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Provenance, age, and environment of mid-wisconsinan slackwater lake sediment in the St. Louis Metro East Area, USA

Published online by Cambridge University Press:  20 January 2017

B. Brandon Curry  and
David A. Grimley
B. Brandon Curry*
Affiliation:
Illinois State Geological Survey, 615 E. Peabody Dr., Champaign, IL 61820, USA
David A. Grimley
Affiliation:
Illinois State Geological Survey, 615 E. Peabody Dr., Champaign, IL 61820, USA
*
*Corresponding author.Email Address:[email protected](B.B. Curry).
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Abstract

Valleys tributary to the Mississippi River contain fossiliferous slackwater lake sediment (Equality Formation) deposited in response to aggradation of the Mississippi River valley during the last glaciation. In the St. Louis Metro East area, the lower part of the Equality Formation is primarily laminated, fossiliferous silt and clay deposited from about 44,150 to 24,310 14C yr B.P. The upper Equality Formation is primarily very fine sand to silt deposited from about 21,200 to 17,000 14C yr B.P. Among the four cores that sample this succession in the St. Louis Metro East area, core MNK-3 (38.64EN, 90.01EW) was selected for detailed study. Three sources are distinguished by the following characteristics: (1) gray smectite-quartz-Se-rich, feldspar-poor material of the Des Moines, Wadena, and James lobes; (2) reddish brown kaolinite–Cu–Fe-rich sediment of the Superior and Rainy lobes; and (3) brown illite–dolomite–Sr-rich sediment of the Lake Michigan and Green Bay lobes. The earliest sediments (44,150 to 41,700 14C yr B.P.) were derived from the central and western provenances and are chronocorrelative with the lower Roxana Silt. A hiatus occurred from about 41,700 to 29,030 14C yr B.P. when much of the middle Roxana Silt (Meadow Member) was deposited on adjacent uplands. The youngest sediment includes evidence of heightened activity of the Superior Lobe at about 29,000 14C yr B.P., the Lake Michigan and Green Bay lobes from about 25,000 to 24,000 14C yr B.P., and the Wadena-Des Moines-James lobes at about 21,000 14C yr B.P.

Keywords

St. LouisSlackwaterProvenanceWisconsinanMineralogy
Type
Original Articles
Information
Quaternary Research , Volume 65 , Issue 1 , January 2006 , pp. 108 - 122
Copyright
University of Washington

