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Last modified
7/14/2009 5:02:32 PM
Creation date
5/22/2009 5:33:12 PM
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UCREFRP
UCREFRP Catalog Number
8097
Author
American Fisheries Society.
Title
Proceedings of the 18th Annual Meeting, Colorado - Wyoming Chapter, American Fisheries Society.
USFW Year
1983.
USFW - Doc Type
March 2-3, 1983.
Copyright Material
NO
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<br />RELATIONSHIP OF BEAVER TO OTHER RESOURCES <br /> <br />Wildlife <br /> <br />Beaver ponds and associated flooding and high water tables create <br />habitat diversity, edge effect, and vegetative changes that attract wild- <br />life species that are not often found in other areas of the forest. Water- <br />fowl, shorebirds, and songbirds that feed over open water are commonly <br />attracted to flooded areas (Neff, 1957). On the Lolo National Forest in <br />western Montana, American reds tarts (Setophaga ruticilla) were found to in- <br />habit flooded habitats disproportionately than other streamside areas (M. <br />Hillis, personal communication). Furbearer populations, such as mink, <br />muskrat, and otter are also attracted to these pond conditions (Yeager <br />and Rutherford, 1957). Otter have been found to coinhabit beaver lodges <br />and appear to select for beaver ponds when first inhabiting a drainage in <br />Idaho (Wayne Melquist, personal communication). <br />The higher water tables often create vegetative responses that pro- <br />vide cover, forage, or edge effects that are attractive to a variety of <br />wildlife. Perhaps the most noticeable wildlife are the large ungulates. <br />Moose, elk, and whitetail deer in western Montana are commonly found assoc- <br />iated with beaver-influenced habitats in greater density than areas with- <br />out beaver. <br /> <br />Water Quality and Quantity <br /> <br />The reduction of velocities as a stream flows through beaver ponds <br />results in considerable amounts of sediments deposited in ponds, depend- <br />ing on the age and structure of the ponds. Reductions in stream sediment <br />up to 90 percent have been documented (Smith, 1981). Stream associated <br />resources or uses that are adversely influenced by sediment could be bene- <br />fitted by this reduction. <br />Water temperatures can be modified by ponding action (Adams, 1953; <br />Patterson, 1950; Reid, 1952). A springfed stream could be cooled during <br />winter, while the same stream during summer may have temperatures increased. <br />Trout populations existing in marginally high water temperatures could be <br />adversely affected, while populations in cold headwater conditions could <br />be benefitted by the warming of water resulting in increased basic bio- <br />logical productivity. <br />Beaver have the potential to increase the level of pathogens down- <br />stream from their activities, resulting from beaver excrement. Beaver <br />are one of many warm blooded mammals capable of transmitting the flagel- <br />lated protozoan, Giardia lamblia. As a result, this can be a concern to <br />municipal water supplies without adequate treatment facilities (J. <br />Bonham, in press). Variability in seasonal flows is commonly reduced <br />through the reservoir effect of bank storage adjacent to the ponds. The <br />amount of this storage capability is often quite low relative to the total <br />amount of spring runoff flows; however, as this bank storage is released <br />through late summer, the additional amount of water may be important <br />to water users or resources. <br /> <br />74 <br />
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