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Buried trees,water table fluctuations,and 3000 years of changing climate in west-central Oklahoma
Authors:Stephen A Hall  Christopher Lintz
Institution:Department of Geography, North Texas State University, Denton, Texas 76203 USA;Department of Anthropology, University of Oklahoma, Norman, Oklahoma 73019 USA
Abstract:A sequence of radiocarbon-dated buried trees, buried soils, a carbonate zone, and a molluscan fauna from Carnegie Canyon indicate that between 3200 and 2600 yr B.P. the climate of west-central Oklahoma was drier than today. A high water table accompanied a period of moister climate 2000 to 1000 yr B.P. The water table dropped after 1000 yr B.P. due to a change toward dry conditions.
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