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I <br /> 30 <br /> of mammoth and other extinct mammals. Such sites represent <br /> components of a hunting oriented lifeway that occurred globally <br /> during the late Pleistocene. <br /> By approximately 10, 500 years B.P. Clovis projectile points were <br /> replaced by a form indicative of the Folsom period. This <br /> technological change coincided with a shift away from primary <br /> dependence on mammoth to increased exploitation of Pleistocene <br /> bison (Bison antiauus) . The largest and most thoroughly inves- <br /> tigated Folsom occupation in northeastern Colorado is the Lin- <br /> denmeier site, located north-northeast of the Study Area in <br /> Larimer County. <br /> The majority of Paleo-Indian sites or components represent the <br /> Plano period, which began by ca. 9000 years B. P. This period <br /> includes several technologically related complexes, most notably <br /> Agate Basin, Hell Gap, and Cody. Increased exploitation of plant <br /> resources is indicated at one Plano period site in eastern <br /> Colorado (Wheat 1979) . Some researchers feel that a greater <br /> level of social organization is indicated at certain Plano period <br /> sites than at earlier Paleo-Indian occupations (Kalasz et al. <br /> 1992:26) . <br /> 2.2.2 Archaic Stage <br /> The Archaic Stage is divisible into Early, Middle, and Late <br /> periods. By approximately 7, OOO years B.P. cultural materials <br /> indicative of the Plano period of the Paleo-Indian stage began to <br /> be replaced by evidence of markedly different technological <br /> adaptations and subsistence strategies. During this time much of <br /> North America was affected by an accelerated continental warming <br /> trend, the Altithermal episode, which resulted in ecological <br /> changes. The lifeway that developed in response to these <br /> conditions during the Early Archaic period was characterized by <br /> increased dependence on small mammals and wild plants. A <br /> decrease in the exploitation of the plains region and increased <br /> utilization of foothills and montane environments is <br /> characteristic of this period. (Larson et al. 1992; Benedict and <br />