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Quaternary eolian dunes in the Savannah River Valley, Jasper County, South Carolina, USA

Published online by Cambridge University Press:  20 January 2017

Christopher S. Swezey ,
Arthur P. Schultz ,
Wilma Alemán González ,
Christopher E. Bernhardt ,
William R. Doar III ,
Christopher P. Garrity ,
Shannon A. Mahan  and
John P. McGeehin
Christopher S. Swezey*
Affiliation:
U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 926A, Reston, VA 20192, USA
Arthur P. Schultz
Affiliation:
U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 926A, Reston, VA 20192, USA
Wilma Alemán González
Affiliation:
U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 926A, Reston, VA 20192, USA
Christopher E. Bernhardt
Affiliation:
U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 926A, Reston, VA 20192, USA
William R. Doar III
Affiliation:
South Carolina Geological Survey, 5 Geology Road, Columbia, SC 29212, USA
Christopher P. Garrity
Affiliation:
U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 956, Reston, VA 20192, USA
Shannon A. Mahan
Affiliation:
U.S. Geological Survey, Box 25046, Denver Federal Center, MS 974, Denver, CO 80225, USA
John P. McGeehin
Affiliation:
U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 926A, Reston, VA 20192, USA
*
*Corresponding author. Fax: + 1 703 648 6953. E-mail address:cswezey@usgs.gov (C.S. Swezey).
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Abstract

Sand hills in the Savannah River valley in Jasper County (South Carolina, USA) are interpreted as the remnants of parabolic eolian dunes composed of sand derived from the Savannah River and stabilized by vegetation under prevailing climate conditions. Optically stimulated luminescence ages reveal that most of the dunes were active ca. 40 to 19 ka ago, coincident with the last glacial maximum (LGM) through early deglaciation. Modern surface winds are not sufficient for sustained eolian sand transport. When the dunes were active, winds blew at velocities of at least 4 m/s from west to east, and some vegetation was present. The ratio of annual precipitation to potential evapotranspiration (P:PE) was less than the modern ratio of 1.23 and may have been < 0.30, caused by stronger winds (which would have resulted in greater evaporation) and/or reduced precipitation. The Savannah River dunes are part of a larger assemblage of eolian dunes that were active in the eastern United States during and immediately after the LGM, suggesting that eolian sediment behavior in this region has been controlled by regional forcing mechanisms during the Quaternary.

Keywords

EolianDuneQuaternarySouth Carolina
Type
Original Articles
Information
Quaternary Research , Volume 80 , Issue 2 , September 2013 , pp. 250 - 264
Copyright
University of Washington

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References

Alley, R., Messe, D., Shuman, C., Gow, A., Taylor, K., Grootes, P., White, J., Ram, M., Waddington, E., Mayewski, P., Zielinski, G., (1993). Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. Nature 362, 527–529.Google Scholar
Ash, J.E., Wasson, R.J., (1983). Vegetation and sand mobility in the Australian desert dunefield. Zeitschrift für Geomorphologie Supplementband 45, 7–25.Google Scholar
Baldwin, J.L., (1975). Weather Atlas of the United States. Gale Research Company, Detroit, MI.(262 pp.).Google Scholar
Bartlein, P.J., Anderson, K.H., Anderson, P.M., Edwards, M.E., Mock, C.J., Thompson, R.S., Webb III, T., Whitlock, C., (1998). Paleoclimate simulations for North America over the past 21,000 years: features of the simulated climate and comparisons with paleoenvironmental data. Quaternary Science Reviews 17, 549–585.CrossRefGoogle Scholar
Bateman, M.D., Boulter, C.H., Carr, A.S., Frederick, C.D., Peter, D., Wilder, M., (2007a). Detecting post-depositional sediment disturbance in sandy deposits using optical luminescence. Quaternary Geochronology 2, 57–64.Google Scholar
Bateman, M.D., Boulter, C.H., Carr, A.S., Frederick, C.D., Peter, D., Wilder, M., (2007b). Preserving the palaeoenvironmental record in drylands: bioturbation and its significance for luminescence-derived chronologies. Sedimentary Geology 195, 5–19.Google Scholar
