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• 11. [Article] Fish Management Plan Detroit Reservoir 1982

  Abstract -- Detroit Reservoir is a 3,580 acre Corps of Engineers multipurpose reservoir located at river mile 48.5 on the North Santiam River. The dam is located just below the confluence of the North ...

  Citation × Citation Citation Abstract Copy Title: Fish Management Plan Detroit Reservoir 1982 Abstract -- Detroit Reservoir is a 3,580 acre Corps of Engineers multipurpose reservoir located at river mile 48.5 on the North Santiam River. The dam is located just below the confluence of the North Santiam and Breitenbush rivers. The reservoir was impounded in 1953 and is 9 miles long and over 1 mile at its widest point. Surface elevation is 1,569 ft at full pool. The reservoir is located about 50 miles east of Salem and road access is via State Highway 22. A large overnight campground and a day use area, both with boat launching facilities, are maintained by the Parks and Recreation Division of the Oregon Department of Transportation. The U.S. Forest Service (USFS) maintains two campgrounds on the south side of the reservoir, and there are two commercial boat concessions near the town of Detroit. Most of the area surrounding the lake is USFS land, although there are some private homesites on the North Santiam arm near Detroit. The reservoir receives heavy recreational use during the spring and summer months, including fishing, swimming, boating, camping, and water skiing. Fish passage structures were not incorporated in either Detroit or Big Cliff (reregulating dam) dams and consequently some 82 miles of stream are no longer available to former runs of spring chinook salmon and winter steelhead. In July 1982, the Oregon Fish and Wildlife Commission accepted the Department's recommendation to manage Detroit Reservoir for hatchery fish. Title: Fish Management Plan Detroit Reservoir 1982 Abstract -- Detroit Reservoir is a 3,580 acre Corps of Engineers multipurpose reservoir located at river mile 48.5 on the North Santiam River. The dam is located just below the confluence of the North Santiam and Breitenbush rivers. The reservoir was impounded in 1953 and is 9 miles long and over 1 mile at its widest point. Surface elevation is 1,569 ft at full pool. The reservoir is located about 50 miles east of Salem and road access is via State Highway 22. A large overnight campground and a day use area, both with boat launching facilities, are maintained by the Parks and Recreation Division of the Oregon Department of Transportation. The U.S. Forest Service (USFS) maintains two campgrounds on the south side of the reservoir, and there are two commercial boat concessions near the town of Detroit. Most of the area surrounding the lake is USFS land, although there are some private homesites on the North Santiam arm near Detroit. The reservoir receives heavy recreational use during the spring and summer months, including fishing, swimming, boating, camping, and water skiing. Fish passage structures were not incorporated in either Detroit or Big Cliff (reregulating dam) dams and consequently some 82 miles of stream are no longer available to former runs of spring chinook salmon and winter steelhead. In July 1982, the Oregon Fish and Wildlife Commission accepted the Department's recommendation to manage Detroit Reservoir for hatchery fish. Close

• 12. [Article] Trout Management Plan Lost Lake 1982

  Abstract -- Lost Lake is located adjacent to State Highway 20 about 43 mi west of Bend and 4 mi west of the Santiam Pass. The lake has about 50 surface acres and is located at an elevation of 3,980 ft. ...

  Citation × Citation Citation Abstract Copy Title: Trout Management Plan Lost Lake 1982 Abstract -- Lost Lake is located adjacent to State Highway 20 about 43 mi west of Bend and 4 mi west of the Santiam Pass. The lake has about 50 surface acres and is located at an elevation of 3,980 ft. Three tributaries enter the lake, the largest being Lost Lake Creek. The lake has a maximum depth of 12 ft, but most of the lake basin is from 3 to 4 ft deep. The U.S. Forest Service (USFS) maintains a campground on the west side of the lake, but it is not accessible until snow melts. Recreational use is primarily camping and angling. The lake receives varying amounts of angling pressure. In 1979, the USFS estimated all recreational use to be 4,000 visitor days. In 1957, the lake receded to only the stream channels, as considerable flow was visible escaping through the lava fissures. With help from the local resort operator, truckloads of cinders and lava rock were used to fill the two known outlets. Water still escapes through the cinder fills, but the lake has never dropped to the low level experienced in 1957. In July 1982, the Oregon Fish and Wildlife Commission accepted the Department's recommendation to manage Lost Lake for wild and hatchery fish. Title: Trout Management Plan Lost Lake 1982 Abstract -- Lost Lake is located adjacent to State Highway 20 about 43 mi west of Bend and 4 mi west of the Santiam Pass. The lake has about 50 surface acres and is located at an elevation of 3,980 ft. Three tributaries enter the lake, the largest being Lost Lake Creek. The lake has a maximum depth of 12 ft, but most of the lake basin is from 3 to 4 ft deep. The U.S. Forest Service (USFS) maintains a campground on the west side of the lake, but it is not accessible until snow melts. Recreational use is primarily camping and angling. The lake receives varying amounts of angling pressure. In 1979, the USFS estimated all recreational use to be 4,000 visitor days. In 1957, the lake receded to only the stream channels, as considerable flow was visible escaping through the lava fissures. With help from the local resort operator, truckloads of cinders and lava rock were used to fill the two known outlets. Water still escapes through the cinder fills, but the lake has never dropped to the low level experienced in 1957. In July 1982, the Oregon Fish and Wildlife Commission accepted the Department's recommendation to manage Lost Lake for wild and hatchery fish. Close

