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<br />.""- ." <br /> <br />Recordings were reviewed using a VHS editor, which time-referenced each 2-hour tape <br />recording. Recordings were paused at precise 5-min intervals. Fish and tadpoles were <br />counted for that single frame and then the tape was pl<;tyed for 60-sec as additional <br />organisms were counted. Based on these counts and area assumptions, the occurrence of <br />razorback sucker, bonytail, and bullfrog tadpoles were converted to organisrn/~ for <br />single frame counts. Number of organisms/m2 provides an approximation of density <br />while organisms/l-min provides an indicator of activity since a single organism could be <br />viewed more than once. Unique behavior was also noted in the monitoring log. <br /> <br />Results and Discussion <br /> <br />More than 124 hours of underwater monitoring was recorded. All but four hours <br />(control) were directed at bonytail and razorback sucker spawning activity. <br /> <br />Razorback Sucker. Razorback suckers were already spawning when field activities <br />started 18 February, 2003. Groups of adults were seen schooling along the river levee. <br />Actual spawning events caused plumes of sediment to 'boil' to the surface and then <br />gradually disperse. Snorkeling revealed the substrate was comprised of cobble and large <br />gravel. Spawning occurred on the levee's toe, or the deepest area of the pond. Disturbed <br />substrate extended 3 m from the levee's toe and ran parallel to the levee for <br />approximately 30 m (90 m2). Depth ranged from 1 to 2 m and gradually increased to <br />2-3 m as water elevation increased in response to rising river stage. Surrounding <br />substrates were covered with approximately 10 cm of fine sediment. <br /> <br />Spawning continued well into March as eggs were discovered on the 19th and larvae were <br />collected on 24 March. Water temperature during spawning ranged from 15.3 to 20.10 C <br />(bottom temperature, Fig. 1). Spawners had dispersed and bonytails were finally <br />observed in the area by 1 April, 2003. <br /> <br />25 <br />() 23 <br />c. 21 <br />E 19 <br />~ 17 <br />15 <br /> <br /> <br />_ Bottom Temp <br />__ Surface Temp <br /> <br />C"') <br />o <br />o <br />I::::! <br />0) <br />...- <br />N <br /> <br />C"') <br />o <br />o <br />I::::! <br />!:Q <br />C"') <br /> <br />C"') <br />o <br />o <br />N <br />0; <br />..- <br />?i <br /> <br />C"') <br />o <br />o <br />I::::! <br />I::::! <br />oq- <br /> <br />C"') <br />o <br />o <br />I::::! <br />co <br />..- <br />~ <br /> <br />Figure 1. Water temperature taken at the surface and bottom of Cibola High Levee Pond, <br />Arizona-California. <br /> <br />8 <br />