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New insights on Illinoian deglaciation from deposits of Glacial Lake Quincy, central Indiana

Published online by Cambridge University Press:  20 January 2017

J.R. Wood ,
S.L. Forman ,
J. Pierson  and
J. Gomez
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Abstract

The deposits of Glacial Lake Quincy overlie a diamicton associated with the classically defined Illinoian limit in central Indiana. This lake covered at least 180 km2 with a depth of > 20 m and developed when the Illinoian ice sheet retreated 15 km from the maximum limit, causing lake impoundment against Devore Ridge. Overflow from Glacial Lake Quincy eroded across the ridge forming a number of steeped-walled outlets. A section along Mill Creek exposes a sedimentologic sequence associated with Glacial Lake Quincy from a subglacial diamicton to ice-proximal to ice-distal glacial lacustrine sediments. We report new optical ages by multiple aliquot regenerative dose procedure for the fine-grained rhythmically bedded sediments presumed to represent the lowest energy depositional facies, dominated by suspension settling, which maximized sunlight exposure. In turn, optical ages were determined on the fine-grained (4-11 μm) polymineral and quartz fractions under infrared and blue excitation, which yielded statistically similar ages. Optical ages span from ca. 170 to 108 ka, with the average of 16 optical ages indicating deglaciation at ca. 135 ka, generally coincident with Marine Oxygen Isotope Stage 6-to-5 transition and rise in global sea level.

Keywords

Illinoian limitGlacial lacustrine sedimentsOptical dating
Type
Original Articles
Information
Quaternary Research , Volume 73 , Issue 2 , March 2010 , pp. 374 - 384
Copyright
University of Washington

