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148 The Southwestern Naturalist vol. 34, no. 1 ~ March 1989 Notes 149 "~ <br />/ <br /> <br />NEV UTAH <br />CALIF °LaM• <br />Mo~av~ <br />_ ARIZ <br />MEXICO ~ <br /> \\ <br />.24m/s ~ l" <br />v <br />.36 m/a \ <br />~~I <br /> <br /> ~\~ .12 m/ra 0.0 m/a <br />.46 m/s ~\ \~ `\ ~ <br />~ ~ ~ \ <br />\ <br /> ~ ~ <br />\ <br />` ` <br /> ~ <br />~ ~\ <br />• <br />1 Baekwoter <br /> <br />V <br />1 1t t <br /> ~ <br />~ 1 <br /> ~ ~ <br />\ t 1 Wo9h ~ <br /> <br /> t ~ ~ <br /> ~ ~ <br />1 <br /> I <br />~ ~ <br />1 <br /> I t <br />I 1 <br /> I <br />I t~ <br />/ I 1 <br />/ I <br /> ~ <br />/ / ~ <br />' <br />/ /~~ I <br /> ~ 4 <br />/ <br />~ / 1 <br /> / <br />• <br />i ~ ~ , ~~ <br /> / <br /> / <br />1.5m 1.4m <br /> I.Tm <br /> Lfim <br /> <br />X 2.Om ` <br />~` <br /> <br /> LEGEND <br />10 0 10 20 30 <br />DEPTH <br />SCALE OF METERS ' <br /> ----- VELOCITY <br /> ~ SPAWNING <br /> DEPRESSIONS <br />FIG. 1-Spawning depression distribution, water depth, and velocity profiles for razorback suckers <br />(Xyrauchen texanus) in the Colorado River, Lake Mohave, Nevada-Arizona. <br />1 <br />location. Spawning activities appeared to be restricted to a 300-mz area of scoured sands and gravels <br />deposited in the river channel From a dry wash located 4.6 km downstream of Hoover Dam. Substrate <br />size in this area was different from the larger armored material or fine sands observed in other areas <br />of the river. ` <br />Additional dives were conducted over the spawning area on 11 February, 25 February, and 11 <br />March 1984 with suckers (1 to 37) observed on each occasion. All observations, measurements, and <br />underwater sampling were accomplished using scuba equipment. The spawning site was mapped with <br />water depth and velocity profiles shown in Fig. 1. Scuba observations revealed that vigorous and <br />repeated spawning activities disturbed the substrate and resulted in obvious depressions. Activities <br />Rushed finer materials from the substrate leaving depressions lined with larger gravels and cobble. <br />Within the spawning area, i8 depressions measuring 0.25 to 1 mz were identified and occurred at <br />depths of 1.2 to 2.0 m (28 January). Mean water velocities (Marsh McBirney Row meter, Mod. 201) <br />ranged from 0.00 to 0.37 m/s. Nose velocities (10 cm from substrate) at Rve specific sites where <br />spawning was observed averaged 0.15 m/s (range of 0.12 to 0.18 m/s). <br />Twenty-three Surber samples yielded 103 eggs and 34 larvae. Eggs and larvae were collected during <br />January and February, but none were found during March. Samples (n = 19) taken directly from <br />spawning depressions yielded 10.5 to 16.7 eggs/m2 and 0.7 to 5.7 larvae/m2. Samples (n = 3) taken <br />from finer material outside of depressions did not yield any eggs or larvae. One sample collected from <br />large-cobble substrate located immediately downstream from the spawning site yielded 52 eggs (273.7 <br />eggs/mz) and 21 larvae (110.5 larvae/mz), suggesting a high degree of drift. <br />Fecundity of adult female razorback suckers has been found to average nearly 1,800 ova/cm standard <br />length, and most females are >50 cm standard length (=about 100,000 ova/female; Minckley, 1983). <br />Based on maximum observed density of 274 eggs/m2, it appears females deposit only a few eggs at a <br />time. <br />Spawning behavior was similar to that reported for populations in reservoirs. However, spawning <br />males appeared to be less mobile in the river. The majority of fish, which appeared to be "small" <br />(approximately 40 cm total length) males, maintained stationary positions on the downstream end of <br />the site. This behavior was different from the roving nature previously observed and reported for <br />reservoir-spawning groups (Minckley, 1983). Larger fish, presumably females, periodically moved into <br />the area from the adjacent river, attracting some of the otherwise stationary males to form spawning <br />groups of three to eight fish. These groups, composed of one female and several males, would spawn <br />over depressions or swim around the area before dispersing. The spawning act only took a few seconds <br />and, other than orienting with the current, was similar to that reported elsewhere. However, on several <br />occasions spawning groups appeared to seek shelter downstream of large boulders and, while maintaining <br />their position, would roll in mass for several seconds. <br />These observations illustrate that razorback suckers can and do spawn in lotic environments down- <br />stream from major impoundments. Possibly, these riverine spawning conditions more closely resemble <br />the structural habitats utilized by razorback suckers in the Colorado River prior to man's influence on <br />the system. <br />I thank P. Marsh and R. Leutheuser for critical review of the manuscript. <br />LITERATURE CITED <br />HOLDEN, P. B., AND C. B. STALNARER. 1975. Dis[ilbu[IOn and abundance Of mainstream fishes Of <br />the middle and upper Colorado River basins, 1967-1973. Trans. Amer. Fish. Soc., 104:217- <br />231. <br />MARSH, P. C., AND D. R. LANGHORST. In press. Feeding and fate of wild larval razorback sucker. <br />Environ. Biol. Fishes. <br />HINCKLEY, C. O., AND S. W. CAROTHERS. 1979, Recent collections of the Colorado squawfish and <br />razorback sucker from the San Juan and Colorado rivers in New Mexico and Arizona. <br />Southwestern Nat., 24:686-687. <br />HINCKLEY, W. L. 1983. Status of the razorback sucker, Xyrauchen texanus (Abbott), in the lower <br />Colorado River basin. Southwestern Nat., 28:165-187. <br />ULMER, L. ] 980. Movement and reproduction of razorback sucker inhabiting Senator Wash Reservoir, <br />California. Proc. Desert Fishes Council, 12:106. <br />GORDON MUELLER, Bureau of Reclamation, Boulder City, NV 89005. <br />