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Missouri River Basin
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Last modified
4/8/2013 5:26:26 PM
Creation date
3/6/2013 1:04:48 PM
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Water Supply Protection
Description
related to the Platte River Endangered Species Partnership (aka Platte River Recovery Implementation Program or PRRIP) Technical Advisory Committee (TAC) Meeting - Pallid Sturgeon
State
CO
WY
NE
MO
Basin
South Platte
Water Division
1
Author
CWCB Staff
Title
Staff comments on the US Fish and Wildlife's Biological Opinion on the Missouri River Main Stem Reservoir System, Operation and Maintenance of the Missouri River Bandk Stabilization and Navigation Project, and the Operation o fthe Kansas River Reservoir
Water Supply Pro - Doc Type
Report/Study
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Erickson (1992) found pallid sturgeon movement greater during the night while Bramblett (1996) <br />observed greater movements during the day. The primary habitat difference suspected in those findings <br />was turbidity. Erickson (1992) had secchi readings as high as 157 in (400 cm) while Bramblett (1996) <br />averaged 8 in (20 cm) and rarely exceeded 39 in (100 cm). Bramblett (1996) modeled the information <br />from his study and found that predictive depth of pallid sturgeon was greater during the hours following <br />sunrise and suggested that pallid sturgeon may be photophobic. <br />The spawning period for pallid sturgeon, believed to occur from late April into July, historically <br />corresponded with increased flows from runoff, which also has been known to trigger spawning of <br />other ancient big -river fish such as paddlefish (Russell 1986) and shovehiose sturgeon (Berg 1981). <br />Gardner (1995a) radio tracked 14 pallid sturgeon in the upper Missouri River during a low water runoff <br />year and a near - normal year. He found that adult pallid sturgeon moved an average of 3.2, 12.9, and <br />17.6 mi (5.1, 20.7, 28.3 km) further upriver during May, June, and July of the normal runoff year <br />compared to the low runoff year. <br />Both shovelnose sturgeon and paddlefish spawning migrations occur in response to increased flows in <br />June (Berg 1981). Although there is limited information on pallid sturgeon spawning migrations, <br />Bramblett (1996) stated that discharge and photoperiod may be important environmental cues for the <br />timing of movements for both shovelnose and pallid sturgeon. He found a typical pattern of movement <br />for pallid sturgeon was to move upstream into the Yellowstone River and out of the Missouri River in <br />the early spring during increasing discharge and photoperiod; reside in the Yellowstone River during <br />high discharge; and move downstream, back into the Missouri River during late summer. A similar <br />pattern has been observed in the paddlefish population (John Firehammer, University of Idaho, pers. <br />comm.). <br />Erickson (1992) and Bramblett (1996) observed that movement rates of pallid sturgeon were lowest in <br />winter months and a significant positive correlation between water temperatures and movement rate of <br />pallid sturgeon existed. <br />Juvenile pallid sturgeon from Gavins Point NFH in South Dakota were subjected to swimming stamina <br />tests in 1998. Adams et al. (1999) found sustained and prolonged speeds of juvenile pallid sturgeon <br />were comparable to similar sized lake sturgeon; however, pallid sturgeon exhibited a higher capacity <br />for burst swimming. Adult shovelnose sturgeon, a closely related species, were also tested for <br />swimming endurance. Sturgeon were found to swim volitionally at low speeds (5 -30 c /s), but at higher <br />speeds (40 -120 c /s), sturgeon alternated between active swimming and appressing themselves to the <br />bottom of the swimming tunnel (USFWS 1999). This second behavior is enhanced by sturgeon <br />morphology - streamlined body shape, flat rostrum, and large pectoral fins. It allows sturgeon to <br />exploit river bottoms as a refugia from current and maintain position in high velocities. <br />Population Status and Trends <br />Status Range Wide -PS 103 <br />
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