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References

Baker, F.C., (1939). Fieldbook of Illinois land snails. Illinois Natural History Survey Manual vol. 2, Illinois Natural History Survey, Champaign, IL.166 pp.Google Scholar
Bettis, E.A. III(1997). Late–Middle and Early Wisconsin glaciation in north-central Iowa. Geological Society of America Abstracts With Programs 29, 5.Google Scholar
Bettis, E.A. III, Quade, D.J., Schwert, D.P., Torpen, H.J., Baker, R.G., (1996). Stop 2. National gypsum company, Kauffman-George Pit, Fort Dodge, Iowa. Guidebook Series vol. 18, Geological Survey Bureau, Iowa Department of Natural Resources, 95–98.Google Scholar
Brouwers, E.M., Cronin, T.M., Horne, D.J., Lord, A.R., (2000). Recent shallow marine ostracods from high latitudes: implications for late Pliocene and Quaternary Paleoclimatology. Boreas 29, 127–143.Google Scholar
Chapman, M.R., Shackleton, N.J., (1998). What level of resolution is attainable in a deep-sea core? Results of a spectrophotometer study. Paleoceanography 13, 311–315.Google Scholar
Commission Internationale de l'Eclairage (CIE), (1978). Recommendations on Uniform Color Spaces, Color Difference and Psychometric Color Terms.. Paris, CIE, Colorimetry, publication 15, supplement 2, 21 pp.Google Scholar
Curry, B.B., (1989). Absence of Altonian glaciation in Illinois. Quaternary Research 31, 1–13.Google Scholar
Curry, B.B., (1998). Evidence at Lomax, Illinois, for mid-Wisconsin (ca. 40,000 yr B.P.) position of the Des Moines Lobe, and for diversion of the Mississippi River by the Lake Michigan Lobe (20,350 yr B.P.). Quaternary Research 50, 128–138.Google Scholar
Curry, B.B., Follmer, L.R., (1992). The last interglacial–glacial transition in Illinois: 123–25 ka.Clark, P.U., Lea, P.D. The Last Interglacial–Glacial Transition in North America: Geologic Society of America Special Paper vol. 270, Geological Society of America, Boulder, CO.71–88.Google Scholar
Curry, B.B., Pavich, M.J., (1996). Absence of glaciation in Illinois during marine oxygen isotope stages 3 through 5. Quaternary Research 46, 19–26.Google Scholar
Curry, B.B., Grimley, D.A., Stravers, J.A., (1999). Quaternary geology, geomorphology, and climatic history of Kane County, Illinois. Illinois State Geological Survey Guidebook vol. 28, Illinois State Geological Survey, Champaign, IL.40 pp.Google Scholar
Curry, B.B., Dorale, J.A., Henson, R.A., (2002). Function-fitting vegetation proxy record profiles of the Sangamon and Wisconsin Episodes from Missouri and Illinois. Geological Society of America, Abstracts with Programs 34, 6, 199.Google Scholar
Curry, B.B., Grimley, D.A., Phillips, A.C., (2003). Slackwater Lake Deposits Along the Large Rivers in the Midwestern U.S.—Archives of Distal Glacial Environments South of the Laurentide Ice Sheet.Third International Limnogeology Congress, Abstract Volume. Department of Geology, University of Arizona, 61.Google Scholar
Dorale, J.A., Edwards, R.E., Ito, E., Gonzalez, L.A., (1998). Climate and vegetation history of the Midcontinent from 75 to 25 ka: a speleothem record from Crevice Cave, Missouri, USA. Science 282, 1871–1874.Google Scholar
Fox, J., (1987). Mineralogy and Stratigraphy of Illinoian and Pre-Illinoian Tills Across South-Central Illinois, Unpublished Master's Thesis.. Urbana-Champaign, University of Illinois., 113 pp.Google Scholar
Frye, J.C., Glass, H.D., Willman, H.B., (1968). Mineral Zonation of Woodfordian Loesses of Illinois. Illinois State Geological Survey Circular vol. 427, Illinois State Geological Survey, Champaign, IL.44 pp.Google Scholar
Frye, J.C., Leonard, A.B., Willman, H.B., Glass, H.D., (1972). Geology and Paleontology of Late Pleistocene Lake Saline, Southeastern Illinois. Illinois State Geological Survey Circular vol. 471, Illinois State Geological Survey, Champaign, IL.44 p.Google Scholar
Gowan, A.S., (1998). Methods of till analysis for correlation and provenance studies in Minnesota.Patterson, C.J., Wright, H.E. Jr. Contributions to Quaternary Studies in Minnesota. Minnesota Geological Survey, Report of Investigations vol. 49, Minnesota Geological Survey, St. Paul, MN.159–178.Google Scholar
Grimley, D.A., (2000). Glacial and nonglacial sediment contributions to Wisconsin Episode loess in the central United States. Bulletin Geological Society of America 112, 1475–1495.Google Scholar
Grimley, D.A., (2002). Surficial Geology Map, Elsah Quadrangle, Jersey and Madison Counties, Illinois.. Illinois State Geological Survey, Illinois Geologic Quadrangle Map IGQ Elsah-SG, scale 1:24,000..Google Scholar
Grimley, D.A. and McKay, E.D. III (2004). Surficial Geology of French Village Quadrangle, St.. Clair County, Illinois. Illinois State Geological Survey, Illinois Geologic Quadrangle Map IGQ French Village-SG, scale 1:24,000..Google Scholar
Grimley, D.A., Follmer, L.R., McKay, E.D. III(1998). Magnetic susceptibility and mineral zonations controlled by provenance in loess along the Illinois and central Mississippi River Valleys. Quaternary Research 49, 24–36.Google Scholar
Grimley, D.A., Phillips, A.P., Follmer, L.R., Wang, H., Nelson, R.S., (2001). Quaternary and environmental geology of the St. Louis Metro East area.Malone, David Guidebook for Field Trip for the 35th Annual Meeting of the North-Central Section of the Geological Society of America Illinois State Geological Survey Guidebook vol. 33, Illinois State Geological Survey, Champaign, IL.21–73.Google Scholar