Bernhardt, C., Swezey, C.S., Schultz, A.P., (2012). Palynological studies reveal Holocene climate changes in a forested flood plain wetland, Savannah River valley, South Carolina (USA). Geological Society of America, Abstracts with Programs .Google Scholar
Bradley, R.S., Diaz, H.F., Kiladis, G.N., Eischeild, J.K., (1987). ENSO signal in continental temperature and precipitation records. Nature 327, 497–501.CrossRefGoogle Scholar
Bush, A.B.G., (2007). Extratropical influences on the El NiñoñSouthern Oscillation through the Late Quaternary. Journal of Climate 20, 788–800.Google Scholar
Carver, R.E., Brook, G.A., (1989). Late Pleistocene paleowind directions, Atlantic coastal plain, U.S.A.. Palaeogeography, Palaeoclimatology, Palaeoecology 74, 205–216.CrossRefGoogle Scholar
Christensen, N.L., (2000). Vegetation of the southeastern coastal plain. Barbour, M.G., Billings, W.D. North American Terrestrial Vegetation. second ed. Cambridge University Press, Cambridge.397–448.Google Scholar
Clark, P.U., Dyke, A.S., Shakun, J.D., Carlson, A.E., Clark, J., Wohlfarth, B., Mitrovica, J.X., Hostetler, S.W., McCabe, A.M., (2009). The last glacial maximum. Science 325, 710–714.Google Scholar
COHMAP Members, (1988). Climate changes of the last 18,000 years: observations and model simulations. Science 241, 1043–1052.Google Scholar
Court, A., (1974). The climate of the conterminous United States. Bryson, R.A., Kare, F.K. Climates of North America. Elsevier, Amsterdam.193–343.Google Scholar
Daniels, R.B., Gamble, E.E., Boul, S.W., (1969). Eolian sands associated with coastal plain river valleys—some problems in their age and source. Southeastern Geology 11, 97–110.Google Scholar
Davis, R.E., Hayden, B.P., Gay, D.A., Phillips, W.L., Jones, G.V., (1997). The North Atlantic subtropical anticyclone. Journal of Climate 10, 728–744.Google Scholar
Delcourt, P.A., Delcourt, H.R., (1984). Late-Quaternary paleoclimates and biotic responses in eastern North America and the western North Atlantic Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology 48, 263–284.Google Scholar
Delcourt, H.R., Delcourt, P.A., (1985). Quaternary palynology and vegetational history of the southeastern United States. Bryant jr., V.M., Holloway, R.G. Pollen Records of Late-Quaternary North American Sediments. American Association of Stratigraphic Palynologists Foundation, Dallas, TX.1–37.Google Scholar
Denny, C.S., Owens, J.P., (1979). Sand dunes on the central Delmarva Peninsula, Maryland and Delaware. U.S. Geological Survey 1067-C, 15p(Professional Paper).Google Scholar
Denny, C.S., Owens, J.P., Sirkin, L.A., Rubin, M., (1979). The Parsonsburg Sand in the central Delmarva Peninsula, Maryland and Delaware. U.S. Geological Survey Professional Paper 1067-B, 16p.Google Scholar
Dracup, J.A., Kahya, E., (1994). The relationships between U.S. streamflow and La Niña events. Water Resources Research 30, 2133–2141.Google Scholar
Enfield, D.B., Mestas-Nu"ez, A.M., Trimble, P.J., (2001). The Atlantic multidecadal oscillation and its relation to rainfall and river flows in the continental U.S.. Geophysical Research Letters 28, 2077–2080.Google Scholar
Forman, S.L., Oglesby, R., Markgraf, V., Stafford, T., (1995). Paleoclimatic significance of Late Quaternary eolian deposition on the Piedmont and High Plains, central United States. Global and Planetary Change 11, 35–55.Google Scholar
Foss, J.E., Fanning, D.S., Miller, F.P., Wagner, D.P., (1978). Loess deposits of the Eastern Shore of Maryland. Soil Science Society of America 42, 329–334.CrossRefGoogle Scholar
Galbraith, R.F., Laslett, G.M., (1993). Statistical models for mixed fission track ages. Nuclear Tracks and Radiation Measurements 21, 459–470.Google Scholar
Galbraith, R.F., Roberts, R.G., Laslett, G.M., Yoshida, H., Olley, J.M., (1999). Optical dating of single and multiple grains of quartz from Jinmium rock shelter, northern Australia: Part I Experimental design and statistical models. Archaeometry 41, 339–364.Google Scholar
Hack, J.T., (1955). Geology of the Brandywine area and origin of the upland of southern Maryland. U.S. Geological Survey Professional Paper 267-A, 42p.Google Scholar
