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Radiocarbon Dating of Buried Trees and Climate Change in West-Central Oklahoma

Published online by Cambridge University Press:  18 July 2016

Owen K. Davis
Affiliation:
Department of Geosciences, The University of Arizona Tucson, Arizona 85721 USA
Dai Kaimei
Affiliation:
Department of Physics, Nanjing University, Nanjing, China
Jeffrey S. Dean
Affiliation:
Laboratory of Tree-Ring Research, The University of Arizona, Tucson, Arizona 85721 USA
Jim Parks
Affiliation:
Laboratory of Tree-Ring Research, The University of Arizona, Tucson, Arizona 85721 USA
Robert M. Kalin
Affiliation:
Department of Civil Engineering, The Queen's University of Belfast, Belfast BT9 1NN Northern Ireland
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Abstract

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Eleven radiocarbon dates and tree-ring analyses of 3 juniper logs demonstrate the potential for 14C analysis of buried logs in the American Midwest. Three junipers (cf. Juniperus virginiana) were recovered from 9.20, 10.50, and 10.60 m in the fill of Carnegie Canyon, west-central Oklahoma. Their 14C ages are calibrated between 3300 and 2800 yr ago. A negative correlation of tree rings and ∆14C (p = 0.013) supports the findings of Schmidt and Gruhle (1988), who demonstrate the association of global cooling with reduced solar activity.

Type
IV. 14C as a Tracer of the Dynamic Carbon Cycle in the Current Environment
Copyright
Copyright © the Department of Geosciences, The University of Arizona 

References

Davis, O. K. 1992 Rapid climatic change in coastal southern California inferred from pollen analysis of San Joaquin marsh. Quaternary Research 37: 89100.CrossRefGoogle Scholar
Davis, O. K. 1994 The correlation of summer precipitation in the southwestern U.S.A. with isotopic records of solar activity during the Medieval Warm period. Climate Change 26: 271287.CrossRefGoogle Scholar
Eddy, J. A. 1967 The Maunder Minimum. Science 192: 11891202.CrossRefGoogle Scholar
Eddy, J. A. 1977 Climate and the changing sun. Climate Change 1: 173190.CrossRefGoogle Scholar
Hall, S. A. and Lintz, C. 1984 Buried trees, water table fluctuations, and 3000 years of changing climate in West-Central Oklahoma. Quaternary Research 22: 129133.CrossRefGoogle Scholar
Jirikowic, J. L., Kalin, R. M. and Davis, O. K. 1993 Tree-ring 14C as an indicator of climate change. In Climatic Change in Continental Isotopic Records. AGU Geophysical Monograph 78: 353366.Google Scholar
Lintz, C. and Hall, S. A. 1983 The geomorphology and archaeology of Carnegie Canyon, Ft. Cobb Laterals Watershed, Caddo Co., Oklahoma. Oklahoma Conservation Commission Archaeological Research Report 10: 220 p.Google Scholar
Long, A., Andresen, J. and Klein, J. 1987 Construction of the Casa Grande by sequential high precision C-14 dataing. Geoarchaeology 2: 217222.CrossRefGoogle Scholar
May, D. W. 1992 Late Holocene valley-bottom aggradation and erosion in the South Loop River Valley, Nebraska. Physical Geography 13: 115132.CrossRefGoogle Scholar
Meko, D. M., Stockton, C. W. and Biasing, T. J. 1985 Periodicity in tree rings from the corn belt. Science 229: 381384.CrossRefGoogle ScholarPubMed
Schmidt, B., and Gruhle, W. 1988 Klima Radiokohlenst-offgehalt und dendrochronologie. Naturwissenschaftliche Rundschau 41: 177182.Google Scholar
Stuiver, M. and Reimer, P. J. 1993 Extended 14C data base and revised CALIB 3.0 14C calibration program. In Stuiver, M., Long, A. and Kra, R. S., eds., Calibration 1993. Radiocarbon 35(1): 215230.CrossRefGoogle Scholar
Vries, H. L. de 1958 Variation in concentration of radiocarbon with time and location on Earth. Koninklijke Nederlandse Akademie van Wetenschappen B 61: 94102.Google Scholar