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Chronology of advance and recession dynamics of the southern Green Bay Lobe of the Laurentide Ice Sheet, south-central Wisconsin, USA

Published online by Cambridge University Press:  25 March 2020

Eric C. Carson Open the ORCID record for Eric C. Carson [Opens in a new window] ,
John W. Attig ,
J. Elmo Rawling III ,
Paul R. Hanson  and
Stefanie E. Dodge
Eric C. Carson*
Affiliation:
Wisconsin Geological and Natural History Survey, University of Wisconsin–Madison, Madison, Wisconsin53705, USA
John W. Attig
Affiliation:
Wisconsin Geological and Natural History Survey, University of Wisconsin–Madison, Madison, Wisconsin53705, USA
J. Elmo Rawling III
Affiliation:
Wisconsin Geological and Natural History Survey, University of Wisconsin–Madison, Madison, Wisconsin53705, USA
Paul R. Hanson
Affiliation:
Conservation and Survey Division, School of Natural Resources, University of Nebraska–Lincoln, Lincoln, NE68583, USA
Stefanie E. Dodge
Affiliation:
Wisconsin Geological and Natural History Survey, University of Wisconsin–Madison, Madison, Wisconsin53705, USA
*
*Corresponding author e-mail address: eric.carson@wisc.edu (E.C. Carson).
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Abstract

We used a combination of accelerator mass spectrometry (AMS) radiocarbon dating, optically stimulated luminescence (OSL) age estimates, and stratigraphic data from cores collected along the southern margin of the Green Bay Lobe (GBL) of the Laurentide Ice Sheet to provide new information on the timing and dynamics of the end of advance of the GBL and the dynamics of the ice sheet while very near its maximum position. Coring at multiple sites along the margin of the GBL indicate that ice had reached a stable position near its maximum extent by 24.7 ka; that ice advanced several kilometers to the Marine Isotope Stage 2 maximum position sometime shortly after 21.2 ka; and that ice remained at or beyond that position through the time interval represented by an OSL age estimate of 19.2 ± 3.2 ka. The timeline developed from these chronological data is internally consistent with, and further refines, AMS radiocarbon ages and OSL age estimates previously published for the southern margin of the GBL. It also provides new chronological control on the expansion of the GBL from its late Marine Isotope Stage (MIS) 3 extent to its MIS 2 maximum.

Keywords

Green Bay LobeLaurentide Ice SheetchronologyMIS 2Devils Lake
Type
Research Article
Information
Quaternary Research , Volume 95 , May 2020 , pp. 142 - 153
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2020