Hsu, S.A., (1974). Computing eolian sand transport from routine weather data. Proceedings of the 14th Coastal Engineering Conference (24"28 June 1974). 2, Copenhagen, Denmark.1619–1626.Google Scholar
Huddlestun, P.F., (1988). A revision to the lithostratigraphic units of the coastal plain of Georgia-the Miocene through Holocene. Georgia Geological Survey Bulletin 104, 162p.Google Scholar
Hugenholtz, C.H., (2010). Topographic changes of a supply-limited inland parabolic sand dune during the incipient phase of stabilization. Earth Surface Processes and Landforms 35, 1674–1681.Google Scholar
Hugenholtz, C.H., Wolfe, S.A., Moorman, B.J., (2008). Effects of sand supply on the morphodynamics and stratigraphy of active parabolic dunes, Bigstick Sand Hills, southwestern Saskatchewan. Canadian Journal of Earth Sciences 45, 321–335.CrossRefGoogle Scholar
Ivester, A.H., Leigh, D.S., (2003). Riverine dunes on the coastal plain of Georgia, USA. Geomorphology 51, 289–311.Google Scholar
Ivester, A.H., Leigh, D.S., Godfrey-Smith, D.I., (2001). Chronology of inland eolian dunes on the coastal plain of Georgia. Quaternary Research 55, 293–302.Google Scholar
Johnson jr., H.S., (1961). Fall line stratigraphy northeast of Columbia, S. C. South Carolina Division of Geology. Geologic Notes 5, 81–87.Google Scholar
Katz, R.W., Parlange, M.B., Tebaldi, C., (2003). Stochastic modeling of the effects of large-scale circulation on daily weather in the southeastern U.S.. Climatic Change 60, 189–216.Google Scholar
King, P.D., Beikman, H.M., (1974). United States Geological Survey geologic map of the United States (exclusive of Alaska and Hawaii). U.S. Geological Survey scale 1:2,500,000 (2 sheets).Google Scholar
Kocurek, G., Lancaster, N., (1999). Aeolian system sediment state: theory and Mojave Desert Kelso dune field example. Sedimentology 46, 505–515.Google Scholar
Kushnir, Y., Seager, R., Ting, M., Naik, N., Nakamura, J., (2010). Mechanisms of tropical SST influence on North American precipitation variability. Journal of Climate 23, 5610–5628.Google Scholar
Kutzbach, J.E., Guetter, P.J., Behling, P.J., Selin, R., (1993). Simulated climatic changes: results from the COHMAP climate-model experiments. Wright jr., J.E., Kutzbach, J.E., Webb III, T., Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J. Global Climates since the Last Glacial Maximum. University of Minnesota Press, Minneapolis, MN.24–93.Google Scholar
Kutzbach, J., Gallimore, R., Harrison, S., Behling, P., Selin, R., Laarif, F., (1998). Climate and biome simulations for the past 21,000 years. Quaternary Science Reviews 17, 473–506.Google Scholar
LaMoreaux, H.K., Brook, G.A., Knox, J.A., (2009). Late Pleistocene and Holocene environments of the southeastern United States from the stratigraphy and pollen content of a peat deposit on the Georgia Coastal Plain. Palaeogeography, Palaeoclimatology, Palaeoecology 280, 300–312.Google Scholar
Lancaster, N., (1995). Geomorphology of Desert Dunes. Routledge, London.(290 pp.).Google Scholar
Lancaster, N., Baas, A., (1998). Influence of vegetation cover on sand transport by wind: field studies at Owens Lake, California. Earth Surface Processes and Landforms 23, 69–82.Google Scholar
Leigh, D.S., (2008). Late Quaternary climates and river channels of the Atlantic coastal plain, southeastern USA. Geomorphology 101, 90–108.Google Scholar
Leigh, D.S., Srivastava, P., Brook, G.A., (2004). Late Pleistocene braided rivers of the Atlantic coastal plain, USA. Quaternary Science Reviews 23, 65–84.CrossRefGoogle Scholar
Mahan, S.A., Miller, D.M., Menges, C.M., Yount, J.C., (2007). Late Quaternary stratigraphy and luminescence geochronology of the northeastern Mojave Desert. Quaternary International 166, 61–78.Google Scholar
Makou, M.C., Eglinton, T.I., Oppo, D.W., Hughen, K.A., (2010). Postglacial changes in El Niño and La Niña behavior. Geology 38, 36–43.Google Scholar
Markewich, H.W., Markewich, W., (1994). An overview of Pleistocene and Holocene inland dunes in Georgia and the Carolinas—morphology, distribution, age, and paleoclimate. U.S. Geological Survey Bulletin 2069, 32p.Google Scholar
