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Dominance of an ∼150-Year Cycle of Sand-Supply Change in Late Holocene Dune-Building along the Eastern Shore of Lake Michigan

Published online by Cambridge University Press:  20 January 2017

Walter L. Loope  and
Alan F. Arbogast
Walter L. Loope
Affiliation:
U.S. Geological Survey, Munising, Michigan, 49862
Alan F. Arbogast
Affiliation:
Department of Geography, Michigan State University, East Lansing, Michigan, 48824
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Abstract

Outcrops of buried soils on lake-plains and glacial headlands along Lake Michigan's eastern shore suggest that periodic dune-building has occurred there after relatively long (≥100 yr) periods of low sand supply. We located, described, and radiocarbon dated 75 such buried soils that crop out in 32 coastal dune fields beside the lake. We assume that peaks in probability distributions of calibrated 14C ages obtained from wood, charcoal, and other organic matter from buried A horizons approximate the time of soil burial by dunes. Plotted against a late Holocene lake-level curve for Lake Michigan, these peaks are closely associated with many ∼150-yr lake highstands previously inferred from beach ridge studies. Intervening periods of lower lake levels and relative sand starvation apparently permitted forestation and soil development at the sites we studied. While late Holocene lake-level change led to development and preservation of prominent foredunes along the southern and southwestern shores of Lake Michigan, the modern dune landscape of the eastern shore is dominated by perched dunes formed during ∼150-yr lake highstands over the past 1500 yr.

Keywords

Lake Michiganlake-leveldunesHolocenepaleosols
Type
Research Article
Information
Quaternary Research , Volume 54 , Issue 3 , November 2000 , pp. 414 - 422
Copyright
University of Washington