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References

REFERENCES

Aitken, M.J., 1998. An Introduction to Optical Dating: The Dating of Quaternary Sediments by the Use of Photon-stimulated Luminescence. Oxford University Press, Oxford.Google Scholar
Alden, W.C., 1918. Quaternary Geology of South-Eastern Wisconsin. U.S. Geological Survey Professional Paper 106. U.S. Government Printing Office, Washington, DC.Google Scholar
Attig, J.W., Clayton, L., Mickelson, D.M., 1985. Correlation of late Wisconsin glacial phases in the western Great Lakes area. Geological Society of America Bulletin 96, 1585–1593.2.0.CO;2>CrossRefGoogle Scholar
Attig, J.W., Hanson, P.R., Rawling, J.E. III, Young, A.R., Carson, E.C., 2011. Optical ages indicate the southwestern margin of the Green Bay Lobe in Wisconsin, USA, was at its maximum extent until about 18,500 years ago. Geomorphology 130, 384–390.CrossRefGoogle Scholar
Attig, J.W., Mickelson, D.M., Clayton, L., 1989. Late Wisconsin landforms and glacier-bed conditions in Wisconsin. Sedimentary Geology 62, 399–405.CrossRefGoogle Scholar
Batchelor, C.J., Orland, I.J., Marcott, S.A., Slaughter, R., Edwards, R.L., Zhang, P., Li, X., Cheng, H., 2019. Distinct permafrost conditions across the last two glacial periods in mid-latitude North America. Geophysical Research Letters 46, 13318–13326.CrossRefGoogle Scholar
Carlson, A.E., Tarasov, L., Pico, T., 2018. Rapid Laurentide ice-sheet advance towards southern Last Glacial Maximum limit during marine isotope stage 3. Quaternary Science Reviews 196, 118–123.CrossRefGoogle Scholar
Carson, E.C., Hanson, P.R., Attig, J.W., Young, A.R., 2012a. Numeric control on the late-glacial chronology of the southern Laurentide Ice Sheet derived from ice-proximal lacustrine deposits. Quaternary Research 78, 583–589.CrossRefGoogle Scholar
Carson, E.C., Hanson, P.R., Attig, J.W., Young, A.R., 2012b. Refining the late glacial chronology of the Green Bay Lobe of the Laurentide Ice Sheet using ice-marginal lacustrine sediments. Geological Society of America, Abstracts with Programs 44, 454.Google Scholar
Ceperley, E.G., Marcott, S.A., Rawling, J.E. III, Zoet, L.K., Zimmerman, S.R.H., 2019. The role of permafrost on the morphology of an MIS 3 moraine from the southern Laurentide Ice Sheet, Geology 47, 440–444.CrossRefGoogle Scholar
Chamberlin, T.C., 1883. General Geology of Wisconsin. Geology of Wisconsin 1. The Commissioners of Public Printing, Madison, WI.Google Scholar
Clark, P.U., Hostetler, S.W., Pisias, N.G., Schmittner, A., Meissner, K.J., 2007. Mechanisms for an 7-kyr climate and sea-level oscillation during marine isotope stage 3. In: Schmittner, A., Chang, J.C.H., Hemming, S.R., (Eds.), Ocean Circulation: Mechanisms and Impacts—Past and Future Changes of Meridional Overturning. American Geophysical Union Geophysical Monographs 173. Wiley, New York, p. 209.CrossRefGoogle Scholar
Clayton, L., Attig, J.W., 1989. Glacial Lake Wisconsin. Geological Society of America Memoir 173. Geological Society of America, Boulder, CO.CrossRefGoogle Scholar
Clayton, L., Attig, J.W., 1990. Geology of Sauk County, Wisconsin. Wisconsin Geological and Natural History Survey Information Circular 67. Division of Extension, University of Wisconsin–Madison, Madison.Google Scholar
Clayton, L., Attig, J.W., 1997. Pleistocene Geology of Dane County, Wisconsin. Wisconsin Geological and Natural History Survey Bulletin 95. Division of Extension, University of Wisconsin–Madison, Madison.Google Scholar
Clayton, L., Attig, J.W., Mickelson, D.M., 2001. Effects of late Pleistocene permafrost on the landscapes of Wisconsin, USA. Boreas 30, 173–188.CrossRefGoogle Scholar
Clayton, L., Moran, S.R., 1982, Chronology of late Wisconsinan glaciation in middle North America. Quaternary Science Reviews, 1, 55–82.CrossRefGoogle Scholar
Cline, D.R., 1965. Geology and Ground-Water Resources of Dane County, Wisconsin. U.S. Geological Survey Water-Supply Paper 1779-U. U.S. Government Printing Office, Washington, DC.Google Scholar
Curry, B.B., Lowell, T.V., Wang, H., Anderson, A.C., 2018. Revised time-distance diagram for the Lake Michigan Lobe, Michigan Subepisode, Wisconsin Episode, Illinois, USA. In: Kehew, A.E., Curry, B.B. (Eds.), Quaternary Glaciation of the Great Lakes Region: Process, Landforms, Sediments, and Chronology. Geological Society of America Special Paper 530. Geological Society of America, Boulder, CO, pp. 69–101.Google Scholar
Dalton, A.S., Finkelstein, S.A., Barnett, P.J., Forman, S.L., 2016. Constraining the late Pleistocene history of the Laurentide Ice Sheet by dating the Missinaibi Formation, Hudson Bay Lowlands, Canada. Quaternary Science Reviews 146, 288–299.CrossRefGoogle Scholar
Dalziel, I.W.D. and Dott, R.H. Jr., 1970. Geology of the Baraboo District, Wisconsin. Wisconsin Geological and Natural History Survey Information Circular 14. Division of Extension, University of Wisconsin–Madison, Madison.Google Scholar
Heath, S.L., Loope, H.M., Curry, B.B., Lowell, T.V., 2018. Pattern of southern Laurentide Ice Sheet margin position changes during Heinrich Stadials 2 and 1. Quaternary Science Reviews 201, 362–379.CrossRefGoogle 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 Jimmium rock shelter, northern Australia Part I, experimental design and statistical models. Archaeometry, 41, 339–364.CrossRefGoogle Scholar
