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<br />.. <br /> <br />-, <br /> <br />structures regulate the mainstream and others have been constructed on <br />major tributaries. Flooding ha.; been eliminated e:{cept in period.::. of <br />unusual runoff, silt and sand are caught by quiet waters of reservoirs, and <br />:~mperatures are ame1 iorated b;1 hypol imnetic relea.~es of ~oJater -from <br />:-:;idroelectr:c dam~. (Dolan et 3.1. 1974; ~1jndle/ 197?a; iurnerand V:<.r;:::::':3.1< <br />1982). Biological characteristics. of the lower Colorado Ri'.Je!'" ha'.Je :,een <br />c~anged e\Jen more .~pectac!Jlarl;' (Dill 1944; ~1il1er 19,51; ~1incKley 1973~ <br />:979a, 1982; Nicola 1979; Carothers and ~.~inckle/ :'?81; and others::'; th~ <br />~ative fish fauna has been essentially replaced by introduced species. <br /> <br />Reaches downstream from Grand Canyon <br /> <br />Much of the watercourse downstream from LaKe Head is channel ized, <br />dredged, rip-rapped, diKed, or otherwise directly altered from the original <br />state. Harnessed water resources are used for irrigation, generation of <br />hydroelectric power, municipal and domestic water supp1 ies, and recreation, <br />and impounding structures also function in flood control. Under average <br />watershed conditions the entire volume of flow is withdrawn several times <br />for use before all water is ultimately consumed. Progressively smaller <br />downstream flows are maintained by return of agricultural and domestic <br />wastewaters, seepage, and tributary inflow, until no surface flow reaches <br />the Sea of Cortez in periods of average precipitation. <br /> <br />Altered flow regimes, increased water clarity, and creation of large <br />reservoirs ~ echulon alternating with cold tailwater reaches, are habitats <br />heretofore unKnown to the lowermost Colorado River downstream from Grand <br />Canyon. These laKes and interconnecting streams provided suitable homes <br />for a variety of introduced fishes such as trouts, common carp, a number of <br />catfishes, mosquitofish and other poeci1 i ids, sunfishes (including large- <br />and sma1lmouth basses), striped bass, and tropical cichl ids in ~oJarmer <br />places. Concommitant with physical-chemical alterations and estab1 ishment <br />of an exotic fauna was a dramatic decl ine in abundances, diversities, and <br />distributions of native fishes. Once plentiful species such as C01orado <br />squawfish, bony tail , razorbacK sucKer, and desert pupfish are extirpated or <br />reduced to tiny fractions of their former populations in only a few places. <br />Other natives of lesser historic abundance, woundfin, roundtail chub, <br />flannelmouth sucKer, are gone. Only marine forms sporadicallY entering <br />from the Gulf of Ca1 ifornia continue to represent the former native fauna <br />at any level of abundance. <br /> <br />Modifications of the lowermost Colorado River mainstream are so vast <br />and the system is so large that most reaches now may be unsui table for <br />reclamation for management of native fishes. Only the 101)Jermost portion of <br />the reach below ParKer, Arizona, has yet to be severely modified, and plans <br />have long e:<isted for channelization and installation of control structures <br />in that area. On the other hand, we do not Known why native big-river <br />fi shes disappeared, and if it resul ted from an event or events now passed, <br />the;- might I,'Jel1 re-es~abl ish i": d.,)O\ila.ble to colonize the area. Calorac::) <br />SGuawfish from Willow Beach and De~ter NFHs stocKed in the upper Colorado <br /> <br />River bas;n h~ve survived at least three ;ears (Valentine :983 I ~n~ nc <br /> <br />prep?r'",:::-, :- <br /> <br />~ere ~ade prior to their re-introduc~:on. Natural <br /> <br />: o::~ <br />