• 13. [Article] Passage behavior of radio-tagged yearling chinook salmon and steelhead at Bonneville Dam associated with the Surface Bypass Program, 2000

  Abstract -- In 1994, the U.S. Army Corps of Engineers (COE) initiated a program to develop and evaluate surface-oriented juvenile salmonid bypass systems at hydroelectric dams on the Columbia and Snake ...

  Citation × Citation Citation Abstract Copy Title: Passage behavior of radio-tagged yearling chinook salmon and steelhead at Bonneville Dam associated with the Surface Bypass Program, 2000 Abstract -- In 1994, the U.S. Army Corps of Engineers (COE) initiated a program to develop and evaluate surface-oriented juvenile salmonid bypass systems at hydroelectric dams on the Columbia and Snake rivers. The goal of the program was to develop juvenile bypass systems that would significantly improve the passage efficiency and survival of juvenile salmonids during their downstream migration. In 1998 a prototype surface collector (PSC) was installed at Bonneville Dam's first powerhouse. The PSC was designed not to bypass fish around the turbines but rather to examine fish behavior and hydraulics at the entrances and to determine the efficacy of surface bypass at BI before building a full production surface bypass system. In 1998 and 1999, our radio telemetry evaluation indicated that only 27-49% of the fish that came within 6 m of the entrances entered the PSC. We also determined that a 6 m entrance width was more efficient than a 1.5 m entrance width. In 2000, the PSC was extended to include turbines 1-6 and each of the six entrances was 6 m wide. To continue our evaluation of the PSC in 2000, we used radio telemetry to examine the movements and behavior of subyearling chinook salmon Oncorhynchus tshawytscha in the forebay of Bonneville Dam. The objectives of this research were to: 1) determine the behavior, distribution, and approach patterns of subyearling chinook salmon in the forebay areas of Bonneville Dam; 2) determine the time and route of dam passage of sub yearling chinook salmon; 3) determine movement patterns and behavior of subyearling chinook salmon in the vicinity of the PSC; and 4) assess the efficiency and effectiveness of the PSC. From 25 April to 1 June 2000, we radio-tagged and released 1,193 juvenile hatchery steelhead and 2,075 yearling chinook salmon. These fish were released from four locations upstream of Bonneville Dam: Rock Creek, John Day Dam, The Dalles Dam, and Hood River, Oregon. Median travel times from release to Bonneville Dam ranged from 14 h to 76 h, depending on species and the location of release. Of all the fish released, we detected 80% of steelhead and 82% of chinook salmon at Bonneville Dam. Of the fish released at Hood River, we detected 95% of steelhead and 94% of chinook salmon. Median residence time in the forebay areas of Bonneville Dam ranged from 8 min to 9 .7 h, depending on species and forebay area. Discharge rates and die! periods effected residence times of both species. Passage routes were determined for 91 % of steelhead and 92% of chinook salmon detected at Bonneville Dam. Nearly half ( 49%) of steelhead passed at powerhouse one (BI), and the largest proportion ( 44%) of chinook salmon passed through the spillway. Thirty-four percent of steelhead detected at Bonneville Dam passed through the spillway. Of the steelhead that passed at Bl, 44% passed into the sluiceway, 33% were guided into the downstream migration channel (DSM) via the standard-length submersible traveling screens (STS) or extended-length submersible bar screens (ESBS), and 23% were unguided and passed directly through the turbines. Of the chinook salmon that passed at Bl, 29% passed into the sluiceway, 36% were guided into the DSM, and 35% were unguided and passed directly through the turbines. Of the fish that passed at B2, 55% of steelhead and 39% of chinook salmon were guided into the DSM by the STS and 45% of steelhead and 60% of chinook salmon passed through the turbines unguided. No steelhead and 1 % of chinook salmon were detected passing through the sluice chute at B2, which was minimally operated during spring 2000. Passage rates were highest for both species during the day at the spillway and B 1. However, passage rates were highest for both species during the night at B2. Of the fish that entered the Bl forebay, 74% of steelhead and 63% of chinook sahnon were detected within 6 m of the PSC and were therefore considered to have discovered the PSC. Of the fish that discovered the PSC, 60% of steelhead and 72% of chinook salmon entered the PSC. However, of the fish that entered the PSC, only 29% (61 of 214) of steelhead and 41 % (100 of 246) of chinook salmon entered the PSC via the entrance they were first detected at without meandering to one or more entrances. Therefore, of the fish that entered the PSC, 71 % (153 of214) of steelhead and 59% (146 of 246) of chinook salmon meandered to one or more entrances before entering the PSC. In relation to units 1-6 at B 1, the PSC was quite efficient at collecting fish. Of the fish that passed at units 1-6 (guided and unguided) 83% of steelhead and 78% of chinook salmon entered the PSC. The PSC was also relatively effective compared to water passing into the turbines and the spillway. An effectiveness of 2.5 for steelhead and 2.4 for chinook salmon indicated that the proportion of fish that entered the PSC out of total passage at units 1-6 was over twice as high as the proportion of discharge that entered the PSC out of total discharge into and under the PSC at units 1-6. When compared to spillway effectiveness (1.0 for steelhead and 1.3 for chinook salmon), PSC effectiveness was about twice as high. Since fish that entered the PSC could pass through other routes, the PSC was not considered an actual passage route