King, G.E., Robinson, R.A.J., Finch, A.A., 2014. Towards successful OSL sampling strategies in glacial environments; deciphering the influence of depositional processes on bleaching of modern glacial sediments from Jostedalen, southern Norway. Quaternary Science Reviews 89, 94–107.CrossRefGoogle Scholar
Knox, J.C., 2019. Geology of the Driftless Area. In: Carson, E.C., Rawling, J.E III, Daniels, J.M., Attig, J.W. (Eds.), The Physical Geography and Geology of the Driftless Area: The Career and Contributions of James C. Knox. Geological Society of America Special Paper 543. Geological Society of America, Boulder, CO, pp. 1–35.Google Scholar
Konert, M., Vandenberghe, J., 1997. Comparison of laser grain size analysis with pipette and sieve analysis: a solution for the underestimation of the clay fraction. Sedimentology 44, 523–535.CrossRefGoogle Scholar
Lundqvist, J., Clayton, L., Mickelson, D.M., 1993. Deposition of the late Wisconsin Johnstown moraine, south-central Wisconsin. Quaternary International 18, 53–59.CrossRefGoogle Scholar
Maher, L.J. Jr., Mickelson, D.M., 1996, Palynological and radiocarbon evidence for deglaciation events in the Green Bay Lobe, Wisconsin. Quaternary Research, 46, 119–135.CrossRefGoogle Scholar
Martin, L.M., 1932. The Physical Geography of Wisconsin. Wisconsin Geological and Natural History Survey Bulletin 36. University of Wisconsin Press, Madison.Google Scholar
Medaris, L.G. Jr., Singer, B.S., Dott, R.H. Jr., Naymark, A., Johnson, C.M., Schott, R.C., 2003. Late Paleoproterozoic climate, tectonics, and metamorphism in the southern Lake Superior Region and proto-North America: evidence from the Baraboo interval quartzites. Journal of Geology 111, 243–257.CrossRefGoogle Scholar
Mickelson, D.M., Knox, J.C., Clayton, L., 1982. Glaciation of the Driftless Area: an evaluation of the evidence. Wisconsin Geological and Natural History Survey Field Trip Guidebook 5, 155–170.Google Scholar
Miller, B.A., Schaetzl, R.J., 2012. Precision of soil particle size analysis using laser diffractometry. Soil Science Society of America Journal 76, 1719–1727.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32, 57–73.CrossRefGoogle Scholar
Olcott, P.G., 1972. Bedrock Topography of Dane County. Wisconsin Geological and Natural History Survey Open-File Report 72–3, Scale 1:62,500. Division of Extension, University of Wisconsin–Madison, Madison.Google Scholar
Pico, T., Mitrovica, J.X., Ferrier, K.L., Braun, J., 2016. Global ice volume during MIS 3 inferred from a sea-level analysis of sedimentary core records in the Yellow River Delta. Quaternary Science Reviews 152, 72–79.CrossRefGoogle Scholar
Pico, T., Creveling, J.R., Mitrovica, J.X., 2017. Sea- level records from the US mid-Atlantic constrain Laurentide Ice Sheet extent during marine isotope stage 3. Nature Communications 8, 15612.CrossRefGoogle 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.CrossRefGoogle Scholar
Salisbury, R.D., Atwood, W.W., 1900. The Geography of the Region about Devils Lake and the Dalles of Wisconsin, with Some Notes on Its Surface Geology. Wisconsin Geological and Natural History Survey Bulletin 5. Division of Extension, University of Wisconsin–Madison, MadisonGoogle Scholar
Schaetzl, R.J., Lepper, K., Thomas, S.E., Grove, L., Treiber, L., Farmer, A., Fillmore, A. et al., 2017. Kame deltas provide evidence for a new glacial lake and suggest early glacial retreat from central Lower Michigan, USA. Geomorphology 280, 167–178.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., Reimer, R.W., 2019. CALIB 7. 1 [WWW program], (accessed October 15, 2019) http://calib.org.Google Scholar
Syverson, K.M., Colgan, P.M., 2011. The Quaternary of Wisconsin: an updated review of stratigraphy, glacial history and landforms. In: Ehlers, J., Gibbard, P.L., Hughes, P.D. (Eds.), Quaternary Glaciations—Extent and Chronology: A Closer Look. Elsevier, Amsterdam, pp. 537–552.CrossRefGoogle Scholar
Trowbridge, A.C., 1917. The history of Devils Lake, Wisconsin. Journal of Geology 25, 344–372.CrossRefGoogle Scholar
Ullman, D.J., Carlson, A.E., LeGrande, A.N., Anslow, F.S., Moore, A.K., Caffee, M., Syverson, K.M., Licciardi, J.M., 2014. Southern Laurentide ice-sheet retreat synchronous with rising boreal summer insolation. Geology 43, 23–26.CrossRefGoogle Scholar
Warren, G.K., 1874. Water communication between the Mississippi River and Lake Michigan: representation of surveys made in 1867–’68–’69; their object and extent; maps and diagrams constructed from measurements; tables of hydraulic data; anomalous physical features considered, and referred to a generalization of similar exhibitions elsewhere. 44th Congress, 1st Session, Senate Executive Document 28, Washington, DC, 60–89.Google Scholar
Wen, B., Aydin, A., Duzgoren-Aydin, N., 2002. A comparative study of particle size analyses by sieve-hydrometer and laser diffraction methods. Geotechnical Testing Journal 25, 434–442.Google Scholar
Wintle, A.G., Murray, A.S., 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41, 369–391.CrossRefGoogle Scholar
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