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The OSL chronology of eolian sand deposition in a perched dune field along the northwestern shore of Lower Michigan

Published online by Cambridge University Press:  20 January 2017

Bradley E. Blumer
Affiliation:
Geographic Information System and Earth Science Specialist, City of Janesville, WI, 53548, USA
Alan F. Arbogast*
Affiliation:
Department of Geography, Michigan State University, East Lansing, MI, 48824, USA
Steven L. Forman
Affiliation:
Department of Earth and Environmental Sciences, The University of Illinois at Chicago, Chicago, IL, 60607, USA
*
*Corresponding author: Fax: + 1 517 432 1671. E-mail address:dunes@msu.edu (A.F. Arbogast).

Abstract

Extensive coastal dunes occur in the Great Lakes region of North America, including northwestern Michigan where some are perched on high (~ 100 m) bluffs. This study focuses on such a system at Arcadia Dunes and is the first to systematically generate optical ages from stratigraphic sections containing buried soils. Dune growth began ca. 4.5 ka during the Nipissing high lake stand and continued episodically thereafter, with periods of increased sand supply at ca. 3.5 ka and ca. 1.7 ka. The most volumetrically dominant phase of dune growth began ca. 1.0 ka and continued intermittently for about 500 years. It may have begun due to the combined effects of a high lake phase, potential changes in lake hydrodynamics with final isostatic separation of Lake Superior from Lakes Michigan and Huron, and increased drought and hydrologic variability associated with the Medieval Warm Period. Thus, this latest eolian phase likely reflects multiple processes associated with Great Lakes water level and climate variability that may also explain older eolian depositional events. Comparison of Arcadia ages and calendar corrected 14C ages from previous studies indicate broad chronological agreement between events at all sites, although it appears that dune growth began later at Arcadia.

