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.1998 Nov 24;95(24):14576-83.
doi: 10.1073/pnas.95.24.14576.

Paleoindian large mammal hunters on the plains of North America

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Paleoindian large mammal hunters on the plains of North America

G C Frison. Proc Natl Acad Sci U S A..

Abstract

From approximately 11,200 to 8,000 years ago, the Great Plains of North America were populated by small Paleoindian hunting groups with well developed weaponry and the expertise to successfully hunt large mammals, especially mammoths and bison. Mammoths became extinct on the Plains by 11,000 years ago, and, although paleoecological conditions were worsening, their demise may have been hastened by human predation. After this, the main target of the Plains Paleoindian hunters consisted of subspecies of bison, Bison antiquus and Bison occidentalis. As bison populations gradually diminished, apparently because of worsening ecological conditions, by approximately 8,000 years ago, human subsistence was forced into a greater dependence on small animal and plant foods. Human paleoecology studies of the Paleoindian time period rely heavily on multidisciplinary efforts. Geomorphologists, botanists, soil scientists, palynologists, biologists, and other specialists aid archaeologists in data recovery and analysis, although, with few exceptions, their contributions are derived from the fringes rather than the mainstream of their disciplines.

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Figures

Figure 1
Figure 1
Locations of Paleoindian sites referred to in the text. 1, Agate Basin; 2, Blackwater Draw; 3, Carter–Kerr/McGee; 4, Casper; 5, Cattle Guard; 6, Colby; 7, Cooper; 8, Dent; 9, Finley; 10, Fletcher; 11, Folsom; 12, Hell Gap; 13, Horner; 14, Hudson–Meng; 15, James Allen; 16, Jones–Miller; 17, Lange–Ferguson; 18, Lindenmeier; 19, Lipscomb; 20, Mill Iron; 21, Olsen–Chubbuck; 22, Plainview; 23, Scottsbluff.
Figure 2
Figure 2
Paleoindian cultural complexes and approximate time periods.
Figure 3
Figure 3
Paleoindian weaponry diagnostics. (a) Clovis. (b) Goshen. (c) Folsom. (d) Agate Basin. (e) Hell Gap. (f) Alberta. (g) Eden. (h) Scottsbluff.
Figure 4
Figure 4
Male (a) and female (b)B. antiquus skulls; male (c) and female (d) 6,500-year-old intermediate type bison skulls; male (e) and female (f)Bison bison skulls.
Figure 5
Figure 5
Artist’s misconception of bison jumping.
Figure 6
Figure 6
Excavating a 10,000-year-old bison bone bed at the Horner site.
Figure 7
Figure 7
Nearly complete bison skeletons after removal of unarticulated bones in Fig. 7.
Figure 8
Figure 8
Ten-thousand-year-old bison bone bed in the bottom of a parabolic sand dune at the Casper site.
Figure 9
Figure 9
Leeward view of present-day parabolic sand dune similar to the one originally used to trap bison at the Casper site. Dimensions are ≈30 m wide, 300 m long, and 12 m deep. Maximum slope of sides is ≈35 degrees.
Figure 10
Figure 10
Present-day arroyo headcut forming an ideal analog of a Paleoindian arroyo bison trap. Perpendicular clay wall is ≈4.5 m high.
Figure 11
Figure 11
Mammoth bone pile at the Colby kill site.
See this image and copyright information in PMC

References

    1. Adovasio J M, Pedler D R. Antiquity. 1997;71:573–580.
    1. Gore R. National Geographic. 1997;192:92–99.
    1. Martin P S, Wright H E, editors. Pleistocene Extinctions. New Haven, CT: Yale Univ. Press; 1967.
    1. Martin P S, Klein R G, editors. Quaternary Extinctions. Tucson, AZ: Univ. of Ariz. Press; 1984.
    1. Marshall L G. In: Quaternary Extinctions. Martin P S, Klein R G, editors. Tucson, AZ: Univ. of Ariz. Press; 1984. pp. 785–806.

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