for purposes of calculating passage metrics such as FPE. However, if the PSC were an actual passage route, FPE would have increased from 78% to 85% for steelhead and from 73% to 78% for chinook salmon. Title: Passage behavior of radio-tagged yearling chinook salmon and steelhead at Bonneville Dam associated with the Surface Bypass Program, 2000 Abstract -- In 1994, the U.S. Army Corps of Engineers (COE) initiated a program to develop and evaluate surface-oriented juvenile salmonid bypass systems at hydroelectric dams on the Columbia and Snake rivers. The goal of the program was to develop juvenile bypass systems that would significantly improve the passage efficiency and survival of juvenile salmonids during their downstream migration. In 1998 a prototype surface collector (PSC) was installed at Bonneville Dam's first powerhouse. The PSC was designed not to bypass fish around the turbines but rather to examine fish behavior and hydraulics at the entrances and to determine the efficacy of surface bypass at BI before building a full production surface bypass system. In 1998 and 1999, our radio telemetry evaluation indicated that only 27-49% of the fish that came within 6 m of the entrances entered the PSC. We also determined that a 6 m entrance width was more efficient than a 1.5 m entrance width. In 2000, the PSC was extended to include turbines 1-6 and each of the six entrances was 6 m wide. To continue our evaluation of the PSC in 2000, we used radio telemetry to examine the movements and behavior of subyearling chinook salmon Oncorhynchus tshawytscha in the forebay of Bonneville Dam. The objectives of this research were to: 1) determine the behavior, distribution, and approach patterns of subyearling chinook salmon in the forebay areas of Bonneville Dam; 2) determine the time and route of dam passage of sub yearling chinook salmon; 3) determine movement patterns and behavior of subyearling chinook salmon in the vicinity of the PSC; and 4) assess the efficiency and effectiveness of the PSC. From 25 April to 1 June 2000, we radio-tagged and released 1,193 juvenile hatchery steelhead and 2,075 yearling chinook salmon. These fish were released from four locations upstream of Bonneville Dam: Rock Creek, John Day Dam, The Dalles Dam, and Hood River, Oregon. Median travel times from release to Bonneville Dam ranged from 14 h to 76 h, depending on species and the location of release. Of all the fish released, we detected 80% of steelhead and 82% of chinook salmon at Bonneville Dam. Of the fish released at Hood River, we detected 95% of steelhead and 94% of chinook salmon. Median residence time in the forebay areas of Bonneville Dam ranged from 8 min to 9 .7 h, depending on species and forebay area. Discharge rates and die! periods effected residence times of both species. Passage routes were determined for 91 % of steelhead and 92% of chinook salmon detected at Bonneville Dam. Nearly half ( 49%) of steelhead passed at powerhouse one (BI), and the largest proportion ( 44%) of chinook salmon passed through the spillway. Thirty-four percent of steelhead detected at Bonneville Dam passed through the spillway. Of the steelhead that passed at Bl, 44% passed into the sluiceway, 33% were guided into the downstream migration channel (DSM) via the standard-length submersible traveling screens (STS) or extended-length submersible bar screens (ESBS), and 23% were unguided and passed directly through the turbines. Of the chinook salmon that passed at Bl, 29% passed into the sluiceway, 36% were guided into the DSM, and 35% were unguided and passed directly through the turbines. Of the fish that passed at B2, 55% of steelhead and 39% of chinook salmon were guided into the DSM by the STS and 45% of steelhead and 60% of chinook salmon passed through the turbines unguided. No steelhead and 1 % of chinook salmon were detected passing through the sluice chute at B2, which was minimally operated during spring 2000. Passage rates were highest for both species during the day at the spillway and B 1. However, passage rates were highest for both species during the night at B2. Of the fish that entered the Bl forebay, 74% of steelhead and 63% of chinook sahnon were detected within 6 m of the PSC and were therefore considered to have discovered the PSC. Of the fish that discovered the PSC, 60% of steelhead and 72% of chinook salmon entered the PSC. However, of the fish that entered the PSC, only 29% (61 of 214) of steelhead and 41 % (100 of 246) of chinook salmon entered the PSC via the entrance they were first detected at without meandering to one or more entrances. Therefore, of the fish that entered the PSC, 71 % (153 of214) of steelhead and 59% (146 of 246) of chinook salmon meandered to one or more entrances before entering the PSC. In relation to units 1-6 at B 1, the PSC was quite efficient at collecting fish. Of the fish that passed at units 1-6 (guided and unguided) 83% of steelhead and 78% of chinook salmon entered the PSC. The PSC was also relatively effective compared to water passing into the turbines and the spillway. An effectiveness of 2.5 for steelhead and 2.4 for chinook salmon indicated that the proportion of fish that entered the PSC out of total passage at units 1-6 was over twice as high as the proportion of discharge that entered the PSC out of total discharge into and under the PSC at units 1-6. When compared to spillway effectiveness (1.0 for steelhead and 1.3 for chinook salmon), PSC effectiveness was about twice as high. Since fish that entered the PSC could pass through other routes, the PSC was not considered an actual passage route for purposes of calculating passage metrics such as FPE. However, if the PSC were an actual passage route, FPE would have increased from 78% to 85% for steelhead and from 73% to 78% for chinook salmon. Close