Type
Original Articles
Copyright
University of Washington

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References

Anderton, J.B., Loope, W.L., (1995). Buried Soils in a perched dunefield as indicators of Late Holocene lake-level change in the Lake Superior basin. Quaternary Research. 44, 190199.Google Scholar
Arbogast, A.F., (1996). Stratigraphic evidence for late-Holocene eolian sand mobilization and soil formation in south-central Kansas. Journal of Arid Environments. 34, 403414.Google Scholar
Arbogast, A.F., (2000). Estimating the time since final stabilization of a perched dune field along Lake Superior. The Professional Geographer. 52, 594606.Google Scholar
Arbogast, A.F., (2009). Sand Dunes. Schaetzl, R.J., Darden, J.T., Brandt, D., Michigan Geography and Geology, Pearson Custom Publishers, Upper Saddle River, NJ, 274287.Google Scholar
Arbogast, A.F., Loope, W.L., (1999). Maximum-limiting ages of Lake Michigan coastal dunes: their correlation with Holocene lake level history. Journal of Great Lakes Research. 25, 372382.CrossRefGoogle Scholar
Arbogast, A.F., Packman, S.C., (2004). Middle-Holocene mobilization of aeolian sand in western upper Michigan and the potential relationship with climate and fire. The Holocene. 14, 464471.Google Scholar
Arbogast, A.F., Hansen, E.C., Van Oort, M.D., (2002a). Reconstructing the geomorphic evolution of large coastal dunes along the southeastern shore of Lake Michigan. Geomorphology. 46, 241255.Google Scholar
Arbogast, A.F., Wintle, A.G., Packman, S.C., (2002b). Widespread middle Holocene dune formation in the eastern Upper Peninsula of Michigan and the relationship to climate and outlet-controlled lake level. Geology. 30, 5558.Google Scholar
Arbogast, A.F., Shortridge, A.M., Bigsby, M.E., (2009). Using volumetric estimates of eolian sand to explain the geography of coastal sand dunes in Lower Michigan. Physical Geography. 30, 479500.Google Scholar
Argyilan, E.P., Forman, S.L., Johnston, J.W., Wilcox, D.A., (2005). Optically stimulated luminescence dating of late Holocene raised strandplain sequences adjacent to Lakes Michigan and Superior, Upper Peninsula, Michigan, USA. Quaternary Research. 63, 122135.CrossRefGoogle Scholar
Argyilan, E.P., Forman, S.L., Thompson, T.A., (2010). Variability of Lake Michigan waterlevel during the past 1000 years reconstructed through optical dating of a coastal strandplain. The Holocene. 20, 723731.Google Scholar
Baedke, S., Thompson, T.A., (2000). A 4,700 year record of lake level and isostasy for Lake Michigan. Journal of Great Lakes Research. 26, 416426.Google Scholar
Bailey, S.D., Wintle, A.G., Duller, G.A.T., Bristow, C.S., (2001). Sand deposition during the last millennium at Aberffraw, Anglesey, North Wales as determined by OSL dating of quartz. Quaternary Science Reviews. 20, 701704.Google Scholar
Bauer, B.O., Sherman, D.J., (1999). Coastal dune dynamics: problems and prospects. Goudie, A.S., Livingstone, I., Stokes, S., Aeolian Environments, Sediments and Landforms, Wiley, New York, 71104.Google Scholar
Blewett, W.L., (1990). The glacial geomorphology of the Port Huron complex in northwestern Southern Michigan. Ph.D. dissertation. Michigan State University.Google Scholar
Booth, R.K., Notaro, M., Jackson, S.T., Kutzbachm, J.E., (2006a). Widespread drought episodes in the western Great Lakes in the past 2000 years: Geographic extent and potential mechanisms. Earth and Planetary Science Letters. 242, 415427.CrossRefGoogle Scholar
Booth, R.K., Kutzbach, J.E., Hotchkiss, S.C., Bryson, R.A., (2006b). A reanalysis of the relationship between strong westerlies and precipitation in the Great Plains and Midwest regions of North America. Climatic Change. 76, 427441.Google Scholar
Bøtter-Jensen, L., Bulur, E., Duller, G.A.T., Murray, A.S., (2000). Advances in luminescence instrument systems. Radiation Measurements. 32, 523528.Google Scholar
Carter, R.W.G., Nordstrom, K.F., Psuty, N.P., (1990). The study of coastal dunes. Nordstron, K.F., Psuty, N.P., Carter, R.W.G., Coastal Dunes Form and Process, Wiley, New York, 114.Google Scholar
Clemmensen, L.B., Pye, K., Murray, A., Heinemeir, J., (2001). Sedimentology, stratigraphy and landscape evolution of a Holocene coastal dune system, Lodbjerg, NW Jutland, Denmark. Sedimentology. 48, 327.Google Scholar
