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Palynological and Radiocarbon Evidence for Deglaciation Events in the Green Bay Lobe, Wisconsin

Published online by Cambridge University Press:  20 January 2017

Louis J. Maher Jr.  and
David M. Mickelson
Louis J. Maher Jr.
Affiliation:
Department of Geology and Geophysics, University of Wisconsin—Madison, 1215 West Dayton St. Madison, Wisconsin, 53706
David M. Mickelson
Affiliation:
Department of Geology and Geophysics, University of Wisconsin—Madison, 1215 West Dayton St. Madison, Wisconsin, 53706
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Abstract

A new and significant site of organic silty sand has been found beneath the Valders till at Valders Quarry in northeastern Wisconsin. This is now the earliest known late-glacial site associated with red till ice advances in the western Great Lakes area. Leaves of terrestrial plants washed into a small depression provide a date of 12,965 ± 200 yr B.P. (WIS-2293), which is significantly older than the Two Creeks Forest Bed (ca. 11,800 yr B.P.). Percentage and concentration pollen diagrams suggest that the site was open and distant from a closed Picea forest. No wood or Picea needles have been found. This date is statistically indistinguishable from 12,550 ± 233 yr B.P., the mean of three dates for the end of inorganic varve sedimentation at Devils Lake, 160 km southwest at the terminus of the Green Bay Lobe. Assuming that the Green Bay lobe vacated its outermost moraine in the interval from 13,000 to 12,500 yr B.P., only a short time was available for retreat of the ice margin over 350 km, drainage of red sediment from Lake Superior into the Lake Michigan basin, readvance of over 250 km, retreat of at least 80 km, and advance to this site. The time for these events appears to have been too short to resolve by current radiocarbon technique. This extremely rapid collapse of the Green Bay lobe has a calibrated age of about 15,000 cal yr B.P., about that of the dramatic warming seen in the Greenland ice cores.

Type
Research Article
Information
Quaternary Research , Volume 46 , Issue 3 , November 1996 , pp. 251 - 259
Copyright
University of Washington

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