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Buried Soils in a Perched Dunefield as Indicators of Late Holocene Lake-Level Change in the Lake Superior Basin

Published online by Cambridge University Press:  20 January 2017

John B. Anderton  and
Walter L. Loope
John B. Anderton
Affiliation:
Department of Geography, University of Wisconsin, Madison, Wisconsin 53706
Walter L. Loope
Affiliation:
U.S. Department of the Interior, National Biological Service, Munising, Michigan 49862
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Abstract

A stratigraphic analysis of buried soils within the Grand Sable Dunes, a dune field perched 90 m above the southern shore of Lake Superior, reveals a history of eolian activity apparently linked with lake-level fluctuations over the last 5500 yr. A relative rise in the water plane of the Nipissing Great Lakes initially destabilized the lakeward bluff face of the Grand Sable plateau between 5400 and 4600 14C yr B.P. This led to the burial of the Sable Creek soil by eolian sediments derived from the bluff face. Subsequent episodes of eolian activity appear to be tied to similar destabilizing events; high lake levels may have initiated at least four and perhaps eleven episodes of dune building as expressed by soil burials within the dunes. Intervening low lake levels probably correlate with soil profile development, which varies from the well-developed Sable Creek Spodosol catena to thin organic layers containing in-place stumps and tree trunks. Paleoecological reconstructions available for the area do not imply enough climatic change to account for the episodic dune activity. Burial of soils by fine-fraction sediments links dune-building episodes with destabilization of the lower lake-facing bluff, which is rich in fines.

Type
Research Article
Information
Quaternary Research , Volume 44 , Issue 2 , September 1995 , pp. 190 - 199
Copyright
University of Washington

