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downstream of the Millard Canyon cobble bar (RK 53.9 / RM 33.5) were sampled with light <br />traps and seines (refer to Appendix table 1). No Colorado pikeminnow larvae were collected <br />below the suspected spawning baz. Two larval razorbacks were collected in these habitats. Red <br />shiners dominated the light trap collections, however relatively few fish were collected overall <br />(Table 2). Seine haul samples from this portion of the river were comprised completely of <br />nonnative cyprinids with red shiners being the overwhelmingly dominant species. <br />The ISMP database (1986-1996) was used to determine if YOY Colorado pikeminnow <br />total length has varied longitudinally throughout Reach 3 (RK 193.2-0.0 / RM 120.0-0.0) on an <br />annual basis. The contention was that if a consistent shift in size of YOY was found below <br />Millard Canyon spawning may have occurred there. In figure 7, the average size of YOY <br />pikeminnow collected above and below Millazd Canyon was plotted for eleven years: 1986- <br />1996. The respective means appear to vary little during the years of extended high spring flows; <br />1986, 1993, 1995. There was a greater discrepancy during the low flow years with the greatest <br />difference in size of YOY pikeminnow observed in 1992 (YOY Colorado pikeminnow upstream <br />of Millard Canyon averaged 36.4 mm TL; downstream averaged 49.7 mm TL). There was a <br />statistically significant (t-test for unequal variances; p<0.05) difference in the size of YOY CPM <br />collected above vs. below Millard Canyon in most moderate to low flow years <br />(`87,'88,'89,'90,'92,'94,'96). However, there was no consistency to the nature of that difference, <br />i.e., 3 of 7 years (42.8%) fish were smaller downstream of Millard Canyon with the converse <br />occurring with a similar frequency (58.2% of the time). <br />DISCUSSION <br />Razorback sucker <br />No adult razorback sucker were collected in 1994 or 1995. The lack of captures maybe <br />an indicator of poor timing of sampling or insufficient effort to locate small groups of spawning <br />individuals. The latter explanation likely applies to the razorback sucker sampling in the lower <br />Green River. A comparison of ISMP generated captures of adult razorbacks in the middle <br />(Reach 2 and 3) and the lower Green River (Reach 4) indicates razorback sucker densities are <br />lower in the lower portions of the river (McAda et al 1997). The number of razorback sucker <br />adults in the lower portion of the Green River is likely extremely low, perhaps an order of <br />magnitude less than in the middle Green River. Occasional collections of adult razorback sucker <br />continue to be reported in the lower Green River as referenced in Table 1. In the future, if <br />collecting adult razorback suckers is deemed necessary by the RIP, sampling should become <br />more innovative- employing different collection techniques (primarily fyke nets) and target new <br />or infrequently sampled areas. Radio telemetry may also assist in locating spawning locations / <br />more adults. <br />Larval captures for all species declined from 1994 to 1995, which was exemplified by <br />razorback sucker captures that fell from 44 to 4. A total of 210 flannelmouth sucker larvae were <br />collected in and near the mouth of the San Rafael River in l 994. Similar sampling in 1995 <br />produced 1821arvae. Bluehead larval collections declined from 210 in 1994 to 331arvae in <br />1995. The majority of flannehnouth sucker larvae were collected by early June, during both <br />years. Bluehead suckers became abundant slightly later in the sampling periods. Total numbers <br />6 <br />