It’s the most wonderful time of the year. BBQs, ice cream, cabin trips… and the upriver sockeye salmon spawning migration in British Columbia, Canada is in full swing! Each year millions of sockeye salmon return to the Fraser River to migrate to the same stream where they were born in order to spawn. The upriver migration is a biological wonder. Salmon cease feeding in the ocean, so upriver swimming, morphological changes, and spawning behaviours are fueled entirely by energy stores. The fish develop impressive secondary sexual characteristics during the migration, turning bright red and green, and males develop a pronounced dorsal hump and kype (hooked jaw). Some populations travel over 1,000 km in just a few weeks – traversing rapids, and avoiding predators and fisheries gear. Sockeye salmon have a single opportunity to reproduce and naturally die shortly after spawning (semelparity). Consequently, an individual fish that does not make it back to the spawning ground will have zero lifetime reproductive success.
Male sockeye salmon migrating upstream. Pic 1 - photo credit: M. Casselman
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Our research team has spent the past couple
of weeks on the side of the Fraser River, tagging and collecting sockeye salmon
for our experiments. Unfortunately, it is hot. Very hot. As in, we’re wearing bathing suits instead of waders and
diving into the river to cool off every chance we get. There is simply not
enough beer and ice cream to beat the heat.
Healthy salmon on the spawning ground look
like this. Pic 2 – photo credit: M. Casselman
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When temperatures soar, salmon can start to
look like this. Pic 3 – photo credit: A. Teffer
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Fig 1: Aerobic scope as a function of upriver migration distance for 8 populations of Fraser River sockeye salmon. Data from Eliason et al., 2011; 2013b. |
In addition, sockeye salmon populations encounter varying temperatures depending on when they enter the river and where they spawn. Functional thermal tolerance for each population appears to be tailored to the typical environmental temperatures encountered (Eliason et al., 2011). For example, Weaver Creek sockeye salmon typically migrate upstream in the cool fall months, and they have a correspondingly lower functional thermal tolerance compared to populations that migrate in warm summer temperatures. Chilko sockeye salmon have the highest and broadest thermal tolerance of all the Fraser River populations studied to date. They enter the Fraser River in the middle of the summer and encounter peak river temperatures while migrating through the most challenging sections of the river, but spend the final third of their migration traveling up a cool glacial river to finally spawn in or adjacent to a glacial lake at ~1,200 m in elevation. Collectively, these results provide compelling, though not conclusive, evidence that Fraser River sockeye salmon populations are locally adapted to their upriver migratory environment.
Functional thermal tolerance has been determined for 7 populations so far (Eliason et al., 2011; 2013b) and management agencies are able to use this information to predict how the different populations may fare in a given year. If river temperatures exceed the functional thermal tolerance for populations currently in the river, fisheries can be shut down to enable more fish to arrive on the spawning grounds. This year, we expect many of the returning salmon to be from the Chilko population. This presents us with an interesting natural experiment – how will the super-high-temperature-tolerant population cope with this exceptionally warm year? How will the other co-migrating populations with lower thermal tolerance fare? Tagging experiments from our research group will link migration rates and migration success with river temperature, disease profiles, and population differences.
This work is currently being expanded in a few different directions. On the one hand, I’m interested in the physiological mechanisms that determine thermal tolerance. Cardiac function appears to be the primary factor limiting functional thermal tolerance in salmon (Eliason et al., 2013a; Farrell et al., 2009). Specifically, swimming performance and aerobic capacity decline at warm temperatures due to an inability of the heart to deliver sufficient oxygen to the working muscles (Eliason et al., 2013a). Indeed, Chilko sockeye salmon hearts have an enhanced ability to use adrenaline, which increases cardiac capacity and protection and likely confers a higher thermal tolerance compared to other populations (Eliason et al., 2011). We’re currently trying to understand what other cellular and molecular mechanisms are important for maintaining cardiac function at high temperature.
We’re also interested in the broader
implications of these climate-driven ecological changes on the population and
community dynamics. Pacific salmon are keystone species in the Pacific
Northwest. How do fluctuations in their abundance or migration timing impact
the larger community? Pacific salmon are not just ecologically, but also
economically and culturally important fish species. What are the economic,
social and cultural implications for humans? Almost all of our work thus far
has focused on how ecology is shaping evolution in salmon, but it’s very
interesting to also consider how evolutionary change might influence ecology in
this system.
