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Last modified
7/14/2009 5:02:32 PM
Creation date
5/17/2009 11:32:34 PM
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UCREFRP
UCREFRP Catalog Number
8067
Author
Nance, E. L.
Title
Planktonic and Benthic Invertebrate Densities in Three Backwater Habitats on the Lower Green River Final Report.
USFW Year
1997.
USFW - Doc Type
Grand Junction, CO.
Copyright Material
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<br />STUDY SITES <br /> <br />Sampling trips were made possible through the generous cooperation of Tom Chart and <br />Melissa Trammel, UDWDNR Moab, who were conducting weekly larval fish sampling <br />with light traps. Trips began at Mineral Bottom, RK 52, withjon boats to access the <br />backwaters. The fish team placed six quadrafoil design light traps in Millard Canyon, and <br />three each at Anderson Bottom and Holeman Canyon. Sampling was performed for two <br />consecutive nights during the twelve hour period from dusk to dawn. <br /> <br />Each backwater was divided into front (that portion closest to the main river channel), <br />middle and back thirds, with sampling efforts concentrated in the latter two. Obviously, <br />this changed with increasing river flows, as did depths and dimensions, so that what was <br />initially considered the back one third in the beginning of the study, became the middle <br />third towards the end. <br /> <br />Millard Canyon <br /> <br />Millard Canyon, located at RK 34 on the lower Green River in Canyonlands National <br />Park, was the most upstream backwater. This was the only site that did not have a point <br />bar formed across its entrance at the start of the field season. It was the largest and <br />longest backwater, approximately 10m wide at the mouth, 150 - 200 m long, with uneven <br />depths up to 4 m. The back portion of the site became estuary-like as river levels <br />increased, with shallow depths and submerged vegetation. In general, the substrate was <br />comprised of coarse red sand and silt with very little clay. <br /> <br />Salix sp. grew densely along the sides of the entrance and first one third of the backwater. <br />A large bed of Tvpha lies at the base of a sandstone wall on the south side of the <br />backwater approximately two thirds in, and a mixture of willow and Tamarix fill the <br />shallower, back one third. The USGS 7.5 I HorsethiefQuadrangle map shows a <br />perennial creek draining into the main stem of the river through Millard Canyon, though <br />it was not possible to find it towards the end of the field season. A short hike <br />approximately 800 m up the drainage revealed a dry stream bed suggesting that the <br />stream either submerges or is ephemeral. <br /> <br />Anderson Bottom <br /> <br />Anderson was the middle backwater site located at RK 31. It was roughly circular and <br />pond-like; approximately 20 m in diameter. Access to the backwater was impossible by <br />boat during the first two weeks of sampling due to a large point bar which extended <br />nearly across the mouth, leaving an entrance of one meter wide. <br /> <br />Tamarix, Salix. and a few young Populus trees formed the riparian vegetation. A reed <br />bed grew behind the point bar at the backwater entrance, both of which became <br />submerged with rising water levels. A large, dead cottonwood was submerged <br /> <br />2 <br />
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