Hajic, E.R., (1990). Late Pleistocene and Holocene landscape evolution, depositional subsystems, and stratigraphy in the lower Illinois River Valley and adjacent central Mississippi River valley.. Unpublished PhD. dissertation, University of Illinois at Urbana-Champaign., 342 pp.Google Scholar
Hajic, E.R., Johnson, W.H., Follmer, L.R., (1991). Quaternary deposits and landforms, confluence region of the Mississippi, Missouri, and Illinois Rivers, Missouri and Illinois: terraces and terrace problems.Midwest Friends of the Pleistocene Guidebook, 38th Field Conference, May 10–12, 1991, Department of Geology, University of Illinois at Urbana-Champaign106 pp.Google Scholar
Hubricht, L., (1985). The distributions of the native land mollusks of the eastern United States. Fieldiana: Zoology New Series vol. 24, 191 pp.Google Scholar
Hughen, K., Lehman, S., Southon, J., Overpeck, J., Amrchal, O., Herring, C., Turnbull, J., (2004). 14C activity and global carbon cycle changes over the past 50,000 years. Science 303, 202–207.Google Scholar
Hughes, R.E., Moore, D.M., Glass, H.D., (1994). Qualitative and quantitative analysis of clay minerals in soils.Amonette, J.E., Zelazny, L.W. Quantitative Methods in Soil Mineralogy Soil Science Society of America Miscellaneous Publication, Madison, WI.330–359.Google Scholar
Johnson, W.C., Willey, K.L., (2004). Environment and Distribution of Mid-Wisconsin Grassland in the Central Great Plains.American Quaternary Association Program and Abstracts of the 18th Biennial Meeting. Kansas Geological Survey, Lawrence, KS.113.Google Scholar
Kempton, J.P., Hackett, J.E., (1968). Stratigraphy of the Woodfordian and Altonian drifts of central northern Illinois.Bergstrom, R.E. The Quaternary of Illinois—A Symposium in Observance of the Centennial of the University of Illinois University of Illinois College of Agriculture, Special Publication, Urbana vol. 14, Illinois State Geological Survey, Champaign, IL.27–34.Google Scholar
Larsen, D., Thibault, C., Krutak, P., (2002). Late Pleistocene fluvio-lacustrine deposits at Fulton, Tennessee: Slack-water deposits or tributary aggradation along the ancestral Ohio-Mississippi River Valley. Geological Society of America Abstracts with Programs 34, 2, A98.Google Scholar
Leigh, D.S., (1994). Roxana Silt of the Upper Mississippi Valley: lithology, source, and paleoenvironment. Geological Society of America Bulletin 106, 430–442.Google Scholar
Leigh, D.S., Knox, J.C., (1993). AMS radiocarbon age of the upper Mississippi River Valley Roxana Silt. Quaternary Research 39, 282–289.Google Scholar
Leonard, A.B., Frye, J.C., (1960). Wisconsinan molluscan faunas of the Illinois Valley region. Illinois State Geological Survey Circular vol. 304, Illinois State Geological Survey, Champaign, IL.32 pp.Google Scholar
McKay, E.D. III (1979). Stratigraphy of Wisconsinan and older loesses in southwestern Illinois. Illinois State Geological Survey Guidebook vol. 14, 37–67.Google Scholar
McNeal, J.M., Balistrieri, L.S., (1989). Geochemistry and occurrence of selenium—An overview.Jacobs, L.W. Selenium in Agriculture and The Environment. Madison, Wisconsin, American Society of Agronomy, Inc., and Soil Science Society of America, Inc. 1–13.Google Scholar
Meyer, G.N., (1986). Subsurface and till stratigraphy of the Todd County area, central Minnesota.. Minnesota Geological Survey Report of Investigations 34, 40 pp.Google Scholar
Panno, S.V., Curry, B.B., Wang, H., Hackley, K.C., Liu, C.-L., (2004). Climate change in southern Illinois based on the age and 13C of organic matter in cave sediments. Quaternary Research 61, 301–313.Google Scholar
Phillips, A.C., (2004). Surficial Geology of Collinsville Quadrangle, Madison and St. Clair Counties, Illinois:. Illinois State Geological Survey, Illinois Preliminary Geologic Map, IPGM Collinsville-SG, 1:24,000.Google Scholar
Rittenour, T.M., (2004). Fluvial evolution of the lower Mississippi Valley over the last glacial cycle.. Unpublished PhD dissertation, University of Nebraska, Lincoln.. 295 pp.Google Scholar
Schmidt, R.A., Sellmann, P.V., (1966). Mummified Pleistocene ostracods in Alaska. Science 153, 167–168.Google Scholar
Shaw, E.W., (1915). Newly discovered beds of extinct lakes in southern and western Illinois and adjacent states. Illinois State Geological Survey Bulletin 20, 139–157.Google Scholar
Stewart, M.T., Mickelson, D.M., (1976). Clay mineralogy and relative age of tills in north-central Wisconsin. Journal of Sedimentary Petrology 46, 200–205.Google Scholar
Trent, G.C., Esling, S.P., (1995). The big muddy valley (Chapter 1).Quaternary Sections in Southern Illinois and Southeast Missouri, Midwest Friends of the Pleistocene 42nd Annual Meeting, Southern Illinois University, CarbondaleGoogle Scholar
Wilkinson, L., (1990). SYSTAT: The System for Statistics. SYSTAT, Inc., Evanston, IL.677 pp.Google Scholar
Willman, H.B., Frye, J.C., (1970). Pleistocene Stratigraphy of Illinois. Illinois State Geological Survey Bulletin vol. 94, Illinois State Geological Survey, Champaign, IL.204 pp.Google Scholar