• 14. [Article] Willamette Biological Opinion Chinook Reservoir Research 2010

  Abstract -- We investigated life-history characteristics of juvenile Chinook salmon rearing in Cougar and Lookout Point reservoirs. The study objectives were to provide information on juvenile Chinook ...

  Citation × Citation Citation Abstract Copy Title: Willamette Biological Opinion Chinook Reservoir Research 2010 Abstract -- We investigated life-history characteristics of juvenile Chinook salmon rearing in Cougar and Lookout Point reservoirs. The study objectives were to provide information on juvenile Chinook salmon distribution, relative growth rate, predator/prey interactions, and other population characteristics. In addition, we tested the feasibility of various gear-types and techniques for sampling juvenile Chinook salmon rearing in a reservoir environment. A variety of techniques were necessary to capture juvenile Chinook salmon as reservoir conditions and fish behavior, size, and distribution within the reservoir changed throughout the year. Nighttime snorkel surveys were the least invasive and most productive method to investigate habitat utilization and fry distribution early in the Spring. Minnow traps, hoop nets, Lampara seining, and mid-water trawling were largely ineffective at sampling fry and larger-sized juveniles. Oneida Lake trap nets were the most effective at capturing larger-sized juvenile Chinook salmon when reservoir surface temperatures remained cool. Title: Willamette Biological Opinion Chinook Reservoir Research 2010 Abstract -- We investigated life-history characteristics of juvenile Chinook salmon rearing in Cougar and Lookout Point reservoirs. The study objectives were to provide information on juvenile Chinook salmon distribution, relative growth rate, predator/prey interactions, and other population characteristics. In addition, we tested the feasibility of various gear-types and techniques for sampling juvenile Chinook salmon rearing in a reservoir environment. A variety of techniques were necessary to capture juvenile Chinook salmon as reservoir conditions and fish behavior, size, and distribution within the reservoir changed throughout the year. Nighttime snorkel surveys were the least invasive and most productive method to investigate habitat utilization and fry distribution early in the Spring. Minnow traps, hoop nets, Lampara seining, and mid-water trawling were largely ineffective at sampling fry and larger-sized juveniles. Oneida Lake trap nets were the most effective at capturing larger-sized juvenile Chinook salmon when reservoir surface temperatures remained cool. Close

• 15. [Article] Length and age at maturity of female yelloweye rockfish (Sebastes rubberimus) and cabezon (Scorpaenichthys marmoratus) from Oregon waters based on histological evaluation of maturity Information Report number 2009-04

  Abstract -- Accurate estimates of female age or length at maturity are critical for the conservation of exploited fish stocks. Age at maturity is particularly important, as it strongly influences population ...

