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
Healthy salmon on the spawning ground look like this. Pic 2 – photo credit: M. Casselman
When temperatures soar, salmon can start to look like this. Pic 3 – photo credit: A. Teffer
|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.
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.|