Migration timing and tributary use of spawning flannelmouth sucker (Catostomus latipinnis)
Corresponding Author
Sophia M. Bonjour
Division of Biology, Kansas State University, Manhattan, Kansas, USA
Correspondence
Sophia M. Bonjour, Division of Biology, Kansas State University, 116 Ackert Hall, Manhattan, KS 66506, USA.
Email: [email protected]
Search for more papers by this authorKeith B. Gido
Division of Biology, Kansas State University, Manhattan, Kansas, USA
Search for more papers by this authorMark C. McKinstry
Upper Colorado Regional Office, U.S. Bureau of Reclamation, Salt Lake City, Utah, USA
Search for more papers by this authorCharles N. Cathcart
Alaska Department of Fish and Game, Alaska Freshwater Fish Inventory, Anchorage, Alaska, USA
Search for more papers by this authorMatthew R. Bogaard
Washington Department of Fish and Wildlife, Washington, District of Columbia, USA
Search for more papers by this authorMaria Dzul
U.S. Geological Survey, Southwest Biological Science Center, Grand Canyon Monitoring and Research Center, Flagstaff, Arizona, USA
Search for more papers by this authorBrian D. Healy
U.S. Geological Survey, Eastern Ecological Science Center at Patuxent Research Refuge, Laurel, Maryland, USA
Search for more papers by this authorZachary E. Hooley-Underwood
Colorado Parks and Wildlife, Montrose, Colorado, USA
Search for more papers by this authorDavid L. Rogowski
Arizona Game and Fish Department, Phoenix, Arizona, USA
Search for more papers by this authorCharles B. Yackulic
U.S. Geological Survey, Southwest Biological Science Center, Grand Canyon Monitoring and Research Center, Flagstaff, Arizona, USA
Search for more papers by this authorCorresponding Author
Sophia M. Bonjour
Division of Biology, Kansas State University, Manhattan, Kansas, USA
Correspondence
Sophia M. Bonjour, Division of Biology, Kansas State University, 116 Ackert Hall, Manhattan, KS 66506, USA.
Email: [email protected]
Search for more papers by this authorKeith B. Gido
Division of Biology, Kansas State University, Manhattan, Kansas, USA
Search for more papers by this authorMark C. McKinstry
Upper Colorado Regional Office, U.S. Bureau of Reclamation, Salt Lake City, Utah, USA
Search for more papers by this authorCharles N. Cathcart
Alaska Department of Fish and Game, Alaska Freshwater Fish Inventory, Anchorage, Alaska, USA
Search for more papers by this authorMatthew R. Bogaard
Washington Department of Fish and Wildlife, Washington, District of Columbia, USA
Search for more papers by this authorMaria Dzul
U.S. Geological Survey, Southwest Biological Science Center, Grand Canyon Monitoring and Research Center, Flagstaff, Arizona, USA
Search for more papers by this authorBrian D. Healy
U.S. Geological Survey, Eastern Ecological Science Center at Patuxent Research Refuge, Laurel, Maryland, USA
Search for more papers by this authorZachary E. Hooley-Underwood
Colorado Parks and Wildlife, Montrose, Colorado, USA
Search for more papers by this authorDavid L. Rogowski
Arizona Game and Fish Department, Phoenix, Arizona, USA
Search for more papers by this authorCharles B. Yackulic
U.S. Geological Survey, Southwest Biological Science Center, Grand Canyon Monitoring and Research Center, Flagstaff, Arizona, USA
Search for more papers by this authorAbstract
Spawning phenology and associated migrations of fishes are often regulated by factors such as temperature and stream discharge, but flow regulation of mainstem rivers coupled with climate change might disrupt these cues and affect fitness. Flannelmouth sucker (Catostomus latipinnis) persisting in heavily modified river networks are known to spawn in tributaries that might provide better spawning habitat than neighboring mainstem rivers subject to habitat degradation (e.g., embedded sediments, altered thermal regimes, and disconnected floodplains). PIT tag data and radio telemetry were used to quantify the timing and duration of flannelmouth sucker tributary spawning migrations in relation to environmental cues in McElmo Creek, a tributary of the San Juan River in the American Southwest. We also tested the extent of the tributary migration and assessed mainstem movements prior to and after tributary migrations. Additionally, multiyear data sets of PIT detections from other tributaries in the Colorado River basin were used to quantify interannual and cross-site variation in the timing of flannelmouth sucker spawning migrations in relation to environmental cues. The arrival and residence times of fish spawning in McElmo Creek varied among years, with earlier migration and a 3-week increase in residence time in relatively wet years compared to drier years. Classification tree analysis suggested a combination of discharge- and temperature-determined arrival timing. Of fish PIT tagged in the fall, 56% tagged within 10 km of McElmo Creek spawned in the tributary the following spring, as did 60% of radio-tagged fish, with a decline in its use corresponding to increased distance of tagging location. A broader analysis of four tributaries in the Colorado River basin, including McElmo Creek, found photoperiod and temperature of tributary and mainstem rivers were the most important variables in determining migration timing, but tributary and mainstem discharge also aided in classification success. The largest tributary, the Little Colorado River, had more residential fish or fish that stayed for longer periods (median = 30 days), whereas McElmo Creek fish stayed an average of just 10 days in 2022. Our results generally suggest that higher discharge, across years or across sites, results in extended use of tributaries by flannelmouth suckers. Conservation actions that limit water extraction and maintain natural flow regimes in tributaries, while maintaining open connection with mainstem rivers, may benefit migratory species, including flannelmouth suckers.
Supporting Information
Filename | Description |
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jfb15509-sup-0001-Figures.docxWord 2007 document , 1.5 MB | Figure S1. Mean daily discharge for McElmo Creek (USGS 09372000) and the San Juan River (USGS 09379500). Figure S2. Mean residence days in McElmo Creek, Utah, and mean discharge between January and June. F(1,6) = 16.08, p = 0.007, adjusted R2 = 0.63. Figure S3. Cumulative plots of flannelmouth sucker (Catostomus latipinnis) arrivals for each year across sites. The x-axis shows (a) the photoperiod (h) to represent the time of year but also accounts for some of the latitudinal displacement among sites and (b) tributary mean daily temperature. BAC, Bright Angel Creek; LCR, Little Colorado River. Figure S4. Partial dependence of environmental factors in the random forest model for all tributaries. |
Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.
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