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References

Anderton, J.B., Loope, W.L.. Buried soils in a perched dunefield as indicators of late Holocene lake level change in the Lake Superior basin. Quaternary Research, 44, (1995). 190–199.CrossRefGoogle Scholar
Arbogast, A.F., Loope, W.L.. Maximum-limiting ages of Lake-Michigan coastal dunes: Their correlation with Holocene lake level history. Journal of Great Lakes Research, 25, (1999). 372–382.Google Scholar
Baedke, S.J., Thompson, T.A.. A 4,700 year record of lake level and isostasy for Lake Michigan. Journal of Great Lakes Research, 26, (2000). 416–426.CrossRefGoogle Scholar
Birkeland, P.W.. Pedology, Weathering and Geomorphological Research. (1974). Oxford Univ. Press, London.Google Scholar
Bishop, C.T.. Historical variation of water levels in Lakes Erie and Michigan-Huron. Journal of Great Lakes Research, 16, (1994). 406–425.Google Scholar
Bronk Ramsey, C.. Radiocarbon calibration and analysis of stratigraphy: The OxCal program. Radiocarbon, 37, (1995). 425–430.CrossRefGoogle Scholar
Bronk Ramsey, C.. Probability and dating. Radiocarbon, 40, (1998). 461–474.Google Scholar
Buckler, R. W. (1979). Dune Inventory and Barrier Dune Classification Study of Michigan's Lake Michigan Shore.Michigan Department of Natural Resources,Geological Survey Division Investigation 23, Lansing, MI.Google Scholar
Calver, J. L. (1946). The Glacial and Post-glacial History of the Platte and Crystal Lake Depressions, Benzie County, Michigan, Michigan Geological Survey. Occasional Papers on the Geology of Michigan for 1946,Publication 45, Geological Series 38, Lansing, MI.Google Scholar
Chrzastowski, M. J., Thompson, T. A. (1992). The late Wisconsinan and Holocene coastal evolution of the southern shore of Lake Michigan. InQuaternary Coasts of the United States: Marine and Lacustrine Systems(Fletcher, C. H., Wehmiller, J. F. Eds.),SEPM (Society for Sedimentary Geology) Special Publication 48,pp, 397–413.Google Scholar
Cowles, H.C.. The ecological relations of the vegetation on the sand dunes of Lake Michigan. Botanical Gazette, 27, (1899). 95–117.CrossRefGoogle Scholar
Dorr, J.A., Eschman, D.F.. Geology of Michigan. (1970). Univ. of Michigan Press, Ann Arbor.CrossRefGoogle Scholar
Dott, E.R., Mickelson, D.M.. Lake Michigan water levels and the development of Holocene beach-ridge complexes at Two Rivers, Wisconsin: Stratigraphic, geomorphic, and radiocarbon evidence. Geological Society of America Bulletin, 107, (1995). 286–296.2.3.CO;2>CrossRefGoogle Scholar
Dow, K.W.. The origin of perched dunes on the Manistee moraine, Michigan. Michigan Academy of Science, Arts and Letters Papers, 23, (1937). 427–440.Google Scholar
Farrand, W. R., Bell, D. L. (1982). Quaternary Geology of Michigan (Map). Michigan Department of Natural Resources-Geological Survey, .Google Scholar
Fraser, G.S., Larsen, C.E., Hester, N.C.. Climatically controlled high lake levels in the Lake Michigan and Lake Huron basins. Anais. Academia Brasileira Ciencias, 47, (1975). 51–66.Google Scholar
Fraser, G.S., Larsen, C.E., Hester, N.C.. Climatic control of lake levels in the Lake Michigan and Lake Huron basins. Schneider, A.F., Fraser, G.S.. Late Quaternary History of the Lake Michigan Basin. (1990). Geol. Soc. Am, Boulder., 75–89.Google Scholar
Fuller, G.D.. Some perched dunes of northern Lake Michigan and their vegetation. Illinois Academy of Science Transactions, 11, (1918). 111–112.Google Scholar
Geyh, M.A., Roeschmann, G.. The unreliability of 14C dates obtained from buried sandy podzols. Radiocarbon, 25, (1983). 409–416.Google Scholar
Gilet-Blein, N., Marien, G., Evin, J.. Unreliability of 14C dates from organic matter of soils. Radiocarbon, 22, (1980). 919–929.Google Scholar
Hands, E.B.. A geomorphic map of Lake Michigan shoreline. Proceedings of the 13th Conference on Great Lakes Research. International Association of Great Lakes Research. (1970). Great Lakes Research CenterU.S. Lake Survey, Detroit.p. 250–265Google Scholar
Hands, E.B.. The Great Lakes as a test model for profile responses to sea level changes. Komar, P.D.. CRC Handbook of Coastal Processes. (1983). CRC Press, Boca Raton., 167–189.Google Scholar
Hough, J.L.. The prehistoric Great Lakes of North America. American Scientist, 51, (1963). 84–109.Google Scholar
Hunter, R. E., Reiss, T. E., Chin, J. L., Anima, R. J. (1990). Coastal Erosional and Depositional Effects of the 1985–1987 High Lake Levels in Lake Michigan. Open-File Report 90-272,U.S. Geological Survey, Washington, D.C..Google Scholar