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References

Addington, A.R., (1926). Porter's Cave and recent drainage adjustments in its vicinity. Proceedings of the Indiana Academy of Science 36, 116–117.Google Scholar
Agersnap-Larsen, N., Bulur, E., McKeever, S.W.S., (2000). Use of LM-OSL for the detection of partial bleaching in quartz. Radiation Measurements 32, 5-6, 419–425.Google Scholar
Aitken, M.J., (1985). Thermoluminescence Dating. Academic Press, New York. Google Scholar
Aitken, M.J., Bowman, S.G.E., (1975). Thermoluminescent dating: assessment of alpha particle contribution. Archaeometry 17, 132–138.Google Scholar
Ashley, G.M., Smith, N.D., (1985). Proglacial Lacustrine Environment. Ashley, G.M., Shaw, J., Smith, N.D., Glacial Sedimentary Environments: Short Course 16. Society of Economic Paleontologists and Mineralogists, 135–216.Google Scholar
Autio, R.J., (1990). Stratigraphy and geomorphology of the sediments of glacial lakes Quincy, Eminence, and Alaska, west-central Indiana. Masters Thesis, Indiana University, Bloomington, , Indiana. Google Scholar
Banerjee, D., (2001). Supralinearity and sensitivity changes in optically stimulated luminescence of annealed quartz. Radiation Measurements 33, 47–57.Google Scholar
Berger, G.W., Mulhern, P.J., Huntley, D.H., (1980). Isolation of silt-sized quartz from sediments. Ancient TL 18, 7–11.Google Scholar
Bleuer, N.K., (1991). The Lafayette bedrock valley system of Indiana; concept, form and fill stratigraphy. In: Melhorn, W.N, Kempton, J.P., (Eds.), Geology and Hhydrology of the Teays-Mahomet Bedrock Valley System . Geological Society of America Special Paper 258, 51-78.Google Scholar
Brodzikowski, K., van Loon, A.J., (1991). Glacigenic Sediments. Elsevier Science Publishing Company, Inc., New York. Google Scholar
Brown, R.T., (1884). Geology of Morgan County. In: Collett, J., (Ed.), Indiana Department of Geology and Natural History; Thirteenth Annual Report, Indiana Department of Natural History, Indianapolis, 71-85.Google Scholar
Bulur, E., B"tter-Jensen, L., Murray, A.S., (2000). Optically stimulated luminescence from quartz using linear modulation technique. Radiation Measurements 32, 5-6, 407–411.Google Scholar
Clark, P.U., (1992). Surface form of the Southern Laurentide ice sheet and its implications to ice sheet dynamics. Geological Society of America Bulletin 104, 595–605.Google Scholar
Collett, J., (1876). The Geology of Owen County. In: Cox, E.T, (Ed.), Indiana Department of Geology and Natural History, Seventh Annual Report, Geological Survey of Indiana, Indianapolis, pp. 301–360.Google Scholar
Curry, B.B., (1989). Absence of Altonian glaciation in Illinois. Quaternary Research 31, 1–13.Google Scholar
Curry, B.B., Pavich, M.J., (1996). Absence of glaciation in Illinois during marine isotope stages 3 through 5. Quaternary Research 46, 19–26.Google Scholar
Donnelly, R., Harris, C., (1989). Sedimentology and origin of deposits from a small ice-dammed lake, Leirbreen, Norway. Sedimentology 36, 581–600.Google Scholar
Flint, R.F., (1971). Glacial and Quaternary Geology. John Wiley and Sons, New York. Google Scholar
Follmer, L.R., (1983). Sangamon soil and Wisconsinan pedogenesis in the midwestern United States. Porter, S.C., Late-Quaternary Environments of the United States: The Pleistocene. University of Minnesota Press, Minneapolis., 138–144.Google Scholar
Follmer, L.R., (1996). Loess studies in the central United States: evolution of concepts. Engineering Geology 45, 287–304.Google Scholar
Forman, S.L., Pierson, J., (2002). Late Pleistocene luminescence chronology of loess deposition in the Missouri and Mississippi river valleys, United States. Palaeogeography, Palaeoclimatology, Palaeoecology 186, 25–46.Google Scholar
Frye, J.C., (1968). Development of Pleistocene stratigraphy in Illinois. In: Bergstrom, R.E., (Ed.), The Quaternary of Illinois . University of Illinois and Illinois State Geological Survey, pp. 3-10.Google Scholar
Frye, J.C., Willman, H.B., Black, R.F., (1965). Outline of Glacial Geology of Illinois and Wisconsin. Wright, H.E., Frey, D.G., The Quaternary of the United States. Princeton University Press, Princeton., 43–61.Google Scholar
Fullerton, D.S., (1996). Stratigraphy and correlation of glacial deposits from Indiana to New York and New Jersey. Quaternary Science Reviews 5, 23–37.Google Scholar