If Chilko sockeye salmon are so great, why don’t we just spread their genes all over the Fraser River watershed to save the salmon? This question gets me riled up every time. The research outlined above is focused on a single, brief time period in the life cycle of salmon. The upriver migration only lasts ~4 weeks and thus represents ~2% of the lifespan of a sockeye salmon. The other 98% of the time is spent on spawning grounds, incubating as eggs, rearing in their natal lake as fry, migrating downstream to the ocean as smolts, and feeding and growing in the ocean for a couple of years as sub-adults and adults. The environmental conditions and selection pressures vary widely across the life cycle and among habitats. It would be foolish to assume that traits are fixed across all life stages (i.e. no phenotypic plasticity), or that traits beneficial for one environment are advantageous in all environments. In fact, Chilko sockeye salmon eggs incubate in a cool alpine lake or stream, and studies have shown that Chilko eggs have a correspondingly lower thermal tolerance compared to populations that incubate at warmer temperatures (Whitney et al., 2013, 2014). Given the broad environmental heterogeneity across salmonid habitats, and the uncertain future with respect to ongoing climate change, we should be focusing on preserving biodiversity and maintaining sufficient genetic and phenotypic variability within the species.
Will Fraser River sockeye salmon adapt fast enough to keep pace with climate change? The short answer? I don’t know. The long answer? Fraser River temperatures have increased by ~2°C over the last 60 years (Patterson et al., 2007), and are expected to continue to increase along the same trajectory. In order to cope with warming river temperatures, salmon will need to undergo some combination of behavioural and physiological adaptation.
Fig 4: Yearly maximum Summer Fraser River Temperatures. Data from Patterson et al., 2007. |
The other option is to increase their
physiological thermal tolerance, by improving cardiorespiratory performance at
high temperature for example. Some salmonid populations do have the capacity to
cope with warm temperatures – redband trout in Oregon can encounter summer
river temperatures between 24 and 30°C (Rodnick
et al., 2004). Hatchery-reared rainbow trout in southern Western
Australia have undergone passive selection over 19 generations to increase
thermal tolerance (Chen et al., 2015).
Studies have shown that rapid evolution can occur in salmon populations over
just 11–30 generations (Hendry et al., 2000;
Quinn and Adams, 1996; Quinn et al., 2000). However, 11–30 generations
is a fairly long time, since Fraser River sockeye salmon typically have a 4
year life cycle; we’re talking about 44–120 years.
All told, salmon are remarkably resilient.
So it’s not all doom and gloom, and I wouldn’t count Fraser River sockeye
salmon out just yet.
References:
Chen, Z., Snow, M.,
Lawrence, C.S., Church, A.R., Narum, S.R., Devlin, R.H., Farrell, A.P., 2015.
Selection for upper thermal tolerance in rainbow trout (Oncorhynchus mykiss
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Crossin, G.T., Hinch,
S.G., Farrell, A.P., Higgs, D.A., Lotto, A.G., Oakes, J.D., Healey, M.C., 2004.
Energetics and morphology of sockeye salmon: effects of upriver migratory
distance and elevation. Journal of Fish Biology 65, 788-810.
Eliason, E.J., Clark, T.D., Hague, M.J., Hanson, L.M., Gallagher, Z.S.,
Jeffries, K.M., Gale, M.K., Patterson, D.A., Hinch, S.G., Farrell, A.P., 2011.
Differences in thermal tolerance among sockeye salmon populations. Science 332,
109-112.
Eliason, E.J., Clark, T.D., Hinch, S.G., Farrell, A.P., 2013a.
Cardiorespiratory collapse at high temperature in swimming adult sockeye
salmon. Conservation Physiology 1, 10.1093/conphys/cot1008.
Eliason, E.J., Wilson, S.M., Farrell, A.P., Cooke, S.J., Hinch, S.G.,
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Farrell, A.P., Eliason, E.J., Sandblom, E., Clark, T.D., 2009. Fish
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Hinch, S.G., Martins, E.G., 2011. A review of potential climate change
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interannual trends in en route loss and pre-spawn mortality. Cohen Commission Technical
Report 9, Vancouver, B.C., pp 1-134. www.cohencommission.ca
Patterson, D.A., Macdonald, J.S., Skibo, K.M., Barnes, D.P., Guthrie, I.,
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River, 1941 to 2006, and implications for adult sockeye salmon (Oncorhynchus nerka) spawning migration.
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Reed, T.E., Schindler, D.E., Hague, M.J., Patterson, D.A., Meir, E.,
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Rodnick, K.J., Gamperl, A.K., Lizars, K.R., Bennett, M.T., Rausch, R.N.,
Keeley, E.R., 2004. Thermal tolerance and metabolic physiology among redband trout
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Taylor, E.B., 1991. A review of local adaptation in Salmonidae, with
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