Markewich, H.W., Litwin, R.J., Pavich, M.J., Brook, G.A., (2009). Late Pleistocene eolian features in southeastern Maryland and Chesapeake Bay region indicate strong WNS-NW winds accompanied growth of the Laurentide Ice Sheet. Quaternary Research 71, 409–425.CrossRefGoogle Scholar
McCabe, G.J., Palecki, M.A., Betancourt, J.L., (2004). Pacific and Atlantic Ocean influences on multidecadal drought frequency in the United States. Proceedings of the National Academy of Sciences 101, 4136–4141.CrossRefGoogle ScholarPubMed
McGee, W.J., (1890). The southern extension of the Appomattox Formation. American Journal of Science 40, 15–41.(3rd series).Google Scholar
McGee, W.J., (1891). The Lafayette Formation. 12th Annual Report of the United States Geological Survey to the Secretary of the Interior 1890–91. 347–521.Google Scholar
McKee, E.D., Bigarella, J.J., (1979). Sedimentary structures in dunes. McKee, , A Study of Global Sand Seas. U.S. Geological Survey Professional Paper 1052, 83–134.Google Scholar
Melton, F.A., (1940). A tentative classification of sand dunes, its application to dune history in the southern high plains. Journal of Geology 48, 113–145.Google Scholar
Miller III, W., (1979). Stratigraphic framework of the Wharton Station dune field, easternmost Beaufort County, North Carolina. Southeastern Geology 20, 261–273.Google Scholar
Muhs, D.R., Holliday, V.T., (1995). Evidence of active dune sand on the Great Plains in the 19th Century from accounts of early explorers. Quaternary Research 43, 198–208.Google Scholar
Murray, A.S., Wintle, A.G., (2000). Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32, 57–73.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., (2003). The single aliquot regenerative dose protocol: potential for improvements in reliability. Radiation Measurements 37, 377–381.Google Scholar
Murray, A.S., Marten, R., Johnston, A., Martin, P., (1987). Analysis for naturally occurring radionuclides at environmental concentrations by gamma spectrometry. Journal of Radioanalytical and Nuclear Chemistry 115, 263–288.Google Scholar
Oglesby, R.J., (1991). Springtime soil moisture, natural climate variability, and North American drought as simulated by the NCAR Community Climate Model 1. Journal of Climate 4, 890–897.Google Scholar
Oglesby, R.J., Maasch, K.A., Saltzman, B., (1989). Glacial meltwater cooling of the Gulf of Mexico: GCM implications for Holocene and present-day climates. Climate Dynamics 3, 115–133.Google Scholar
Pickering, S.M., Jones, R.C., (1974). Morphology of aeolian parabolic sand features along streams in southeast Georgia. Geological Society of America Abstracts with Programs 6, 4 387–388.Google Scholar
Piechota, T.C., Dracup, J.A., (1996). Drought and regional hydrologic variation in the United States: associations with the El Niño–Southern Oscillation. Water Resources Research 32, 1359–1373.Google Scholar
Prescott, J.R., Hutton, J.T., (1994). Cosmic ray contribution to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements 23, 497–500.Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., Buck, C.E., Burr, G.S., Edwards, R.L., Friedrich, M., Grootes, P.M., Guilderson, T.P., Hajdas, I., Heaton, T.J., Hogg, A.G., Hughen, K.A., Kaiser, K.F., Kromer, B., McCormac, F.G., Manning, S.W., Reimer, R.W., Richards, D.A., Southon, J.R., Talamo, S., Turney, C.S.M., van der Plicht, J., Weyhenmeyer, C.E., (2009). IntCal09 and Marine09 radiocarbon age calibration curves, 0-50,000 years cal BP. Radiocarbon 51, 1111–1150.Google Scholar
Rittenour, T.M., Brigham-Grette, J., Mann, M.E., (2000). El Niño-like climate teleconnections in New England during the Late Pleistocene. Science 288, 1039–1042.CrossRefGoogle ScholarPubMed
Ropelewski, C.F., Halpert, M.S., (1986). North American precipitation and temperature patterns associated with the El Niño/Southern Oscillation (ENSO). Monthly Weather Review 114, 2352–2362.Google Scholar
Sahsamanoglou, H.S., (1990). A contribution to the study of action centres in the North Atlantic. International Journal of Climatology 10, 247–261.Google Scholar
Soller, D.R., (1988). Geology and tectonic history of the lower Cape Fear River valley, southeastern North Carolina. U.S. Geological Survey Professional Paper 1466-A, 60p.Google Scholar
