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AMS Radiocarbon Age of the Upper Mississippi Valley Roxana Silt

Published online by Cambridge University Press:  20 January 2017

David S. Leigh  and
James C. Knox
David S. Leigh
Affiliation:
Department of Geography, University of Georgia, Athens, Georgia 30602
James C. Knox
Affiliation:
Department of Geography, University of Wisconsin, Madison, Wisconsin 53706
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Abstract

Accelerator mass spectrometer radiocarbon ages of the Roxana Silt (loess) along the Upper Mississippi Valley of Wisconsin and Minnesota indicate that loess sedimentation of the Roxana Silt occurred between about 55,000 and 27,000 14 C yr B.P. However, due to local environmental controls, the basal age at any given site may range from 55,000 to 35,000 14C yr B.P. The radiocarbon ages presented here are in agreement with previous radiocarbon ages for the Roxana Silt in its type area of west-central Illinois, but indicate that long-term sedimentation rates along the bluffline of the Upper Mississippi Valley were very slow (4-8 cm/1000 yr) compared to long-term sedimentation rates along the bluffline of the type area (40-70 cm/1000 yr). Comparison of radiocarbon ages for midcontinent middle Wisconsinan loess deposits indicates that sedimentation along the Mississippi River valley may have preceded loess sedimentation along the Missouri River valley by as much as 20,000 yr or that basal ages for middle Wisconsinan loess along the Missouri Valley are erroneously young. The bracketing ages for the Upper Mississippi Valley Roxana Silt indicate that the Mississippi River valley was receiving outwash sedimentation between 55,000 and 27,000 14C yr B.P.

Type
Articles
Information
Quaternary Research , Volume 39 , Issue 3 , May 1993 , pp. 282 - 289
Copyright
University of Washington

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