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Population Histories of Artiodactyls during the Holocene of Western North America: Archaeological Evidence and Implications for Management
Jack M. Broughton
A rich body of data bearing on the Holocene history of artiodactyl populations resides in archaeological and paleontological deposits distributed across western North America. Viewed from the perspective of foraging theory and combined with high-resolution paleoclimatic records and archaeological information on human demographic trends, these data suggest that artiodactyl populations experienced a series of dramatic long-term fluctuations over the last 10,000 years. During the early and middle Holocene (9,000 to 5,000 B.P.), artiodactyl populations in many areas were substantially depressed due to prevailing drought conditions. Human populations were negatively affected at these times as well, to judge from the paucity of archaeological remains dating to these periods. With the abrupt onset of moister conditions of the late Holocene (5000 to 3000 B.P.) and with human predator populations then low, artiodactyl populations expanded to reach record-high densities. However, in many settings, burgeoning human populations and hunting pressure ultimately overtook ungulate herds causing dramatic late Holocene population declines. After A.D. 1492, European-based diseases rapidly swept through many areas of the west causing dramatic declines in native hunters and ultimately irruptions of artiodactyl herds. These patterns suggest that Holocene artiodactyl populations have been limited by both climate-based deterioration of forage quality and human predation and have implications for the future management of mountain areas.


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