Laserfiche WebLink
Lower Colorado River Basin <br />Primary drainage units of the LCRB are the mainstream <br />Colorado River and four major tributaries, the Little Colorado, <br />Virgin, Bill Williams, and Gila rivers. Razorback suckers in the <br />LCRB historically occurred in the mainstream Colorado River and <br />the Gila River drainage. <br />Colorado River--Historic distribution of razorback suckers <br />in the mainstream Colorado River (LCRB) extended from the <br />Colorado River delta in Mexico upstream to present-day Lake <br />Powell. It was most abundant downstream of present-day Lake <br />Mead, and particularly so around Yuma (Gilbert and Scofield <br />1898). Few records exist for razorback sucker in Grand and <br />Marble canyons, Arizona, (Smith 1959), and lack of extensive <br />surveys (Miller 1946) made historic estimates of abundance in <br />that reach difficult. Razorback suckers may have been <br />historically uncommon in turbulent canyon reaches of the LCRB. <br />Razorback suckers in the Green River (UCRB) are typically found <br />in calm, "flatwater" river reaches, not in turbulent canyons <br />(Tyus 1987, Lanigan and Tyus 1989). <br />Archeological remains of razorback suckers were common in <br />__.___ the Salton Sea area, and a reproducing population apparently <br />existed there in primeval times (Minckley 1983, Minckley et al. <br />in press). Increasing water salinity due to evaporation rendered <br />habitat for freshwater fishes marginal after 1929 and razorback <br />suckers disappeared (Evermann 1916, Coleman 1929). <br />8 <br />