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<br />pockets on rock benches or along steep rock walls, often adjacent to deep and swift water <br />(Valdez and Clemmer 1982), The young also use backwaters when they are available, Juveniles <br />use water as deep as 10m over sand-silt and boulder-bedrock substrates with velocities ofless <br />than 0.3 mlsec (Valdez et al, 1990), In the Colorado River in Grand Canyon, juveniles <175 mm <br />1'1 used primarily shorelines with vegetation, talus, or debris fans (Valdez and Ryel1997, <br />Converse 1996), as well as backwaters (Arizona Game and Fish Department 1996a), Selected <br />. shoreline habitats for fish <75 mm 1'1 had velocities of 0,0-0,3 mis, with an average of about 0,06 <br />(Valdez and Rye11995), Swimming abilities of juvenile humpback chub (73-134 mm 1'1) in the <br />laboratory were significantly reduced when fish were tested at colder temperatures of 14' C, when <br />compared to 20' C, Larger fish were not tested, but there is no evidence to suggest that larger <br />fish are affected by temperature as dramatically as small fish, Average length at the end of the <br />first year of life for humpback chub in Grand Canyon was 74 mm 1'1 (range, 58-138 mm 1'1) <br />(Valdez and Rye! 1995); hence, age 0 fish are most affected by the cold thennal regimes of the <br />Colorado River through Grand Canyon <br /> <br />Adults are generally found in a variety of depths, occupying shallow shaded areas in the mornings <br />and evenings and depths of 12 m or more during midday, Humpback chub are frequently found <br />along eddy lines in low velocity water adjacent to areas of high velocity, Selected habitats of 69 <br />radio tagged adults in Grand Canyon were large recirculating eddies (88% captures, 74% radio <br />contacts), and subadults used primarily shorelines with vegetation, talus, and debris fans and eddy <br />return channels (backwaters) (Valdez and Rye11997), <br /> <br />R~roduction <br /> <br />Humpback chub are spring spawners; Spawning in Black Rocks occurred from April to June, <br />depending on water temperature and flow (Valdez and Clemmer 1982, Kaeding et ai, 1990), The <br />majority of successful spawning by humpback chub in Grand Canyon presently occurs in the LCR <br />during March-May, at water temperatures of 16-22'C (Kaeding and Zimmerman 1983), Year- <br />around releases of 8-10' C from Glen Canyon Dam preclude successful mainstem reproduction, <br />except possibly for isolated reproductive efforts at mouths of seasonally-warmed tributaries or <br />warm springs; post-larval humpback chub were captured in association with an isolated <br />aggregation of adults at a warm spring atRM 30 (Valdez and Rye! 1997), indicating localized <br />reproductive success. Adult humpback chub from the vicinity of the LCR ascend the LCR <br />annually in February-April to spawn and descend during the summer months. Many young <br />hatched in the l.CR are disp1acedinto the Colorado River by monsoonal floOds during July- <br />September, with annua1 estimates of 246,000-3 ,9 million juveniles during 1990-93 (Valdez and <br />Rye11995), Survival of young to adulthood at age 3 was estimated at 0,001, while estimated <br />annual survival of adults was 0,93, Predation of juvenile humpback chub was documented for <br />brown trout (Salmo tnIUI), channel catfish (Jctalurus punctatus), and rainbow <br /> <br />17 <br />