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<br />Page 36 <br /> <br />FLANNELMOUTH SUCKER <br /> <br />Flannelmouth sucker reside in mainstem and tributary streams. Elements of flannelmouth sucker <br />habitat include 0.9 to 6.1 m deep murky pools with little to no vegetation and deep runs and riffles <br />(Bezzerides and Bestgen 2002, McAda 1977, Sigler and Sigler 1996). Preferred substrates consist of <br />gravel, rock, sand, or mud (McAda 1977, Sigler and Sigler 1996). Flannelmouth sucker partition <br />habitat use by life stage, with young fish occupying quiet, shallow riffles and near-shore eddies, and <br />adults occupying deep riffles and runs. Flannelmouth sucker do not prosper in impoundments <br />(Bezzerides and Bestgen 2002, McAda 1977, Sigler and Sigler 1996), though one introduction during <br />the 1970's in Lake Havasu in the lower Colorado River Basin continues to persist (Mueller and <br />Wydoski 2003). Flannelmouth sucker are opportunistic, benthic omnivores consuming algae, <br />detritus, plant debris, and aquatic invertebrates (Bezzerides and Bestgen 2002, McAda 1977, <br />Osmundson 1999, Sigler and Sigler 1996). Food consumed depends on availability, age class, and <br />time of season (McAda 1977, Sigler and Sigler 1996). <br /> <br />Flannelmouth sucker mature at four or five years of age; males mature earliest (McAda 1977, Sigler <br />and Sigler 1996). Females ripen at water temperatures of lOoC, whereas males ripen earlier in the <br />spring (6.1 to 6.70C) and remain fertile for a longer period of time (McAda 1977, Sigler and Sigler <br />1996). Seasonal migrations are made in the spring to suitable spawning habitat (Sigler and Sigler <br />1996, Suttkus and Clemmer 1979). McKinney et al. (1999; see also Bergersen 1992, Chart 1987, <br />Chart and Bergersen 1987) documented long-range movements (ca. 98-231 kIn) among adult and <br />sub-adult fish, although the roles these movements (and obstructions to such, i.e., dams) play in the <br />life history of the fish are unclear. Many researchers suspect that flannelmouth sucker return to natal <br />tributaries for the purpose of spawning (Snyder and Muth 1990; Weiss et al. 1998). Populations <br />spawn for two to five weeks over gravel substrates. A female will produce 9,000 to 23,000 adhesive, <br />demersal eggs. After fertilization, the eggs sink to the bottom of the stream and attach to substrate or <br />drift between crevices (Sigler and Sigler 1996). <br /> <br />FLANNELMOUTH SUCKER STATUS REVIEW <br /> <br />General <br /> <br />Historical literature suggests that flannelmouth sucker were common to all parts of the Colorado <br />River Basin up to the 1960's (Jordan and Evermann 1902, Minckley 1973, Sigler and Miller 1963). <br />They have been greatly reduced in the lower Colorado River Basin, but are still widespread in the <br />upper basin (Bezzerides and Bestgen 2002). They are thought to remain in at least 50% of their <br />historical range above Glen Canyon Dam (Bezzerides and Bestgen 2002). There are extant <br />populations in the mainstem Colorado and in tributaries in the Grand Canyon reach and in the Virgin <br />River in Utah, Arizona, and Nevada (see Figure 2-8). Of the historical flannelmouth sucker sites in <br />Utah, the species has only been extirpated from sites near Flaming Gorge Dam (Vanicek et al. 1970). <br />Flannelmouth sucker continue to be documented at all other sites. Hybridization with nonnative <br />white sucker is thought to be an increasing threat. White sucker are commonly seen in the Green <br />River and have been seen occasionally in smaller tributaries of the Green and Colorado rivers. As the <br />range of the white sucker increases, it is thought that the range of the flannelmouth sucker will <br />decrease, as hybridization between the two species is prevalent (Anderson and Stewart 2000, Bestgen <br />and Crist 2000, Holden and Crist 1981, Holden and Stalnaker 1975). <br /> <br />Northeastern Region <br />