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<br />916 <br /> <br />COPEIA, 1998, NO.4 <br /> <br />adults congregate at upstream ends of cobble <br />bars to spawn (McAda and Wydowski, 1985). <br />Postreproductive adults remain in flatwater or <br />eddies near margins of strong currents, gener- <br />ally in water at least 1 m deep. Young often con- <br />gregate downstream or on riffles and along <br />shoreline of flatwater reaches. Chart and Ber- <br />gersen (1992) suggested adult movements are <br />size-related, with larger individuals more sed- <br />entary than those 300-400 mm TL. They also <br />suggested that adult C. latipinnis occupy a defin- <br />able home range. Individuals are considered <br />adult at 300-400 mm TL (Minckley and Hol- <br />den, 1980); maximum size recorded in this <br />study was 661 mm TL. <br />Xyrauchen texanus was also historically distrib- <br />uted throughout the Colorado basin. It was <br />common in the lower basin (Kimsey, 1957) and <br />in reservoirs created by main-channel dams. It <br />was uncommon and declining in the upper ba- <br />sin by 1950 [Hubbs and Miller, 1953; Vanicek, <br />1967 (citing early 1960s agency reports)]. Hol- <br />den (1973) collected X. texanus only from mid- <br />dle and lower sections of the upper basin and <br />again noted its scarcity. It was also recorded as <br />sparse within Grand Canyon and areas imme- <br />diately north. Smith (1959) called X. texanus <br />". . . rare, or possibly just difficult to collect in <br />Glen Canyon, since extensive collecting turned <br />up only two immature (i.e., YOY) specimens" <br />(Glen Canyon, immediately upriver from Grand <br />Canyon, is now inundated by Lake Powell). <br />Many researchers (Minckley et aI., 1991:310; <br />this study) contend X. texanus was never abun- <br />dant in Grand Canyon, regardless of its current <br />conservation status. <br />Genetic variability within remnant Colorado <br />River populations of X. texanus is distributed in <br />a north-south cline (Dowling et al., 1996a) sim- <br />ilar to that recorded for abundance. More <br />northern populations (i.e., upper Green and <br />Yampa Rivers, upper Colorado River) exhibited <br />reduced variability, whereas the most extant <br />southern population (i.e., Lake Mohave, AZ) <br />was highest. Geographically intermediate pop- <br />ulations (Le., Lakes Mead and Powell) were <br />themselves intermediate in haplotype diversities <br />(with Powell populations greater than Mead). <br />Over evolutionary time, this species was pan- <br />mictic throughout its range. <br />Hybrids between C. latiPinnis and X. texanus <br />occur in small numbers and have long been rec- <br />ognized. Jordan's (1891) description of X. un- <br />compahgre was based on a C. latipinnis X X. tex- <br />anus hybrid. Hubbs and Miller (1953) exam- <br />ined eight putative hybrids (two from upper <br />Colorado and six from upper Green Rivers) and <br />noted morphological intermediacy in lateral- <br /> <br />line scale count, and a much abbreviated but <br />distinct nuchal keel. Hybrid intermediacy was <br />also reported by Vanicek (1967:45), who subse- <br />quently collected 16 putative hybrids from the <br />Green River following closure of Flaming Gorge <br />Dam (Vanicek et aI., 1970). Holden (1973) col- <br />lected 40 putative hybrids and 53 X. texanus <br />throughout the upper basin, usually associated <br />with one another in quiet backwater areas. Hy- <br />brids in upper Green and lower Yampa Rivers <br />were attributed by Tyus and Karp (1990) to an <br />abundance of C. latipinnis, a paucity of X. tex- <br />anus, and a temporal! spatial overlap in their <br />spawning. Smith (1992b) listed hybrids of these <br />two species as occurring broadly across drain- <br />ages. <br />The present study was a four-year, localized <br />study with three goals: to estimate population <br />numbers and survival probabilities of C. latipin- <br />nis and X. texanuswithin the Little Colorado Riv- <br />er (LCR) area of Grand Canyon; to evaluate <br />their seasonal and yearly movement patterns <br />within that area; and to determine relative <br />abundance and distribution of potential hy- <br />brids. <br /> <br />MATERIALS AND METHODS <br /> <br />Study area and data collection.-Our study was <br />confined to the LCR and its confluence with the <br />mains tern Colorado River, 99 river km (RKM) <br />below Glen Canyon Dam. The study area, in <br />both Grand Canyon National Park (GCNP) and <br />the Navajo Nation (Coconino County, AZ), is <br />described and mapped in Douglas and Marsh <br />(1996). <br />Base camps were established in the LCR <br />gorge at 0.6,3.1, and 10.8 RKM upstream from <br />the confluence. Biologists worked at each camp <br />during 49 six- to 14-day trips at approximately <br />monthly intervals from July 1991 to June 1995 <br />(Appendix). Fishes were captured with hoop <br />and trammel nets (the latter primarily at con- <br />fluence; net dimensions provided in Douglas <br />and Marsh, 1996). Effort was recorded as num- <br />ber of net-hours fished. All captured fishes were <br />identified, measured (TL to nearest mm), <br />weighed (nearest g), and sex determined. Big- <br />river endemics greater than 150 mm TL (= <br />adults) were injected with passive integrated <br />transponder (PIT) tags (Prentice et aI., 1990) <br />and released near points of capture. <br /> <br />Capture matrices.-Adults were classified as newly <br />tagged fish, recaptured fish, or those with old <br />tags. The first group represented fish PIT- <br />tagged by Arizona State University (ASU) per- <br />sonnel at time of capture. The second group <br /> <br />~ <br /> <br />'\ <br />