Dow, K.W., (1937). The origin of perched dunes on the Manistee Moraine, Michigan. Michigan Academy of Science Arts and Letters. 23, 427440.Google Scholar
Duller, G.A.T., Botter-Jensen, L., Murray, A.S., (2003). Combining infrared and green-laser stimulation sources in single-grain luminescence measurements of feldspar and quartz. Radiation Measurements. 37, 543550.Google Scholar
Evenson, E.B., Farrand, W.R., Eschman, D.F., Mickelson, D.M., Maher, L.J., (1976). Greatlakean Substage: A Replacement for Valderan Substage in the Lake Michigan basin. Quaternary Research. 6, 411424.Google Scholar
Fain, J., Soumana, S., Montret, M., Miallier, D., Pilleyre, T., Sanzelle, S., (1999). Luminescence and ESR dating-Beta-dose attenuation for various grain shapes calculated by a Monte-Carlo method. Quaternary Science Reviews. 18, 231234.CrossRefGoogle Scholar
Farrand, W., (1988). Glacial Lakes around Michigan. Michigan Department of Environmental Quality, Geological Survey Division, Lansing, MI.Google Scholar
Farrand, W.R., and Bell, D.L., (1982). Quaternary Geology of Michigan (Map). Michigan Department of Natural Resources-Geological Survey.Google Scholar
Feng, S., Oglesby, R.J., Rowe, C.M., Loope, D.B., Hu, Q., (2008). Atlantic and Pacific SST influences on Medieval drought in North America simulated by the Community Atmospheric Model. Journal of Geophysical Research-Atmospheres. 113, D11 .Google Scholar
Fisher, T.G., Loope, W.L., (2005). Aeolian sand preserved in Silver Lake: A new signal of Holocene high stands of Lake Michigan. The Holocene. 15, 10721078.CrossRefGoogle Scholar
Forman, S.L., Gomez, J., Marin, L., Webb, R., Miller, G.H., (2001). Deciphering eolian sand depositional records from the western Great Plains. Overpeck, J., Trenberth, K., Proceedings of the CLIVAR/PAGES/IPCC Workshop: A multi-millennial perspective on drought and implications for the future. Tucson, AZ, 2003.Google Scholar
Forman, S.L., Nordt, L., Gomez, J., Pierson, J., (2009). Late Holocene dune migration on the south Texas sand sheet. Geomorphology. 108, 159170.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 1, Experimental design and statistical models. Archaeometry. 41, 339364.Google Scholar
Gares, P.A., Nordstrom, K.F., (1995). A cyclic model of foredune blowout evolution for a leeward coast: Island Beach, New Jersey. Annals of the Association of American Geographers. 85, 120.Google Scholar
Hansen, E.C., Arbogast, A.F., Packman, S.C., Hansen, B., (2002). Post-Nipissing origin of a backdune complex along the southeastern shore of Lake Michigan. Physical Geography. 23, 233244.Google Scholar
Hansen, E.C., Fisher, T.G., Arbogast, A.F., Bateman, M., (2010). Geomorphic history of low perched, transgressive dune complexes along the southeastern shore of Lake Michigan. Aeolian Research. 1, 111127.Google Scholar
Hanson, P.R., Joeckel, R.M., Young, A.R., Horn, J., (2009). Late Holocene dune activity in the Eastern Platte River Valley, Nebraska. Geomorphology. 103, 555561.CrossRefGoogle Scholar
Hanson, P.R., Arbogast, A.F., Johnson, W.C., Joeckel, R.M., Young, A.R., (2010). Megadroughts and late Holocene dune activation at the eastern margin of the Great Plains, north-central Kansas, USA. Aeolian Research. 1, 101110.Google Scholar
Hesp, P.A., (2001). The Manawatu Dunefield: Environmental change and human impacts. New Zealand Geographer. 57, 3340.Google Scholar
Holmes, P.J., Barker, C.H., Bateman, M.D., Thomas, D.S.G., Telfer, M.W., Lawson, M.P., (2008). A Holocene-late Pleistocene aeolian record from lunette dunes of the western Free State panfield, South Africa. The Holocene. 18, 11931205.CrossRefGoogle Scholar
Johnston, J.W., Thompson, T.A., Wilcox, D.A., Baedke, S.J., (2007). Geomorphic and sedimentologic evidence for the separation of Lake Superior from Lake Michigan and Huron. Journal of Paleolimnology. 37, 349364.Google Scholar
Kroell III, M.L., (2008). Soil Survey of Benzie and Manistee Counties, Michigan. United States Department of Agriculture Soil Conservation Service, U.S. Government Printing Office, Washington, D.C.Google Scholar
