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Yellowstone's Northern Range - Greater Yellowstone Science ...

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PREHISTORIC AND EARLY HISTORIC SETTING<br />

29<br />

or failure of a given group of hunters today proves<br />

that the game is present or absent. The key<br />

information is the positive evidence provided by<br />

those who saw animals. There were many such<br />

people in <strong>Yellowstone</strong>, and they left many reports<br />

of abundant elk and other wildlife.<br />

CONCLUSIONS<br />

<strong><strong>Yellowstone</strong>'s</strong> long-term climatic record<br />

suggests that the native plant and animal communities<br />

are dynamic and respond to changing environmental<br />

conditions. The paleontological, archeological,<br />

and historical records, though they have<br />

important limitations that must be recognized,<br />

combine to suggest that these plant and animal<br />

communities, though they have been affected by<br />

these changes in climate, are quite resilient.<br />

Relatively few species, in fact, very few, are<br />

elintinated by the variations that the park area has<br />

experienced over the past 10,000 years. The<br />

region's biodiversity, then, seems to hold up well,<br />

but specific biodiversity issues will be discussed<br />

later in this report.<br />

The paleontological, archeological, and<br />

historical evidence provides a picture of pre-I 872<br />

<strong>Yellowstone</strong> as a place continuously inhabited by<br />

essentially the same wildlife community as today.<br />

These three lines of evidence provide abundant<br />

proof that today's native ungulates and their<br />

predators were common residents of the park area<br />

for thousands of years, and provide equally strong<br />

proof that humans were an active part of this<br />

setting for nearly as long.<br />

It is again important to point out, however,<br />

that the paleontological, archeological, and<br />

historical evidence does not pennit us to make<br />

precise estimates of wildlife population sizes.<br />

Though the historical record suggests that large<br />

animals were common, we cannot yet use this<br />

material to prove that they were more common, as<br />

common, or less common than today. In fact, they<br />

may have been less common then than now, simply<br />

because of different environmental conditions.<br />

The period 1800-1872 represented the end (and the<br />

most severe years) of an extended cold and wet<br />

period (circa 1500-1850) known as the Little Ice<br />

Age. If the Little Ice Age resulted in deeper snows<br />

and harsher winters, then there were almost<br />

certainly fewer ungulates and predators wintering<br />

there then than now. Moreover, computer models<br />

suggest that the northern elk population size might<br />

be reduced from 8 to 20 percent when wolves are<br />

restored (Boyce 1990, 1993, 1995a; Garton et a!.<br />

1990; Mack and Singer 1992a, 1992b, 1993a,<br />

1993b); wolves were present prior to 1872, and<br />

presumably played an important role in elk<br />

population size then. Environmental conditions,<br />

including the influences of Native Americans,<br />

change over time; there is no specific date or<br />

period in the past that can serve us as a model for<br />

how the <strong>Yellowstone</strong> landscape should look today.<br />

The highest value of the prehistoric and early<br />

historical record of <strong>Yellowstone</strong> may be in showing<br />

us the range of past variations in that landscape.

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