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References

Ahlbrandt, T. S. (1975). Comparison of textures and structures to distinguish eolian environments, Killpecker dune field, Wyoming. Mountain Geologist 12 , 61–73.Google Scholar
Ahlbrandt, T. S. Swinehart, J. B., and Maroney, D. G. (1983). The dynamic Holocene dune fields of the Great Plains and Rocky Mountain basins, U.S.A. In “Eolian Sediments and Processes,” (Brookfield, M. E. and Ahlbrandt, T. S., Eds.), pp. 379–406. Elsevier, Amsterdam.Google Scholar
Alexander, C. S., and Price, L. W. (1980). Radiocarbon dating of the rate of movement of two solifluction lobes in the Ruby Range, Yukon Territory. Quaternary Research 13 , 365–379.Google Scholar
Bach, D. P. (1978). “Plant Communities, Habitats and Soil Conditions of Grand Sable Dunes, Pictured Rocks National Lakeshore, Michigan.” Master’s thesis, Michigan Technological University.Google Scholar
Baker, R. G. Maher, L. J. Chumbley, C. A., and Van Zant, K. L. (1992). Patterns of Holocene environmental change in the midwestem United States. Quaternary Research 37 , 379–389.Google Scholar
Bartlein, P. J. Webb, T., and Fieri, E. (1954). Holocene climatic change in the northern Midwest’. Potten-derived estimates. Quaternary Research 22 , 361–374.Google Scholar
Berguist, S. C. (1936). The Pleistocene history of the Tahquamenon and Manistique drainage region of the northern peninsula of Michigan. “Michigan Geological Survey Publication 40,” Geological Series 34, Part 1, pp. 1–148.Google Scholar
Birkeland, P. W. (1974). “Pedology, Weathering and Geomorphological Research.” Oxford Univ. Press, London.Google Scholar
Bernabo, J. C. (1981). Quantitative estimates of temperature changes over the last 2700 years in Michigan based on pollen data. Quaternary Research 15 , 143–159.Google Scholar
Bernabo, J. C., and Webb, T. III (1977). Changing patterns in the Holocene pollen record of northeastern North America: A mapped summary. Quaternary Research 8 , 64–96.Google Scholar
Blewett, W. L., and Rieck, R. L. (1987). Reinterpretation of a portion of the Munising Moraine in northern Michigan. Geological Society of America Bulletin 98 , 169–175.Google Scholar
Brown, T. A. Nelson, D. E. Mathewes, R. W. Vogel, J. S., and Southon, J. R., (1989). Radiocarbon dating of pollen by accelerator mass spectrometry. Quaternary Research 32 , 205–212.Google Scholar
Businski, S. A. (1992). “Airphoto Interpretation of Vegetative Cover Change on the Sleeping Bear Dunes Complex, Leelanau County, Michigan, 1938-1987.” Master’s thesis, Michigan State University.Google Scholar
Carey, L. M. (1993). “Soil Survey of Pictured Rocks National Lakeshore, Alger Co., Michigan.” United States Department of Agriculture, Soil Conservation Service, Marquette, MI.Google Scholar
Coordinating Committee on Great Lakes Basin Hydraulic and Hydrologic Data (1977). “Apparent Vertical Movement over the Great Lakes: Detroit District.” United States Corps of Engineers.Google Scholar
Crispin, S. R. Dunevitz, V. L. Katz, D., and Chapman, K. A. (1984). “A Survey for Endangered, Threatened, and Special Concern Plant Species in Pictured Rocks National Lakeshore, Michigan.” Contract report to the National Park Service prepared by Michigan Natural Features Inventory.Google Scholar
Davis, M. B. Spear, R. W., and Shane, L. C. K. (1980). Holocene climate of New England. Quaternary Research 14 , 240–250.Google Scholar
Dean, W. E. Bradbury, J. P., and Anderson, R. Y. (1984). The variability of Holocene climate change: Evidence from varved lake sediments. Science 226 , 1191–1194.Google Scholar
Drexler, C. W. (1981). “Outlet channels for the post-Duluth lakes of the Upper Peninsula of Michigan.” Ph.D. dissertation, University of Michigan, Ann Arbor.Google Scholar
Drexler, C. W. Farrand, W. R., and Hughes, J. D. (1983). Correlation of glacial lakes in the Superior basin with eastward discharge events from Lake Agassiz, Geological Association of Canada Special Paper 26, pp. 303–323.Google Scholar
Eschman, D. F., and Karrow, P. F. (1985). Huron basin glacial lakes: A review. In “Quaternary Evolution of the Great Lakes” (Karrow, P. F. and Calkin, P. E., Eds.), Geological Society of Canada Special Paper 30, pp. 79–93.Google Scholar
Farrand, W. R., and Drexler, C. W. (1985). Late Wisconsinan and Holocene history of the Lake Superior basin. In “Quaternary Evolution of the Great Lakes” (Karrow, P. F. and Calkin, P. E., Eds.), Geological Association of Canada Special Paper 30, pp. 17–32.Google Scholar
Farrell, J. P., and Hughes, J. D. (1985). “Long Term Implications, From a Geomorphological Standpoint, of Maintaining H-58 in its Present Location at Grand Sable Lake,” Contract Report PX60000-4-0839, National Park Service.Google Scholar
Filion, L. (1984). A relationship between dunes, fire and climate recorded in the Holocene deposits of Quebec. Nature 309 , 543–546.Google Scholar
Filion, L. Saint-Laurent, D. Desponts, M., and Payette, S. (1991). The late Holocene record of aeolian and fire activity in northern Quebec, Canada. The Holocene 1 , 201–208.Google Scholar
Forester, R. M. Delorme, L. D., and Bradbury, J. P. (1987). Mid-Holocene climate in northern Minnesota. Quaternary Research 28 , 263–273.Google Scholar
Fraser, G. S. Larsen, C. E., and Hester, N. C. (1990). Climatic control of lake levels in the Lake Michigan and Lake Huron basins. In “Late Quaternary History of the Lake Michigan Basin” (Schneider, A. F. and Fraser, G. S., Eds.), pp. 75–89. Geological Society of America Special Paper 251. Google Scholar
Futyma, R. P. (1981). The northern limits of Glacial Lake Algonquin in Upper Michigan. Quaternary Research 15 , 291–310.Google Scholar