Godfrey-Smith, D.I., Huntley, D.J., Chen, W.H., (1988). Optical dating studies of quartz and feldspar sediment extracts. Quaternary Science Reviews 7, 373–380.Google Scholar
Gray, H.H., (1988). Relict Drainageways Associated with the Glacial Boundary in Southern Indiana. Department of Natural Resources - Geological Survey, Bloomington pp 9.Google Scholar
Grimley, D.A., (2000). Glacial and nonglacial sediment contributions to Wisconsin Episode loess in the central United States. Geological Society of America Bulletin 112, 10, 1475–1495.Google Scholar
Hall, R.D., Anderson, A.K., (2000). Comparative soil development of quaternary paleosols of the central United States. Palaeogeography Palaeoclimatology Palaeoecology 158, 109–145.Google Scholar
Hall, R.D., Anderson, A.K., (2001). Quaterary record at Cagles Mill, Putnam County, Indiana. Proceedings of the Indiana Academy of Science 110, 9–22.Google Scholar
Harrison, S.S., (1975). Turbidite Origin of Glaciolacustrine Sediments, Woodcock Lake, Pennsylvania. Journal of Sedimentary Petrology 45, 738–744.Google Scholar
Hooyer, T.S., Iverson, N.R., (2002). Flow mechanism of the Des Moines lobe of the Laurentide ice sheet. Journal of Glaciology 48, 575–586.Google Scholar
Jacobs, P.M., (1994). Stratigraphy, Landscape Evolution, and a Pleistocene Buried Soil lithosequence in the Flatwoods Region of Owen and Monroe Counties, Indiana. Ph.D. Thesis, University of Wisconsin-Madison, . Google Scholar
Jain, M., Botter-Jensen, L., Singhvi, A.K., (2003). Dose evaluation using multiple-aliquot quartz OSL: test of methods and a new protocol for improved accuracy and precision. Radiation Measurements 37, 67–80.Google Scholar
Jennings, C.E., Aber, J.S., Balco, G., Barendregt, R., Bierman, P.R., Rovey, C.W., Thorleifson, L.H., Mason, J.A., (2007). Mid-quaternary in North America. Elias, S.A., Encyclopedia of Quaternary Sciences. Elsevier, Amsterdam., 1044–1051.Google Scholar
Johnson, W.H., (1986). Stratigraphy and correlation of the glacial deposits of the Lake Michigan Lobe prior to 15 ka BP. Sibrava, V., Bowen, D.Q., Richmond, G.M., Quaternary Glaciations in the Northern Hemisphere. Pergamon Press, New York., 17–22.Google Scholar
Joyce, E.J., Tjalsma, L.R.C., Prutzman, J.M., (1993). North American glacial meltwater history for the past 2.3 m.y.: oxygen isotope evidence from the Gulf of Mexico. Geology 21, 483–486.Google Scholar
Kr"ger, J., Kjaer, K.H., (1999). A data chart for field description and genetic interpretation of glacial diamicts and associated sediments " with examples from Greenland, Iceland, and Denmark. Boreas 28, 386–402.Google Scholar
Lawson, D.E., (1979). Sedimentological analysis of the western terminus region of the Matanuska Glaciaer, Alaska. US Army Cold Regions Research and Engineering Laboratory, Hanover., 122.Google Scholar
Leverett, F., (1898). The weathered zone (Yarmouth) between the Illinoian and Kansan till sheets. Journal of Geology 6, 238–243.Google Scholar
Lowell, T.V, Hayward, R.K, Denton, G.H., (1999). Role of Climate oscillations in determing ice-margin position: Hypothesis, examples and implications. In: Mickelson, D. M, Attig, J.W., (Eds.), Special Paper 337: Glacial Processes Past and Present . Geological Society of America, Denver., pp193-203.Google Scholar
Maat, P.B., Johnson, W.C., (1996). Thermoluminescence and new C-14 age estimates for late Quaternary loesses in southwestern Nebraska. Geomorphology 17, 115–128.Google Scholar
Malott, C.A., (1922). The physiography of Indiana. Logan, W.N., Cumings, E.R., Malott, C.A., Visher, S.S., Tucker, W.M., Reeves, J.R, Handbook of Indiana geology. Indiana Department of Conservation Publication, Indianapolis., 210–211.Google Scholar
Malott, C.A., (1926). The Glacial Boundary in Indiana. The Proceedings of the Indiana Academy of Science 35, 93–107.Google Scholar
Markewich, H.W., Wysocki, D.A., Pavich, M.J., Rutledge, E.M., Millard, H.T., Rich, F.J., Maat, P.B., Rubin, M., McGeehin, J.P., (1998). Paleopedology plus TL, 10Be, and 14C dating as tools in stratigraphic and paleoclimatic investigations, Mississippi River Valley, U.S.A. Quaternary International 51-52 143–167.Google Scholar
McGrain, P., (1949). Geological features of the proposed Cagle's Mill flood control reservoir. The Proceedings of the Indiana Academy of Science 58, 163–172.Google Scholar