  Citation × Citation Citation Abstract Copy Title: Length and age at maturity of female yelloweye rockfish (Sebastes rubberimus) and cabezon (Scorpaenichthys marmoratus) from Oregon waters based on histological evaluation of maturity Information Report number 2009-04 Abstract -- Accurate estimates of female age or length at maturity are critical for the conservation of exploited fish stocks. Age at maturity is particularly important, as it strongly influences population model estimates of sustainable harvest rates (Clark 1991) and, along with mean body size, is an important predictor of the risk of overexploitation (Reynolds et al. 2005). For many U.S. west coast groundfish stocks, data on age and length at maturity is of poor quality. The age at maturity curves used in many stock assessments are currently based on macroscopic (visual) assessment of ovary condition. However, there is abundant evidence that histological evaluation of ovarian thin-sections, especially if combined with optimal seasonal sampling, is much more accurate (Gunderson et al. 1980, Wyllie Echeverria 1987, West 1990, Nichol and Pikitch 1994, Hannah and Parker 2007). The age data that have been used to develop curves of age at maturity for some species is also based on outdated ageing methods, such as surface aging of otoliths, as opposed to the more accurate “break and burn” technique (Barss 1989, Wyllie Echeverria 1987, Chilton and Beamish 1982). For other species, such as cabezon (Scorpaenichthys marmoratus), accurate age and growth data, based on thin-sectioning of otoliths, have just recently been developed (Grebel and Cailliet 2003). Information on age and length at maturity that is based on histological evaluation of maturity status and modern ageing techniques is therefore needed for many U.S. west coast groundfish species. Histology-based maturity data has been developed for some U.S. west coast groundfish species. These include darkblotched rockfish (Sebastes crameri, Nichol and Pikitch 1994), petrale sole (Eopsetta jordani, Hannah et al. 2002), greenstriped rockfish (Sebastes elongatus, Shaw and Gunderson 2006), Pacific ocean perch (Sebastes alutus, Hannah and Parker 2007) and rosethorn rockfish (Sebastes helvomaculatus, Shaw and Gunderson 2008). We report here on the development of similar data for female yelloweye rockfish (Sebastes rubberimus) and cabezon. Title: Length and age at maturity of female yelloweye rockfish (Sebastes rubberimus) and cabezon (Scorpaenichthys marmoratus) from Oregon waters based on histological evaluation of maturity Information Report number 2009-04 Abstract -- Accurate estimates of female age or length at maturity are critical for the conservation of exploited fish stocks. Age at maturity is particularly important, as it strongly influences population model estimates of sustainable harvest rates (Clark 1991) and, along with mean body size, is an important predictor of the risk of overexploitation (Reynolds et al. 2005). For many U.S. west coast groundfish stocks, data on age and length at maturity is of poor quality. The age at maturity curves used in many stock assessments are currently based on macroscopic (visual) assessment of ovary condition. However, there is abundant evidence that histological evaluation of ovarian thin-sections, especially if combined with optimal seasonal sampling, is much more accurate (Gunderson et al. 1980, Wyllie Echeverria 1987, West 1990, Nichol and Pikitch 1994, Hannah and Parker 2007). The age data that have been used to develop curves of age at maturity for some species is also based on outdated ageing methods, such as surface aging of otoliths, as opposed to the more accurate “break and burn” technique (Barss 1989, Wyllie Echeverria 1987, Chilton and Beamish 1982). For other species, such as cabezon (Scorpaenichthys marmoratus), accurate age and growth data, based on thin-sectioning of otoliths, have just recently been developed (Grebel and Cailliet 2003). Information on age and length at maturity that is based on histological evaluation of maturity status and modern ageing techniques is therefore needed for many U.S. west coast groundfish species. Histology-based maturity data has been developed for some U.S. west coast groundfish species. These include darkblotched rockfish (Sebastes crameri, Nichol and Pikitch 1994), petrale sole (Eopsetta jordani, Hannah et al. 2002), greenstriped rockfish (Sebastes elongatus, Shaw and Gunderson 2006), Pacific ocean perch (Sebastes alutus, Hannah and Parker 2007) and rosethorn rockfish (Sebastes helvomaculatus, Shaw and Gunderson 2008). We report here on the development of similar data for female yelloweye rockfish (Sebastes rubberimus) and cabezon. Close

• 16. [Article] Warner Valley Fish Investigations- Warner Suckers Progress Reports 2008

  Abstract -- The Warner sucker (Catostomus warnerensis) is endemic to the Warner Valley, an endorheic subbasin of the Great Basin in southeastern Oregon and northwestern Nevada. This species was historically ...

