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A New Tree-Ring Width, δ 13 C and 14 C Investigation of the Two Creeks Site

Bibliographic Data

ID9241964
AuthorsSteven W Leavitt (0000-0002-7291-208X), Robert M Kalin (0000-0003-3768-3848)
Year1992
Volume34
Issue3
Pages792-797
Publication date1992-01-01
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200064092
OpenAlexW2504506216
LanguageEN
Citations received8
References cited13

We have made isotopic and dendrochronologic measurements on material collected from the Two Creeks site. Radiocarbon dating of outside wood of four logs yielded an average age of 11,760 ± 100 BP, in good agreement with results of Broecker and Farrand (1963) over 25 years ago. The range of 11,640 ± 160 to 11,900 ± 160 BP suggests a period of forest growth of 200–300 years, consistent with a ring-width chronology established by Kaiser (1987). Ring counting of five specimens gave a range of individual tree ages from 110 to 182 years, and width measurements indicate very low year-to-year variation in ring size. However, preliminary cross-dating of five samples produced a 202-year floating chronology. Stable-carbon isotope chronologies on cellulose from five-year ring groups show δ 13 C scatter among trees typical of that found within modern sites, with some matches of isotopic maxima and minima. Some downward δ 13 C trends may result from physiological response to rising lake levels (and/or cooling temperatures) at the site, which also produced very narrow rings in the outer ca. 50 ± 20 years

Absolute dating · Archaeology · Chronology · Dendrochronology · Dendroclimatology · Geography · Isotope · Isotopes of carbon · Nuclear physics · Physical geography · Physics · Radiocarbon dating · Stable isotope ratio · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Tree-ring climate responses · Geology · Paleontology

  • Two Creeks Interstade Dated through Dendrochronology and AMS

    Open Access•Klaus Félix Kaiser•Quaternary Research•1994

  • The Late Glacial Advance of the James Lobe, South Dakota, Suggests Climate-Driven Laurentide Ice Sheet Behavior

    Open Access•Stephanie Heath, Thomas V Lowell•Quaternary•2025

  • A plausible hydrological scenario for the Bølling-Allerød atmospheric methane increase

    Open Access•Robert M Kalin, John L Jirikowic•The Holocene•1996

  • Radiocarbon “Wiggles” in Great Lakes Wood at About 10,000 to 12,000 BP

    Open Access•Steven W Leavitt, Irina P Panyushkina et al.•Radiocarbon•2007

  • Tree-Ring Records of Near-Younger Dryas Time in Central North America—Preliminary Results from the Lincoln Quarry Site, Central Illinois, Usa

    Open Access•Irina P Panyushkina, Steven W Leavitt et al.•Radiocarbon•2004

  • Climate in the Great Lakes Region Between 14,000 and 4000 Years Ago from Isotopic Composition of Conifer Wood

    Open Access•Steven W Leavitt, Irina P Panyushkina et al.•Radiocarbon•2006

  • Δ 13 C Variations in C 3 Plants Over the Past 50,000 Years

    Open Access•S W Leavitt, S R Danzer•Radiocarbon•1992

  • Six Decades of Radiocarbon Dating in New World Archaeology

    Open Access•R E Taylor•Radiocarbon•2009

  • The Fossil Coleoptera of the Two Creeks forest Bed, Wisconsin

    Open Access•Alan V Morgan, Anne Morgan•Quaternary Research•1979

  • Climatic, Solar, Oceanic, and Geomagnetic Influences on Late-Glacial and Holocene Atmospheric 14 C/ 12 C Change

    Open Access•Minze Stuiver, Thomas F Braziunas et al.•Quaternary Research•1991

  • A Suggested Quality Assurance Protocol for Radiocarbon Dating Laboratories

    Open Access•Austin Long, Robert M Kalin•Radiocarbon•1990

Citations per year0.24
Citation span1992 - 2025 (34)
Highly citedNo

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