Larsen, C.E.. A Stratigraphic Study of Beach Features on the Southwestern Shore of Lake Michigan: New Evidence of Holocene Lake Level Fluctuations. (1985). Illinois State Geological Survey, Champaign.Google Scholar
Larsen, C.E.. Beach ridges as monitors of isostatic uplift in the upper Great Lakes. Journal of Great Lakes Research, 20, (1994). 108–134.Google Scholar
Lichter, J.. Lake Michigan beach-ridge and dune development, lake level, and variability in regional water balance. Quaternary Research, 44, (1995). 181–189.Google Scholar
Loope, W. L., Snyder, F. S., Anderton, J. B. (1995). Tentative Correlation of Lake Level. Soil Burial and Vegetation Cover in Perched Dune Fields of the Upper Great Lakes: A Preliminary Report,Report 1443PX632092115, National Park Service, .Google Scholar
Marsh, W.M., Marsh, B.D.. Wind erosion and sand dune formation on high Lake Superior bluffs. Geografiska Annaler, 69A, (1987). 379–391.CrossRefGoogle Scholar
Matthews, J.A., Dresser, P.Q.. Intensive 14C dating of a buried palaeosol horizon. Geol. Foren. Stockholm Forh., 105, (1983). 59–63.CrossRefGoogle Scholar
McEachern, A.K., Bowles, M.L., Pavlovic, N.B.. A metapopulation approach to Pitcher's thistle (Cirsium pitcheri) recovery in southern Lake Michigan dunes. Bowles, M.L., Whelan, C.J.. Restoration of Endangered Species. (1994). Cambridge Univ. Press, Cambridge., 194–218.Google Scholar
. Michigan Legislature. (1976). Sand Dune Protection and Management Act.Public Act 222, 78th Legislature,Regular Session of 1976, .Google Scholar
Olson, J.S.. Rates of succession and soil changes on southern Lake Michigan sand dunes. Botanical Gazette, 119, (1958). 125–170.Google Scholar
Olson, J.S.. Lake Michigan dune development. 1. Wind velocity profiles. Journal of Geology, 66, (1958). 254–263.Google Scholar
Olson, J.S.. Lake Michigan dune development. 2. Plants of agents and tools in geomorphology. Journal of Geology, 66, (1958). 345–351.Google Scholar
Olson, J.S.. Lake Michigan dune development. 3. Lake level, beach and dune oscillations. Journal of Geology, 66, (1958). 473–483.CrossRefGoogle Scholar
Olsson, I.U.. Radiometric dating. Berglund, B.E.. Handbook of Holocene Paleoecology and Paleohydrology. (1986). Wiley, Chichester.Google Scholar
Pilcher, J.R.. Radiocarbon dating and the palynologist: A realistic approach to accuracy. Cahmbers, F.M.. Climate Change and Human Impacts on the Landscape: Studies in Palaeolecolgy and Environmental Archaeology. (1993). Chapman and Hall, New York., 23–32.Google Scholar
Pye, K.. Physical and human influences on coastal dune development between the Ribble and Mersey estuaries, northwest England. Nordstrom, K.F., Carter, R.W.G.. Coastal Dunes: Form and Process. (1990). Wiley, New York., 339–359.Google Scholar
Schoeneberger, P.J., Wysocki, D.A., Benham, E.C., Broderson, W.D.. Field Book for Describing and Sampling Soils. (1998). U.S. Department of AgricultureNatural Resources Conservation ServiceNational Soil Survey Center, Lincoln.Google Scholar
Snyder, F.S.. A Spatial and Temporal Analysis of the Sleeping Bear Dunes Complex, Michigan. (1985). University of Pittsburgh, Google Scholar
Stevenson, E.B.. The dunes of the Manistique area. Papers of the Michigan Academy of Science, Arts and Letters, 14, (1930). 475–485.Google Scholar
Stuiver, M., Reimer, P.J.. Extended 14C data base and revised calib 3.0 14C age calibration program. Radiocarbon, 35, (1993). 215–230.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.. INTCAL98 radiocarbon age calibration 24,000–0 cal B.P. Radiocarbon, 40, (1998). 1041–1083.Google Scholar
Thompson, T.A.. Beach-ridge development and lake-level variation in southern Lake Michigan. Sedimentary Geology, 80, (1992). 305–318.CrossRefGoogle Scholar
Thompson, T.A., Baedke, S.J.. Beach-ridge development in Lake Michigan: Shoreline behavior in response to quasi-periodic lake-level events. Marine Geology, 129, (1995). 163–174.Google Scholar
Thompson, T.A., Baedke, S.J.. Strand-plain evidence for late Holocene lake-level variations in Lake Michigan. Geological Society of America Bulletin, 109, (1997). 666–682.Google Scholar
Thompson, T.A., Baedke, S.J.. 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. (1999). 30–34.Google Scholar
Walbom, T. E. (1999). Surficial Geology of Sleeping Bear Dunes National Lakeshore, Michigan: A Product of the USGS-EDMAP Program (Map). Geological Society of America, North-Central Section Meeting.Abstracts with programs, 31, (5), A-78, Geol. Soc. Am. Boulder, CO, .Google Scholar