  Citation × Citation Citation Abstract Copy Title: Warner Valley Fish Investigations- Warner Suckers Progress Reports 2008 Abstract -- The Warner sucker (Catostomus warnerensis) is endemic to the Warner Valley, an endorheic subbasin of the Great Basin in southeastern Oregon and northwestern Nevada. This species was historically abundant and its historical range includes three permanent lakes (Hart, Crump, and Pelican), several ephemeral lakes, a network of sloughs and diversion canals, and three major tributary drainages (Honey, Deep, and Twentymile Creeks). Warner sucker abundance and distribution has declined over the past century and it was federally listed as threatened in 1985 due to habitat fragmentation and threats posed by the proliferation of piscivorous non-native game fishes (U.S. Fish and Wildlife Service 1985). The Warner Valley is a northeast-southwest trending endorheic basin which extends approximately 90 km (Figure 1). The elevation of the valley floor is approximately 1,370 m and the basin is bound by fault block escarpments, the Warner Rim on the west and Hart Mountain and Poker Jim Ridge on the east. The Warner basin was formed during the middle Tertiary and late Quaternary geologic periods as a result of volcanic and tectonic activity (Baldwin 1976). Abundant precipitation during the Pleistocene Epoch resulted in the formation of Pluvial Lake Warner (Hubbs and Miller 1948). At its maximum extent approximately 11,000 years ago, the lake reached approximately 100 m in depth and 1,300 km2 in area (Snyder et al. 1964, Weide 1975). In 2008, precipitation and snow pack were near average and Hart and Crump Lakes never filled completely. In 2007, Crump Lake water levels were very low with less than a quarter of the surface area wetted during the winter. Both lakes have been watered continuously since 1993. The Warner sucker inhabits the lakes and low gradient stream reaches of the Warner Valley. Two life history forms are present that comprise the metapopulation of Warner suckers: lake and stream morphs. The lake suckers are lacustrine adfluvial or potamodromous fish which normally spawn in the streams. However, upstream migration may be blocked by low stream flows during dry water years or by irrigation diversion dams and spawning may occur in nearshore areas of the lakes (White et al. 1990). The stream suckers inhabit and spawn in the three major tributary drainages (Honey, Deep, and Twentymile Creeks). Large lake-dwelling populations of introduced fishes in the lakes likely reduce sucker recruitment by predation on young suckers (U.S. Fish and Wildlife Service 1998). The Recovery Plan for the Threatened and Rare Native Fishes of the Warner Basin and Alkali Subbasin (U.S. Fish and Wildlife Service 1998) sets recovery criteria for delisting the species. These criteria require that (1) a self-sustaining metapopulation is distributed throughout the Twentymile, Honey, and Deep Creek (below the falls) drainages, and in Pelican, Crump, and Hart Lakes, (2) passage is restored within and among the Twentymile, Honey, and Deep Creek (below the falls) drainages so that the individual populations of Warner suckers can function as a metapopulation, and (3) no threats exist that would likely threaten the survival of the species over a significant portion of its range. In 2008, we conducted investigations in Hart and Crump Lakes to quantify the abundance and distribution of Warner suckers, to search for evidence of recent recruitment, and to estimate sucker abundance relative to nonnative fish abundance. In addition we investigated growth and movement patterns. We used Passive Integrated Transponder (PIT) tagged suckers to determine growth rates and movements, tracked radio-tagged suckers to document seasonal spawning migrations, fished a screw trap in Twelvemile Creek to monitor downstream movements, and operated a trap at the Dyke diversion dam on Twentymile Creek to monitor upstream movements. Title: Warner Valley Fish Investigations- Warner Suckers Progress Reports 2008 Abstract -- The Warner sucker (Catostomus warnerensis) is endemic to the Warner Valley, an endorheic subbasin of the Great Basin in southeastern Oregon and northwestern Nevada. This species was historically abundant and its historical range includes three permanent lakes (Hart, Crump, and Pelican), several ephemeral lakes, a network of sloughs and diversion canals, and three major tributary drainages (Honey, Deep, and Twentymile Creeks). Warner sucker abundance and distribution has declined over the past century and it was federally listed as threatened in 1985 due to habitat fragmentation and threats posed by the proliferation of piscivorous non-native game fishes (U.S. Fish and Wildlife Service 1985). The Warner Valley is a northeast-southwest trending endorheic basin which extends approximately 90 km (Figure 1). The elevation of the valley floor is approximately 1,370 m and the basin is bound by fault block escarpments, the Warner Rim on the west and Hart Mountain and Poker Jim Ridge on the east. The Warner basin was formed during the middle Tertiary and late Quaternary geologic periods as a result of volcanic and tectonic activity (Baldwin 1976). Abundant precipitation during the Pleistocene Epoch resulted in the formation of Pluvial Lake Warner (Hubbs and Miller 1948). At its maximum extent approximately 11,000 years ago, the lake reached approximately 100 m in depth and 1,300 km2 in area (Snyder et al. 1964, Weide 1975). In 2008, precipitation and snow pack were near average and Hart and Crump Lakes never filled completely. In 2007, Crump Lake water levels were very low with less than a quarter of the surface area wetted during the winter. Both lakes have been watered continuously since 1993. The Warner sucker inhabits the lakes and low gradient stream reaches of the Warner Valley. Two life history forms are present that comprise the metapopulation of Warner suckers: lake and stream morphs. The lake suckers are lacustrine adfluvial or potamodromous fish which normally spawn in the streams. However, upstream migration may be blocked by low stream flows during dry water years or by irrigation diversion dams and spawning may occur in nearshore areas of the lakes (White et al. 1990). The stream suckers inhabit and spawn in the three major tributary drainages (Honey, Deep, and Twentymile Creeks). Large lake-dwelling populations of introduced fishes in the lakes likely reduce sucker recruitment by predation on young suckers (U.S. Fish and Wildlife Service 1998). The Recovery Plan for the Threatened and Rare Native Fishes of the Warner Basin and Alkali Subbasin (U.S. Fish and Wildlife Service 1998) sets recovery criteria for delisting the species. These criteria require that (1) a self-sustaining metapopulation is distributed throughout the Twentymile, Honey, and Deep Creek (below the falls) drainages, and in Pelican, Crump, and Hart Lakes, (2) passage is restored within and among the Twentymile, Honey, and Deep Creek (below the falls) drainages so that the individual populations of Warner suckers can function as a metapopulation, and (3) no threats exist that would likely threaten the survival of the species over a significant portion of its range. In 2008, we conducted investigations in Hart and Crump Lakes to quantify the abundance and distribution of Warner suckers, to search for evidence of recent recruitment, and to estimate sucker abundance relative to nonnative fish abundance. In addition we investigated growth and movement patterns. We used Passive Integrated Transponder (PIT) tagged suckers to determine growth rates and movements, tracked radio-tagged suckers to document seasonal spawning migrations, fished a screw trap in Twelvemile Creek to monitor downstream movements, and operated a trap at the Dyke diversion dam on Twentymile Creek to monitor upstream movements. Close

• 17. [Article] Hult Reservoir (Siuslaw Basin) Fish Species Composition Size and Relative Abundance_Final2018

  Abstract -- Seven species of fish were encountered in Hult Reservoir in 2017: largemouth bass (Micropterus salmoides), cutthroat trout (Oncorhynchus clarkii), tainbow trout/winter steelhead (Oncorhynchus ...

