The Pleistocene is a geological epoch that began about 2. The Holocenethe current geological epoch, begins about 11, years ago when the Pleistocene ends. Before the advent of radiocarbon dating, the fossilized trees had been dated by correlating sequences of annually deposited layers of sediment at Two Creeks with sequences in Scandinavia. This led to estimates that the trees were between 24, and 19, years old,  and hence this was taken to be the date of the last advance of the Wisconsin glaciation before its final retreat marked the end of the Pleistocene in North America. This result was uncalibrated, as the need for calibration of radiocarbon ages was not yet understood. Further results over the next decade supported an average date of 11, BP, with the results thought to be the most accurate averaging 11, BP.
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