Larson, G., Schaetzl, R.J., (2001). Origin and evolution of the Great Lakes. Journal of Great Lakes Research. 27, 518546.Google Scholar
Lepczyk, X.C., Arbogast, A.F., (2005). Geomorphic history of dunes at Petoskey State Park, Petoskey, Michigan. Journal of Coastal Research. 21, 231241.Google Scholar
Leverett, F., Taylor, F.B., (1915). The Pleistocene of Indiana and Michigan and the history of the Great lakes. United States Geological Survey Monograph. 53, U.S. Government Printing Office, Washington, D.C, 529 pp.Google Scholar
Loope, W.L., Arbogast, A.F., (2000). Dominance of an 150-year cycle of sand-supply change in late Holocene dune-building along the eastern shore of Lake Michigan. Quaternary Research. 54, 414422.Google Scholar
Martinho, C.T., Hesp, P.A., Dillenburg, S.R., (2010). Morphological and temporal variations of transgressive dunefields of the northern and mid-littoral Rio Grande do Sul coast, Southern Brazil. Geomorphology. 117, 1432.Google Scholar
Mejdahl, V., Christiansen, H.H., (1994). Procedures used for luminescence dating of sediments. Boreas. 13, 403406.Google Scholar
Muhs, D.R., Maat, P.B., (1993). The potential response of eolian sands to greenhouse warming and precipitation reduction on the Great Plains of the U.S.A. Journal of Arid Environments. 25, 351361.Google Scholar
Murray, A.S., Wintle, A.G., (2003). The single aliquot regenerative dose protocol: potential for improvements in reliability. Radiation Measurements. 37, 377381.Google Scholar
Prescott, J.R., Hutton, J.T., (1994). Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements. 23, 497500.Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk, R.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, 11111150.CrossRefGoogle Scholar
Roberts, H.M., Plater, A.J., (2007). Reconstruction of Holocene foreland progradation using optically stimulated luminescence (OSL) dating: an example from Dungeness, UK. The Holocene. 17, 495505.Google Scholar
Short, A.D., (2010). Sediment transport around Australia - Sources, mechanisms, rates, and barrier forms. Journal of Coastal Research. 26, 395402.CrossRefGoogle Scholar
Singhvi, A.K., Bluszcz, A., Bateman, M.D., Rao, M.S., (2001). Luminescence dating of loess-palaeosol sequences and coversands: methodological aspects and palaeoclimatic implications. Earth-Science Reviews. 54, 193211.CrossRefGoogle Scholar
Snyder, F.S., (1985). A spatial and temporal analysis of the Sleeping Bear Dunes complex, Michigan (A contribution to the geomorphology of perched dunes in humid continental regions). Ph.D. dissertation. University of Pittsburgh.Google Scholar
Sridhar, V., Loope, D.B., Swinehart, J.B., Mason, J.A., Oglesby, R.J., Rowe, C.M., (2006). Large wind shift on the Great Plains during the Medieval Warm Period. Science. 313, 345347.Google Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14 C data base and revised CALIB 3.0 14 C age calibration program. Radiocarbon. 35, 215230.CrossRefGoogle Scholar
Tamura, T., Bateman, M.D., Kodama, Y., Saitoh, Y., Watanabe, K., Yamaquchi, N., Matsumoto, D., (2011). Building of shore-oblique transverse dune ridges revealed by ground-penetrating radar and optical dating over the last 500 years on Tottori coast, Japan Sea. Geomorphology. 132, 153166.Google Scholar
Thompson, T.A., Baedke, S.J., (1999). Strandplain evidence for reconstructing late Holocene lake level in the Lake Michigan Basin. Sellinger, C.E., Quinn, F.H., Proceedings of the Great Lakes Paleo-Levels Workshop: The Last 4000 years. Great Lakes Environmental Research Laboratory, NOAA Technical Memorandum ERL GLERL-113, 3034.August, 1999.Google Scholar
Van Oort, M., Arbogast, A.F., Hansen, E.C., Hansen, B., (2001). Geomorphological history of massive parabolic dunes, Van Buren State Park, Van Buren County, Michigan. Michigan Academician. 33, 175188.Google Scholar
Walker, I., Hesp, P.A., Davidson-Arnott, R., Ollerhead, J., (2006). Topographic steering of alongshore flow over a vegetated foredune: Greenwich dunes, Prince Edward Island, Canada. Journal of Coastal Research. 22, 12781291.CrossRefGoogle Scholar
Wang, Y., Amundson, R., Trumbore, S., (1996). Radiocarbon dating of soil organic matter. Quaternary Research. 45, 282288.Google Scholar