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Last modified
7/14/2009 5:01:46 PM
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UCREFRP
UCREFRP Catalog Number
7982
Author
Tyus, H. M.
Title
Ecology and Management of Colorado Squawfish. 379-402.
USFW Year
1991.
USFW - Doc Type
517
Copyright Material
YES
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<br /> <br />I';; o,f the same Colorado squawfish 00 the same <br />;;/spawniog grounds over a number of different <br />'::years; fidelity to these specific areas has been <br />''f::~: demonstrated (Wick et al. 1983; Tyus 1985, <br />,? 1990; Tyus and Karp 1989). There is no rec- <br />~fc ord of a fish moving from one spawning reach <br />~} to the other (e.g., interchanges of Yampa and <br />i;' Gray Canyon fish). Lack of suitable spawning <br />~; substrate or other factors is not judged to be <br />limiting. Migrating squawfish pass through <br />~~.. ~any ki!ometers of apparen~ly suitable spawn- <br />.fZ ' mg habitat to reach other Sites, and an olfac- <br />tory homing mechanism was proposed to ac- <br />count for this behavior (Tyus 1985, 1990). <br />Turbidity in the Green and Yampa rivers <br />has precluded direct observation of Colorado <br />squawfish spawning behavior. However, radio- <br />telemetry observations of wild spawning fish <br />were provided by Archer and Tyus (1984), and <br />Hamman (1981) noted behavior of spawning <br />fish in hatchery conditions. Fish behavior was <br />similar to that described for a congener, the <br />northern squawfish (Ptychocheilus oregonen- <br />sis), by Patten and Rodman (1969) and Beams- <br />derfer and Congleton (1982). Northern squaw- <br />fish remained in deep pools or eddies, moved <br />abruptly to cobble bars to spawn, then re- <br />turned to the pools or eddies. This same <br />behavior in Colorado squawfish prompted <br />division of habitats into two types: a resting- <br />staging area in pools or large, shoreline mix- <br />ing (eddying) currents, where fish find suitable <br />resting and feeding conditions between spawn- <br />ing bouts or where males gather around fe- <br />males until they are ready to deposit eggs; and <br />a deposition-fertilization habitat in riffles and <br />shallow runs where they congregate for actual <br />reproduction (Archer and Tyus 1984; Tyus <br />and Karp 1989; Tyus 1990). <br />It has been difficult to identify spawning <br />grounds for Colorado squawfish in otherloca- <br />tions, in part because the fish is so rare. The <br />presence of small larvae in the upper main- <br />stem Colorado and San Juan rivers indicates <br />successful reproduction, but their low num- <br /> <br />The Colorado Squawfish 3 8 5 <br /> <br />bers suggest limited reproduction or recruit- <br />ment. No conclusive migratory patterns have <br />been detected in the Colorado main stem de- <br />spite years of study, although some migration- <br />like movements have been noted (Archer et <br />at. 1985, 1986). Perhaps spawning behavior <br />documented for the Green and Yampa rivers <br />was disrupted in the Colorado by years of <br />flow and habitat alterations, or perhaps that <br />stream was never optimal for the fish (Kaed- <br />ing and Osmundson 1988b). The San Juan <br />River has been studied far less, and squawfish <br />ecology is less known in that system. <br /> <br />Habitat Relations <br /> <br />Larval ecology <br /> <br />Colorado squawfish larvae hatch in 3.5-6.0 <br />days at 20o-220C (Hamman 1981). Drift net- <br />ting and seining indicate that larvae emerge <br />from the cobble soon after hatching and move <br />downstream out of the Yampa River in three <br />to fifteen days (Haynes et al. 1984; Nesler <br />1986; Nesler et ale 1988). Drifting young are <br />predominantly protolarvae, and those from <br />shoreline backwaters are metalarvae (Haynes <br />and Muth 1982, 1984), suggesting that the <br />fish seek warmer and more productive <br />habitats as they grow (Tyus et al. 1987). <br />Young-of-year (postlarval) squawfish are rare <br />in Yampa and Gray canyons but are distrib- <br />uted 100-250 km downstream a few weeks <br />after the spawn (Fig. 19-3; Tyus et at. 1982b, <br />1987). They occupy shallow, alongshore, <br />ephemeral embayments (backwaters) formed <br />in late summer by receding water levels (Hol- <br />den 1977b; Tyus et a1. 1982b, 1987; Haynes et <br />al. 1984; Tyus and Haines 1991). This obser- <br />vation led to development of a downstream <br />transport hypothesis (\v. H. Miller et al. <br />1982b; Tyus et a1. 1982b). Although the <br />downstream movement of young away from <br />spawning sites was once debated (Holden <br />1977b; Holden and Wick 1982), the hypoth- <br />esis is now generally accepted (USFWS 1978b, <br />
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