The timing of adult sockeye salmon migration into fresh water: adaptations by populations to prevailing thermal regimes
By Sayre Hodgson, Thomas R. Quinn. 2002
223 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/9029b99861b6d37013f20ce3a82bd58fe54ba4f3
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In Global and Planetary Change
In Nature and Landscape Conservation
Citations in the corpus
- Long-term changes in migration timing of adult Atlantic salmon (Salmo salar) at the southern edge of the species distribution (2004, background): “For example, variation in the migration timing among sockeye salmon (Oncorhynchus nerka) populations is primarily related to temperature (Hodgson and Quinn 2002), and the earlier upriver migration of sockeye in the Columbia River is correlated with long-term changes in temperature and river flow (Qu”
- A collective navigation hypothesis for homeward migration in anadromous salmonids (2016, background): “Second, popula tions within watersheds often differ in the timing of their return to freshwater, which largely reflects differences in thermal regimes on the spawning grounds (Hodgson and Quinn 2002; Doctor et al. 2010; Eliason et al. 2011).”
- Exposure to high temperature influences the behaviour, physiology, and survival of sockeye salmon during spawning migration (2008, background): “…Artedi, 1792) begin their spawning migrations through the Fraser River of British Columbia, Canada, and for a given population, the timing of river entry rarely deviates by more than a week interannually (Woodey 1987), though timing can vary appreciably among populations (Hodgson and Quinn 2002).”
- Anadromy and the marine migrations of Pacific salmon and trout: Rounsefell revisited (2004, unknown): “…with long migrations; rather, they are coastal populations in the southern end of the range that avoid warm temperatures in late summer by entering earlier in the year and remaining below the thermocline in lakes until they enter tributaries to spawn in the fall (Hodgson and Quinn, 2002).”
- Reconstructing the Summer Thermal History for the Lower Fraser River, 1941 to 2006, and Implications for Adult Sockeye Salmon (Oncorhynchus nerka) Spawning Migration (2007, background): “The actual timing of river migration is likely bounded by spawning times (Hodgson and Quinn 2002).”
- Comparison of Life History Traits between First-Generation Hatchery and Wild Upper Yakima River Spring Chinook Salmon (2006, background): “Adult passage timing.—We analyzed passage timing by return year rather than BY, because although populations of adult Pacific salmon demonstrate consistent patterns in upstream migration timing, there can be significant year-to-year variation resulting from interannual differences in river discharge”
- Late-season mortality during migration of radio-tagged adult sockeye salmon (Oncorhynchus nerka) in the Columbia River (2005, background): “For example, Columbia River and interior British Columbia stocks of sockeye salmon tend to enter fresh water before peak summer temperatures and hold in spawning tributaries for 1 month or more before fall spawning whereas coastal stocks migrate after peak temperatures just prior to spawning (Gilhou”
- Global climate change and potential effects on Pacific salmonids in freshwater ecosystems of southeast Alaska (2009, background): “In southeast Alaska, stream water temperatures range from freezing to about 20◦C and generally are less than 10◦C in most streams during most of the year (Fig. 2). Anadromous salmon in southeast Alaska are cold water species and have spawning, incubation, and growth characteristics that are tuned to”
- The paradox of “premature migration” by adult anadromous salmonid fishes: patterns and hypotheses (2016, background): “Likewise, similar timing patterns are seen 504 among populations in different river systems that share similar physical conditions such as the 505 sockeye salmon towards the southern end of their distribution that enter early, hold in lakes all 506 summer, and spawn in fall (Hodgson and Quinn 2002).”
- Endogenous Programs and Flexibility in Bird Migration (2020, background): “…of relevant environmental factors, such as nutrients (Newton, 2008; Häfker et al., 2017), breeding site or mate availability (Barlow et al., 1986; Hodgson and Quinn, 2002; Friesen, 2015), predation risk (McKinnon et al., 2010; Häfker et al., 2017), infection probability (O’Connor et al., 2018),…”
- Hydrosystem, Dam, and Reservoir Passage Rates of Adult Chinook Salmon and Steelhead in the Columbia and Snake Rivers (2004, background): “Timing, which integrates environmental conditions and the maturation changes occurring for adult migrants, can be a good predictor of fish activity (Økland et al. 2001; Hodgson and Quinn 2002).”
- Effect of water temperature, timing, physiological condition, and lake thermal refugia on migrating adult Weaver Creek sockeye salmon (Oncorhynchus nerka) (2010, background): “Unsuccessful migration could be a result of many high-temperature-mediated factors (Quinn et al. 1997; Hodgson and Quinn 2002), such as the collapse of aerobic scope (Farrell 2002; Farrell et al.”
- Homing and straying by anadromous salmonids: a review of mechanisms and rates (2014, background): “For example, many populations migrate long distances in freshwater and then hold for weeks to months before fully maturing (Berman and Quinn 1991; Hansen and Jonsson 1991; Økland et al. 2001; Hodgson and Quinn 2002).”
- Ecological and Evolutionary Consequences of Environmental Change and Management Actions for Migrating Fish (2019, background): “, temperature, precipitation, light regime and water flow) along latitudinal and altitudinal gradients and local climate (Hodgson and Quinn, 2002; Dodson et al., 2013), but a growing body of evidence suggests that genetic components are also involved (Skov et al.”
- Stock-Specific Migration Timing of Adult Spring–Summer Chinook Salmon in the Columbia River Basin (2004, background): “Examples of such stocks include some sockeye salmon ( Hodgson and Quinn 2002 ) and steelhead ( Robards and Quinn 2002 ) that migrate well before spawning periods to avoid high water temperatures in migration corridors, and Atlantic salmon Salmo salar that time migration to avoid low flows ( Hansen”
- The effect of exercise and captivity on energy partitioning, reproductive maturation and fertilization success in adult sockeye salmon (2004, background): “…swimming behaviour, adjusting run timing to coincide with favourable river conditions, elevating swimming performance capability and increasing lipid reserves to fuel long and difficult migrations (Gilhousen, 1980; Brett, 1995; Hinch & Rand, 1998; Hodgson & Quinn, 2002; Lee et al., 2003).”