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Radiocarbon Analyses from Cincinnati, Ohio, and Their Implications for Glacial Stratigraphic Interpretations

Bibliographic Data

ID24088337
AuthorsThomas V Lowell (0000-0001-7826-0636, University of Cincinnati), Kevin M Savage (University of Cincinnati), C Scott Brockman (Ohio Department of Natural Resources), Robert Stuckenrath (University of Pittsburgh)
Year1990
Volume34
Issue1
Pages1-11
Publication date1990-07-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueQuaternary Research (JOURNAL)
Journal identifiersISSN: 0033-5894 • E-ISSN: 1096-0287
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1016/0033-5894(90)90068-v
OpenAlexW2047424731
LanguageEN
Citations received3
References cited14

Detailed analysis of a site near Cincinnati, Ohio, shows that 14 C ages of samples in a single geologic unit can have a range of several thousand years and ages from different stratigraphic units can overlap. At the Sharonville site, four 14 C samples from organic silt below glaciogenic deposits have an inverted chronologic sequence, suggesting contamination, but nevertheless they indicate the silt was deposited before 27,000 yr B.P. A stump cluster in growth position, wood fragments, and moss from the upper surface of the silt may differ by as much as 2300 14 C yr. Five ages from the stump cluster constrain the timing of a glacier advance of the Laurentide ice sheet to its southern limit in the Cincinnati area at 19,670 ± 68 yr B.P. Overlying glaciogenic sediments contain transported wood that may be as much as 3200 yr older than the advance. This range of ages points out that, for a given site, several age measurements are required to determine when a glacier advance occurred. Because the measured ages in this study span the entire interval suggested for a twofold sequence of advance, retreat, and readvance of the margin of the Miami sublobe, we suggest a single advance to its terminal position in the Cincinnati area as an alternate hypothesis for testing.

Archaeology · Chronology · Geography · Glacial period · Glacier · Physical geography · Radiocarbon dating · Range (aeronautics) · Sequence (biology) · Silt · Geology · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Paleontology · Pleistocene-Era Hominins and Archaeology

  • OSL ages on glaciofluvial sediment in northern Lower Michigan constrain expansion of the Laurentide ice sheet

    Open Access•Randall J Schaetzl, Steven L Forman•Quaternary Research•2008

  • Deglaciation, basin formation and post-glacial climate change from a regional network of sediment core sites in Ohio and eastern Indiana

    Open Access•Katherine Glover, Katherine C Glover et al.•Quaternary Research•2011

  • Robert Stuckenrath, 1927-1994

    Open Access•J M Adovasio•Radiocarbon•1995

  • Radiocarbon dating and the “old wood” problem

    Open Access•Michael Brian Schiffer•Journal of Archaeological Science•1986

  • The Unreliability of 14 C Dates Obtained from Buried Sandy Podzols

    Open Access•Mebus A Geyh, Günter Roeschmann et al.•Radiocarbon•1983

  • Soil Dating By Fractional Extraction of Humic Acid

    Open Access•Kunihiko Kigoshi, Nobuko Suzuki et al.•Radiocarbon•1980

  • Unreliability of 14 C Dates from Organic Matter of Soils

    Open Access•Nicole Gilet-Blein, Gerard Marien et al.•Radiocarbon•1980

  • Testing Contemporaneity and Averaging Radiocarbon Dates

    Open Access•Austin Long, Bruce E Rippeteau et al.•American Antiquity•1974

Unique citing works3
Citations per year0,1
Citation span1995 - 2011 (17)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 1
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