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Hypsithermal |
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One scenario is that the water table dropped at the beginning of the Hypsithermal between 9000-8000 ybp and that subsequent erosion resulted in the loss of the most recently deposited sediments. Fowler's toad, Bufo fowleri, the six-lined racerunner, Cnemidophorus sexlineatus, and the western slender glass lizard, Ophisaurus attenuatus) presumably entered the Calumet region during a hypsithermal interval (Smith & Minton 1957) about 6200 to 5050 ybp (Ahearn & Kapp 1984). |
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