  Citation × Citation Citation Abstract Copy Title: Hult Reservoir (Siuslaw Basin) Fish Species Composition Size and Relative Abundance_Final2018 Abstract -- Seven species of fish were encountered in Hult Reservoir in 2017: largemouth bass (Micropterus salmoides), cutthroat trout (Oncorhynchus clarkii), tainbow trout/winter steelhead (Oncorhynchus mykiss), bluegill (Lepomis macrochirus), reticulate sculpin (Cottus perplexus), brown bullhead (Ameiurus nebulosus) and western brook lamprey (Lampetra richardsoni). The most abundant fish observed were largemouth bass and bluegill in the summer and fall, and cutthroat in the winter. Cutthroat trout were much more prevalent in the fall and winter sampling than in the summer. Presumably, most cutthroat trout moved up into the tributaries to seek thermal refuge during the summer months and returned to the reservoir once the temperatures were more conducive to growth and survival. However, some of them likely moved downstream, were preyed upon, or perished from the high summer temperatures and low dissolved oxygen conditions in the reservoir in summer. Under current conditions, high surface temperature (>20?), bass predation, and hypoxic dissolved oxygen levels below four meters of depth show that reservoir conditions are inhospitable for juvenile salmonids in the summer. Currently there are well established fisheries for both cutthroat trout (spring, fall, winter) and largemouth bass (summer) in the reservoir, and we talked to several anglers who target each of these species. Habitat segregation in the summer between the salmonids who move out of the reservoir and the warm-water fish that remain and spawn in the reservoir results in a diversified year-round angling opportunity. There were no coho salmon (juvenile or adult) observed in Hult Reservoir in 2017, but adult coho salmon were observed spawning just downstream of the dam. This observation verifies that a proportion of the adult coho attempting to ascend the ladder at Lake Creek Falls are successful and continue migration upstream to the vicinity of Hult Reservoir. It may be possible to keep the current fishery in Hult Reservoir as it stands and still increase coho production in the system by improving adult passage at Lake Creek Falls, and possibly at Hult Dam. Title: Hult Reservoir (Siuslaw Basin) Fish Species Composition Size and Relative Abundance_Final2018 Abstract -- Seven species of fish were encountered in Hult Reservoir in 2017: largemouth bass (Micropterus salmoides), cutthroat trout (Oncorhynchus clarkii), tainbow trout/winter steelhead (Oncorhynchus mykiss), bluegill (Lepomis macrochirus), reticulate sculpin (Cottus perplexus), brown bullhead (Ameiurus nebulosus) and western brook lamprey (Lampetra richardsoni). The most abundant fish observed were largemouth bass and bluegill in the summer and fall, and cutthroat in the winter. Cutthroat trout were much more prevalent in the fall and winter sampling than in the summer. Presumably, most cutthroat trout moved up into the tributaries to seek thermal refuge during the summer months and returned to the reservoir once the temperatures were more conducive to growth and survival. However, some of them likely moved downstream, were preyed upon, or perished from the high summer temperatures and low dissolved oxygen conditions in the reservoir in summer. Under current conditions, high surface temperature (>20?), bass predation, and hypoxic dissolved oxygen levels below four meters of depth show that reservoir conditions are inhospitable for juvenile salmonids in the summer. Currently there are well established fisheries for both cutthroat trout (spring, fall, winter) and largemouth bass (summer) in the reservoir, and we talked to several anglers who target each of these species. Habitat segregation in the summer between the salmonids who move out of the reservoir and the warm-water fish that remain and spawn in the reservoir results in a diversified year-round angling opportunity. There were no coho salmon (juvenile or adult) observed in Hult Reservoir in 2017, but adult coho salmon were observed spawning just downstream of the dam. This observation verifies that a proportion of the adult coho attempting to ascend the ladder at Lake Creek Falls are successful and continue migration upstream to the vicinity of Hult Reservoir. It may be possible to keep the current fishery in Hult Reservoir as it stands and still increase coho production in the system by improving adult passage at Lake Creek Falls, and possibly at Hult Dam. Close

• 18. [Article] Abundance Monitoring of Juvenile Salmonids In Coastal Oregon and Lower Columbia Streams, 2008 Report Number: OPSW-ODFW-2009-1

  Abstract -- As part of the Oregon Plan for Salmon and Watersheds, the Oregon Department of Fish and Wildlife (ODFW) initiated this project in 1998 to monitor the status and trend in abundance and distribution ...

