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<br />10 . Executive Summary <br /> <br />soo <br /> <br />1233 <br /> <br />700 <br /> <br />600 <br /> <br />.c <br />.!!!500 <br />u.. <br />.... <br />~400 <br />ClI <br />.c <br />g300 <br />z <br /> <br />200 <br /> <br />o Shoreline <br />. Offshore <br /> <br />Final Report <br /> <br />aggregations of humpback chub in <br />Grand Canyon, which were river <br />reaches with abundant debris fans and <br />channel expansion zones, These <br />complexes were large recirculation <br />zones that entrained and entrapped <br />drifting food, and provided low- <br />velocity vortices in which the fish <br />could feed and rest. <br /> <br />Adult humpback chub in Grand <br />Canyon used large recirculating eddies <br />to a greater degree than adults have <br />displayed in other populations (Valdez <br />et al. 1990). Adults in other <br />populations appear to use a wider <br />range of habitats, possibly because <br />more normal warm spring, summer, <br />and fall temperatures enable the fish <br /> <br />o <br /> <br /> <br />100 <br /> <br />o g g ~ ~ 2 ~ ~ ~ ~ 8 g g g ~ 2 ~ <br />~ ~ ~ N N N M M M M ~ ~ ~ <br />Total Length (10 mm increments) <br /> <br /> <br />Fig. 9. Length-frequency distribution of humpback chub captured in <br />shoreline habitats (with electrofishing, seines, minnow traps) and in <br />offshore habitats (with gill nets, trammel nets) for 1991-93. <br /> <br />Hence, although shoreline habitats of the type <br />selected by subadults appeared to be suitable and <br />abundant in Grand Canyon, we hypothesize that <br />use was reduced by the limited swimming ability <br />of the young fish at cold temperatures, and by the <br />destabilizing effect of fluctuating dam releases. <br />Greater use of vegetated shorelines was <br />attributed to reduced velocities, high cover value, <br />and relatively high food production among <br />tamarisk, willows, sedges, and other riperian <br />vegetative types. This vegetative cover, which <br />was absent under predam conditions, except <br />during high runoff or flood flows, may be used <br />by the fish in the absence of high constant <br />turbidity as cover from predators and to avoid <br />high light levels. <br /> <br />Nearshore velocities along cobble bars and <br />bedrock exceeded the range of maximum cruising <br />speed ofYOY humpback chub (range, 30-100 <br />mm TL) at 140C (Fig. 10); sand beaches lacked <br />cover and despite low velocities, were not used <br />by YOY during the day or in clear water, <br /> <br />Adult humpback chub used eddy complexes <br />disproportionate to their composition of surface <br />area; 88% of adults captured and 74% of radio <br />contacts were from eddies which averaged only <br />21% of surface river area (Fig. 11). <br />Disproportionate use of eddy complexes <br />coincided with the location of the three largest <br /> <br /> 0.5 <br /> 0 <br /> 0.5 1.5 2.5 0.5 1.5 2.5 <br /> Subreach 1 (Meters from Shore) Subreach 2 <br /> 0.7 <br /> B. Velocity <br /> 0.6 <br /> 0.5 <br />- <br />.!!! <br />.5. 0.4 <br />~ <br />'8 0.3 <br />~ <br /> 0.2 <br /> 0.1 - <br /> 1.5 2.5 0.5 1.5 <br /> Subreach 1 (Meters from Shore) Subreach 2 <br /> <br />2.5 <br /> <br /> <br />Depth <br /> <br />- Bedrock <br />-Cobble <br />- Debris Fan <br />-Sand <br />- Talus <br />- Vegetation <br /> <br />2 <br /> <br />1.5 <br /> <br /> <br /> <br /> <br />Fig. 10. Average depth (A) and velocity (B) at three distances <br />from shore (0.5, 1.5 and 2.5 m) for six shoreline types in <br />Subreach 1 (RM 61.9-65.4) and Subreach 2 (RM 65.4-73.4). <br />The ranges in cruising speed for YOY and juveniles are <br />shaded areas. <br />