Gajewski, K. (1987). Climatic impacts on the vegetation of North America during the past 2000 years. Vegetatio 68 , 179–190.Google Scholar
Gee, G. W., and Bauder, J. W. (1986). Particle-size analysis. In “American Society of Agronomy-Soil Science Society of America. Methods of Soil Analysis: Part I, Physical and Mineralogical Methods,” Agronomy Monograph 9, pp. 383–411.Google Scholar
Gtigal, D. F. Severson, R. C., and Goltz, G. E. (1976). Evidence of eolian activity in north-cenlral Minnesota 8,000 to 5,000 yr ago. Geological Society of America Bulletin 87 , 1251–1254.Google Scholar
Hansel, A. K., and Mickelson, D. M. (1988). A réévaluation of the timing and causes of high lake phases in the Lake Michigan basin. Quaternary Research 29 , 113–128.Google Scholar
Holliday, V. T. (1989). Middle Holocene drought on the southern high plains. Quaternary Research 31 , 74–82.Google Scholar
Hough, J. L. (1958). “Geology of the Great Lakes.” Univ. Illinois Press, Urbana.Google Scholar
Hughes, J. D. (1978). Marquette buried forest 9850 years old. In “Abstracts of AAAS Annual Meeting, February 12-17, 1978.” Google Scholar
Keen, K. L., and Shane, L. C. K. (1990). A continuous record of Holocene eolian activity and vegetation change at Lake Ann, east-central Minnesota. Geological Society of America Bulletin 102 , 1646–1657.Google Scholar
Larsen, C. E. (1985). Lake level, uplift, and outlet incision, the Nipissing and Algoma Great Lakes. In “Quaternary Evolution of the Great Lakes” (Karrow, P. F. and Calkin, P. E., Eds.), Geological Association of Canada Special Paper 30, pp. 63–75.Google Scholar
Larsen, C. E. (1987). Geological history of glacial Lake Algonquin and the upper Great Lakes. U.S. Geological Survey Bulletin 1801. Google Scholar
Larsen, C. E. (1994). Beach ridges as monitors of isostatic uplift in the Upper Great Lakes. Journal of Great Lakes Research 20 , 108–134.Google Scholar
Leverett, F. (1929). “Moraines and Shorelines of the Lake Superior Region,” U.S. Geological Survey Professional Paper 154-A.Google Scholar
Liu, K. (1990). Holocene paleoecology of the boreal forest and Great Lakes-St. Lawrence forest in northern Ontario. Ecological Monographs 60 , 179–212.Google Scholar
Loope, W. L. McEachern, A. K., and Schultz, J. L. (1992). Plant habitat dynamics in a perched dune system adjacent to Lake Superior, Alger County, MI. Bulletin of the Ecological Society of America 73 , 254.Google Scholar
Marsh, W. M., and Marsh, B. D. (1987). Wind erosion and sand dune formation on high Lake Superior bluffs. Geografîska Annuler 69A, 379–391.Google Scholar
McEachern, A. K. (1992). “Disturbance dynamics of Pitcher’s thistle (Cirsium pitcheri) populations in Great Lakes sand dune landscapes.” Ph.D. dissertation, University of Wisconsin, Madison.Google Scholar
Muhs, D. R. (1985). Age and paleoclimatic significance of Holocene sand dunes in northeastern Colorado. Annals of the Association of North American Geographers 75 , 566–582.Google Scholar
Olson, J. S. (1958). Lake Michigan dune development 3: Lake level, dune and beach Oscillations. Journal of Geology 66 , 473–183.Google Scholar
Ruhe, R. V. (1965). Quaternary paleopedology. In “The Quaternary of the United States” (Wright, H. E. and Frey, D. G., Eds.), pp. 755–764. Princeton Univ Press, Princeton, NJ.Google Scholar
Ruhe, R. V. (1969). “Quaternary landscapes in Iowa.” Iowa State Univ Press, Ames, IA.Google Scholar
Schaetzl, R. J., and Mokma, D. L. (1988). A Numerical Index of Podzol and Podzolic Soil Development. Physical Geography 9 , 232–246.Google Scholar
Schultz, J. L. (1988). “Inventory of Several Rare Plant Species within the Grand Sable Dunes Area of Pictured Rocks National Lakeshore.” Report to the National Park Service, Omaha, NE.Google Scholar
Selley, R. C. (1976). “An Introduction to Sedimentology.” Academic Press, New York.Google 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
Soil Survey Division Staff (1975). “Soil Taxonomy: A Basic System for Making and Interpreting Soil Surveys,” Agriculture Handbook 436. United States Department of Agriculture, Soil Conservation Service.Google Scholar
Soil Survey Division Staff (1993). “Soil Survey Manual,” USDA Handbook No. 18. U.S. Government Printing Office, Washington, DC.Google Scholar
Swain, A. M. (1978). Environmental changes during the past 2000 years in north-central Wisconsin: Analysis of pollen, charcoal and seeds from varved lake sediments. Quaternary Research 10 , 55–68.Google Scholar
Teller, J. T., and Thorleifson, L. H. (1983). The Lake Agassiz-Lake Superior connection. In “Glacial Lake Agassiz” (Teller, J. T. and Clayton, L., Eds.), Geological Association of Canada Special Paper 26, pp. 261–290.Google Scholar
Thompson, T. A. Fraser, G. S., and Hester, N. C. (1991). “Lake-Level Variation in Southern Lake Michigan: Magnitude and Timing of Fluctuations over the Past 4,000 Years,” lllinois-Indiana Sea Grant Program Report IL-IN-SG-R-91-2. Illinois Cooperative Extension Service, Univ. Illinois at Urbana-Champaign.Google Scholar
Webb, T. III Cushing, E. J., and Wright, H. E. (1983). Holocene changes in the vegetation of the Midwest. In “Late Quaternary Environments of the United States: Vol. 2, The Holocene” (Wright, H. E. Jr., Ed.), pp. 142–165. Univ. of Minnesota Press, Minneapolis, MN.Google Scholar
Winkler, M. G. (1988). Effect of climate on development of two Sphagnum bogs in south-central Wisconsin. Ecology 69 , 1032–1043.Google Scholar
Winkler, M. G. Swain, A. M., and Kutzbach, J. E. (1986). Middle Holocene dry period in the northern Midwestern United States: Lake levels and pollen stratigraphy. Quaternary Research 25 , 235–250.Google Scholar
Wright, H. E. (1992). Patterns of Holocene climatic change in the midwestem United States, Quaternary Research 38 , 129–134.Google Scholar