McKay, D.E., Berg, R.C., (2008). Optical ages spanning two glacial-interglacial cycles from deposits of the Ancient Mississippi River, north-central Illinois. Geological Society of America Abstracts and Programs 40, 5, 78.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, 497–500.Google Scholar
Rendell, H.M., Webster, S.E., Sheffer, N.L., (1994). Underwater bleaching of signals form sediment grains: new experimental data. Quaternary Science Reviews 13, 433–435.Google Scholar
Richardson, C.A., (1994). Effects of bleaching on the sensitivity to dose of the infrared-stimulated luminescence of potassium-rich feldspars from Ynyslas, Wales. Radiation Measurements 23, 587–591.Google Scholar
Roberts, H.M., (2007). Assessing the effectiveness of the double-SAR protocol in isolating a luminescence signal dominated by quartz. Radiation Measurements 42, 1627–1636.Google Scholar
Roberts, H.M., Wintle, A.G., Maher, B.A., Hu, M.Y., (2001). Holocene sediment-accumulation rates in the western Loess Plateau, China, and a 2500-year record of agricultural activity, revealed by OSL dating. Holocene 11, 477–483.Google Scholar
Rohling, E.J., Fenton, M., Jorissen, F.J., Bertrand, P., Ganssen, G., Caulet, J.P., (1998). Magnitudes of sea-level lowstands of the past 500,000 years. Nature 394, 162–165.Google Scholar
Rodbell, D.T., Forman, S.L., Pierson, J., Lynn, W.C., (1997). Stratigraphy and chronology of Mississippi Valley loess in western Tennessee. Geological Society of America Bulletin 109, 1134–1148.Google Scholar
Ruhe, R.V., (1969). Quaternary Landscapes in Iowa. Iowa State University Press, Ames, Iowa. Google Scholar
Sanderson, D.C.W., Bishop, P., Stark, M., Alexander, S., Penny, D., (2007). Luminescence dating of canal sediments from Angkor Borei, Mekong Delta, southern Cambodia. Quaternary Geochronology 2, 322–329.Google Scholar
Singarayer, J.S., Bailey, R.M., (2003). Further investigations of the quartz optically stimulated luminescence components using linear modulation. Radiation Measurements 37, 451–458.Google Scholar
Stiff, B.J., Hansel, A.K., (2004). Quaternary Glaciations in Illinois. Ehlers, J., Gibbard, P.L., Developments in Quaternary Science: Quaternary Glaciations-Extent and Chronology: Part II. North America. Elsevier, Amsterdam., 71–82.Google Scholar
Syverson, K.M., (1998). Sediment record of short-lived ice-contact lakes, Burroughs Glacier, Alaska. Boreas 27, 44–54.Google Scholar
Thornbury, W. D., (1936). Glacial geology of southern and south-central Indiana. Ph.D Dissertation, Indiana University, Bloomington, Indiana.Google Scholar
Thornbury, W.D., (1940). Glacial lakes quincy and eminence. Indiana Academy of Sciences Proceedings 49, 131–144.Google Scholar
Thornbury, W.D., (1950). Glacial Sluiceways and Lacustrine Plains of Southern Indiana. Indiana Department of Conservation " Division of Geology, Bloomington., 21.Google Scholar
Tripsanas, E.K., Bryant, W.R., Slowey, N.C., Bouma, A.H., Karageorgis, A.P., Berti, D., (2007). Sedimentological history of Bryant Canyon area, northwest Grulf of Mexico, during the last 135 kyr (Marine Isotope Stages 1"6): a proxy record of Mississippi River discharge. Palaeogeography Palaeoclimatology Palaeoecology 246, 1, 137–161.Google Scholar
Wang, H., Lundstrom, C.C., Zhang, Z., Grimley, D.A., Balsam, W.L., (2009). A mid-late quaternary loess-paleosol record in Simmons Farm in southern Illinois, USA. Quaternary Science Reviews 28, 93–106.CrossRefGoogle Scholar
Wayne, W. J., (1963). "Pleistocene formation in Indiana.". Indiana Department of Conservation Geological Survey, Bloomington, Indiana., 85pp.Google Scholar
Willman, H. B, Frye, J. C., (1970). Pleistocene Stratigraphy of Illinois. Illinois State Geological Survey, Champaign., pp 204.Google Scholar
Wintle, A.G., (1997). Luminescence dating: laboratory procedures and protocols. Radiation Measurements 27, 769–817.Google Scholar
Wintle, A.G., Murray, A.S., (2000). Quartz OSL: effects of thermal treatment and their relevance to laboratory dating procedures. Radiation Measurements 32, 387–400.Google Scholar
Wood, J.R., Forman, S.L., Everton, D.W., (2007). The extent and timing of a pre-late Wisconsinan ice margin in central Indiana; a new view from glacial-lacustrine sediments from Porter Cave (abstract). Journal of Cave and Karst Studies 69, 369.Google Scholar