  Citation × Citation Citation Abstract Copy Title: Abundance Monitoring of Juvenile Salmonids In Coastal Oregon and Lower Columbia Streams, 2008 Report Number: OPSW-ODFW-2009-1 Abstract -- As part of the Oregon Plan for Salmon and Watersheds, the Oregon Department of Fish and Wildlife (ODFW) initiated this project in 1998 to monitor the status and trend in abundance and distribution of juvenile coho salmon (Oncorhynchus kisutch) in coastal Oregon streams. This report summarizes the data collected during the summer of 2008 and, for coho salmon, compares it to data previously collected. The project originally surveyed only 1st-3rd order (tributary) streams but was expanded in 2002 to include juvenile steelhead (Oncorhynchus mykiss) and 4th-6th order (mainstem) rearing areas and in 2006 to the Oregon portion of the Lower Columbia River coho evolutionarily significant unit (ESU) (Figure 1). The sampling frame is intended to encompass all non-tidal coho and steelhead rearing habitat. The original 100k stream layer frame was replaced by a 24k frame in 2007. A Generalized Random Tessellation Stratified design (GRTS) (Stevens 2002) was used to create a spatially balanced, random point distribution. Sites were stratified by Monitoring Area (MA) and stream order (Table 1). A detailed description of the sampling frames and survey designs are found in Jepsen and Rodgers (2004) and Jepsen and Leader (2007). Field crews snorkeled all pools meeting the size criteria (6 m2 in surface area and 40 cm in maximum depth) in one kilometer of stream encompassing the GRTS point. Snorkeling was conducted during the minimum flow period from July to September using a single pass of one to four snorkelers, depending on stream width. In each pool counts were made of juvenile coho, Chinook, steelhead 90 mm, and cutthroat 90 mm. Presence was noted for dace, shiners, and trout < 90 mm. Sites with poor water clarity or quality were electrofished using a single pass without block nets to determine presence for coho, steelhead and cutthroat in each pool. To assess repeatability and quality control supervisory staff resurveyed 10% of tributary sites in each MA. Data were summarized by MA and stream order for analyses. Average pool density and percent pool occupancy for each site was averaged by MA. The percent of sites with at least one fish and with >0.7 coho/m2 are reported for each MA. 0.7 coho/m2 is regarded as full seeding after Nickelson et al. (1992) who reported full seeding based on electrofishing as 1.0 coho/m2 and Rodgers et al. (1992) who found that snorkelers observed 70% of the coho counted by electrofishing. CDFs, variances, and confidence intervals were created using tools developed by the EMAP Design and Analysis Team (EPA 2009). Title: Abundance Monitoring of Juvenile Salmonids In Coastal Oregon and Lower Columbia Streams, 2008 Report Number: OPSW-ODFW-2009-1 Abstract -- As part of the Oregon Plan for Salmon and Watersheds, the Oregon Department of Fish and Wildlife (ODFW) initiated this project in 1998 to monitor the status and trend in abundance and distribution of juvenile coho salmon (Oncorhynchus kisutch) in coastal Oregon streams. This report summarizes the data collected during the summer of 2008 and, for coho salmon, compares it to data previously collected. The project originally surveyed only 1st-3rd order (tributary) streams but was expanded in 2002 to include juvenile steelhead (Oncorhynchus mykiss) and 4th-6th order (mainstem) rearing areas and in 2006 to the Oregon portion of the Lower Columbia River coho evolutionarily significant unit (ESU) (Figure 1). The sampling frame is intended to encompass all non-tidal coho and steelhead rearing habitat. The original 100k stream layer frame was replaced by a 24k frame in 2007. A Generalized Random Tessellation Stratified design (GRTS) (Stevens 2002) was used to create a spatially balanced, random point distribution. Sites were stratified by Monitoring Area (MA) and stream order (Table 1). A detailed description of the sampling frames and survey designs are found in Jepsen and Rodgers (2004) and Jepsen and Leader (2007). Field crews snorkeled all pools meeting the size criteria (6 m2 in surface area and 40 cm in maximum depth) in one kilometer of stream encompassing the GRTS point. Snorkeling was conducted during the minimum flow period from July to September using a single pass of one to four snorkelers, depending on stream width. In each pool counts were made of juvenile coho, Chinook, steelhead 90 mm, and cutthroat 90 mm. Presence was noted for dace, shiners, and trout < 90 mm. Sites with poor water clarity or quality were electrofished using a single pass without block nets to determine presence for coho, steelhead and cutthroat in each pool. To assess repeatability and quality control supervisory staff resurveyed 10% of tributary sites in each MA. Data were summarized by MA and stream order for analyses. Average pool density and percent pool occupancy for each site was averaged by MA. The percent of sites with at least one fish and with >0.7 coho/m2 are reported for each MA. 0.7 coho/m2 is regarded as full seeding after Nickelson et al. (1992) who reported full seeding based on electrofishing as 1.0 coho/m2 and Rodgers et al. (1992) who found that snorkelers observed 70% of the coho counted by electrofishing. CDFs, variances, and confidence intervals were created using tools developed by the EMAP Design and Analysis Team (EPA 2009). Close