Stahle, D.W., Cleaveland, M.K., (1992). Reconstruction and analysis of spring rainfall over the southeastern U.S. for the past 1000 years. Bulletin of the American Meteorological Society 73, 1947–1961.Google Scholar
Street, F.A., Grove, A.T., (1979). Global maps of lake-level fluctuations since 30,000 yr B.P.. Quaternary Research 12, 83–118.Google Scholar
Stuck, W.M., (1980). Soil survey of Beaufort and Jasper Counties, South Carolina. U.S. Department of Agriculture Soil Conservation Service, Washington, DC.(179 pp.).Google Scholar
Stuiver, M., Polach, H.A., (1977). Reporting of 14C data. Radiocarbon 19, 355–363.Google Scholar
Stuiver, M., Reimer, P., (1993). Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35, 215–230.Google Scholar
Swezey, C.S., (2003). The role of climate in the creation and destruction of continental stratigraphic records: an example from the northern margin of the Sahara Desert. Cecil, C.B., Edgar, N.T. Climate Controls on Stratigraphy. SEPM Special Publication 77, 207–225.Google Scholar
Thom, B.G., (1970). Carolina Bays in Horry and Marion Counties, South Carolina. Geological Society of America Bulletin 81, 783–814.Google Scholar
Thompson, C.H., (1983). Development and weathering of large parabolic dune systems along the subtropical coast of eastern Australia. Zeitschrift f"r Geomorphologie Supplementband 45, 205–225.Google Scholar
Thornthwaite, C.W., (1931). The climate of North America according to a new classification. Geographical Review 21, 633–655.Google Scholar
Thornthwaite, C.W., (1948). An approach toward a rational classification of climate. Geographical Review 38, 55–94.Google Scholar
Tudhope, A.W., Chilcott, C.P., McCulloch, M.T., Cook, E.R., Chappell, J., Ellam, R.M., Lea, D.W., Lough, J.M., Shimmield, G.B., (2001). Variability in the El Niño–Southern Oscillation through a glacial-interglacial cycle. Science 291, 1511–1517.Google Scholar
(1979). UNESCO, Map of World Distribution of Arid Regions. United Nations Educational, Scientific and Cultural Organization (UNECSO) Programme on Man and the Biosphere (MAB) Technical Notes 7, Explanatory Note (504p.) and Map (1 sheet at scale of 1:25,000,000). Google Scholar
Veatch, O., Stephenson, L.W., (1911). Preliminary report on the geology of the coastal plain of Georgia. Geological Survey of Georgia Bulletin 26, 466p.Google Scholar
Vogel, J.S., Southon, J.R., Nelson, D.E., Brown, T.A., (1984). Performance of catalytically condensed carbon for use in accelerator mass spectrometry. Nuclear Instruments and Methods in Physics Research B B5, 289–293.Google Scholar
Wasson, R.J., Nanninga, P.M., (1986). Estimating wind transport of sand on vegetated surfaces. Earth Surface Processes and Landforms 11, 505–514.CrossRefGoogle Scholar
Watts, W.A., (1980a). Late-Quaternary vegetation history at White Pond on the inner Coastal Plain of South Carolina. Quaternary Research 13, 187–199.Google Scholar
Watts, W.A., (1980b). The late Quaternary vegetation history of the southeastern United States. Annual Review of Ecology and Systematics 11, 387–409.Google Scholar
Webb III, T., Bartlein, P.J., Harrison, S.P., Anderson, K.H., (1993). Vegetation, lake levels, and climate in eastern North America for the past 18,000 years. Wright jr., J.E., Kutzbach, J.E., Webb III, T., Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J. Global Climates Since the Last Glacial Maximum. University of Minnesota Press, Minneapolis, MN.415–467.Google Scholar
Wiggs, G.F.S., Thomas, D.S.G., Bullard, J.E., (1995). Dune mobility and vegetation cover in the southwest Kalahari Desert. Earth Surface Processes and Landforms 20, 515–529.Google Scholar
Wintle, A.G., Murray, A.S., (2006). A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41, 369–391.Google Scholar
Wright jr., H.E., Kutzbach, J.E., Webb III, T., Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J., (1993). Global Climates Since the Last Glacial Maximum. University of Minnesota Press, Minneapolis, MN.(569 pp.).Google Scholar
Yang, X., Li, H., Conacher, A., (2012). Large-scale controls on the development of sand seas in northern China. Quaternary International 250, 74–83.Google Scholar