullman.Google Scholar
Huckleberry, G.A., Beck, C., Jones, G.T., Holmes, A., (1997). Further excavations and paleoenvironmental data at the Sunshine Locality, eastern Nevada.. Current Research in the Pleistocene, 14, 162–163.Google Scholar
Hutchinson, P. W., (1988). . The prehistoric dwellers at Lake Hubbs.. In Early Human Occupation in Far Western North America: The Clovis–Archaic Interface, Willig, J. A., Aikens, C. M., and Fagan, J. L., Eds., pp. 303–318., Nevada State Museum Anthropological Papers No. 21, .Google Scholar
Jones, G.T., Beck, C., Nials, F.L., Neudorfer, J.J., Brownholtz, B.J., Gilbert, H.B., (1996). Recent archaeological and geological investigations at the Sunshine Locality, Long Valley, Nevada.. Journal of California and Great Basin Anthropology, 18, 48–63.Google Scholar
Keeling, C.D., Whorf, T.P., (2000). The 1,800-year oceanic tidal cycle: A possible cause of rapid climate change.. Proceedings of the National Academy of Sciences, U.S.A., 97, 3814–3819.CrossRefGoogle ScholarPubMed
Kutzbach, J.E., Guetter, P.J., (1986). The influence of changing orbital parameters and surface boundary conditions on climatic simulations for the past 18,000 years.. Journal of Atomospheric Science, 43, 1726–1759.Google Scholar
Madsen, D.B., (2000). Late Quaternary Paleoecology in the Bonneville Basin.. Utah Geological Survey Bulletin 130, Salt Lake City.Google Scholar
Malde, H.D., (1968). The Catastrophic Late Pleistocene Bonneville Flood in the Snake River Plain Idaho.. U.S. Government Printing Office, Washington.Google Scholar
Mehringer, P.J. Jr., (1986). Prehistoric environments.. D'Azevedo, W.L., Handbook of North American Indians Volume 11: The Great Basin, Smithsonian Institution, Washington.31–50.Google Scholar
Mifflin, M.D., Wheat, M.M., (1979). Pluvial Lakes and Estimated Pluvial Climates of Nevada.. Nevada Bureau of Mines and Geology Bulletin 94, Carson City.Google Scholar
Morrison, R., (1991). Quaternary stratigraphic, hydrologic, and climatic history of the Great Basin, with emphasis on Lakes Lahontan, Bonneville, and Tecopa.. Morrison, R.B., Quaternary Nonglacial Geology; Conterminous United States, Geological Society of America, Boulder.283–320.Google Scholar
Nials, F, and Davis, J. O., (1990)., Late Quaternary Stratigraphy and Depositional Environments of the Sunshine Wells Locality.. Paper presented at the 22nd biennial Great Basin Anthropological Conference, Reno, NV.Google Scholar
Oviatt, C.G., Geology, 25, (1997). 155–158.Google Scholar
Quade, J., Quaternary Research, 26, (1986). 340–357.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, 129–148.Google Scholar
Rhode, D., (2000). Middle and late Wisconsin vegetation in the Bonneville Basin.. Madsen, D., Late Quaternary Paleoecology in the Bonneville Basin, Utah Geological Survey Bulletin 130, Salt Lake City.137–148.Google Scholar
Rhode, D., (2000). Holocene vegetation history in the Bonneville Basin.. Madsen, D., Late Quaternary Paleoecology in the Bonneville Basin, Utah Geological Survey Bulletin 130, Salt Lake City.149–164.Google Scholar
Scott, W.E., Pierce, K.L., Bradbury, J.P., Forester, R.M., (1982). Revised Quaternary stratigraphy and chronology in the American Falls area, southeastern Idaho.. Bonichsen, B., Brackenridge, R.M., Cenozoic Geology of Idaho, Idaho Bureau of Mines and Geology Bulletin 26, Moscow.581–595.Google Scholar
Severinghaus, J.P., Sowers, T., Brook, E.J., Alley, R.B., Bender, M.L., (1998). Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice.. Nature, 391, 141–146.Google Scholar
Spaulding, W.G., Graumlich, L.J., (1986). The last pluvial climatic episodes in the deserts of southwestern North America.. Nature, 320, 441–444.Google Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C data base and revised Calib 3.0 14C age calibration program.. Radiocarbon, 35, 215–230.Google Scholar
Tadlock, W.L., (1966). Certain crescentic stone objects as a time marker in the western United States.. American Antiquity, 31, 662–675.Google Scholar
Taylor, K., (1999). Rapid climate change.. American Scientist, 87, 320–327.Google Scholar
Thompson, R.S., (1992). Late Quaternary environments in Ruby Valley, Nevada.. Quaternary Research, 37, 1–15.Google Scholar
Thompson, R.S., Benson, L., Hattori, E.M., (1986). A revised chronology for the last Pleistocene lake cycle in the central Lahontan Basin.. Quaternary Research, 25, 1–9.CrossRefGoogle Scholar
Thompson, R.S., Whitlock, C., Bartlein, P.J., Harrison, S.P., Spaulding, W.G., (1993). Climatic changes in the western United States since 18,000 yr B. P.. Wright, H.E. Jr., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J., Global Climates Since the Last Glacial Maximum, University of Minnesota Press, Minneapolis.468–513.Google Scholar
York, R., (1974)., Test Excavations and Controlled Surface Collecting in Long Valley, Nevada.. Report on file at the, Nevada State Museum, Carson City.Google Scholar
Young, M. A, and McCoy, W. D., (1984)., Late Quaternary histories of Long, Ruby, and Jakes Valleys, Nevada.. Abstracts of the Eight Biennial Meeting of the American Quaternary Association, p, 143.Google Scholar