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Natural History
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Aquatic Ecosystem Topics

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Biodiversity

"The normal functioning of our diverse ecosystems depends on the biodiversity of all species, including fish. Fish need a healthy habitat to survive, declining fish populations reflect an unhealthy and unstable ecosystem." MOELP Fisheries website

History of People and Water in the Columbia Basin

1500 BC to the 1990s

When the first inhabitants migrated to the Columbia Basin, 3,500 years ago, they found jagged mountain ranges and valleys full of moist, dense cedar, hemlock and fir forests laced with streams, rivers and lakes. The diversity of plants, animals and geography formed the foundation of a rich native culture. Anadromous (migratory) chinook and sockeye salmon, steelhead trout and white sturgeon migrated up the Columbia River from the Pacific Ocean to spawn in the River's upper reaches, providing food for the forest animals and replenishing the nutrients in the waterways. The culture of the Kootenai Indians evolved around these migratory fish runs which provided food for them and other wildlife in the area (see Earliest Beginnings). They also fished for the rainbow trout, burbot, whitefish and bull trout which flourished in the lakes.

The waterways of the Columbia Basin provided transportation up and down the valleys for the native populations and later for the early explorers. One of the first recorded exploration trips up the Columbia River into Arrow Lakes is Emilius Simpson's 1826 trip. He noted "The Arrow Rock, so named on account of a round hole in the face full of Arrows, said to have been fired at it by the Indians when practicing the Bow and Arrow before a war excursion." (Journal of Emilius Simpson, HBC Archives B223/a/3 1826 Folio 39D-41). This wall of arrows is the source of the name "Arrow Lakes".

Non-native settlement in the Columbia Basin was established when the industrial value was realized, with mining and logging attracting many people to the area. Transportation was the most recognized value of the waterways, with paddlewheelers hauling people and goods up and down the networks of lakes and rivers. Many communities flourished in the valley bottoms, where fertile soil provided great farming. Later, in the 1900s, the hydroelectric potential of rivers of the Columbia Basin led to the damming of several lakes and rivers (see Aquatic Ecosystem Structure). The area's biodiversity began to falter with the intense industrial pressure from forestry, mining, manufacturing and hydroelectric power production.

By the early 1990s, people began to grasp the full impact of human intervention on the aquatic ecosystems of the Columbia Basin. Not only were the large lakes and rivers in a state of ecosystem collapse as a result of being dammed, but small streams and entire watersheds were in jeopardy, also, from the intrusions of industry. Indeed, the rich aquatic biodiversity of the region currently rests in a precarious state, and residents, researchers, governments and industry agents are working together to ensure the waterways of the Columbia Basin flourish again (see Aquatic Ecosystem Management).

The Arrow Lakes Kokanee Connection
Figure 1. Kokanee Spawning (BC Environment, data)

Kokanee salmon are an important sports fish throughout the Kootenays and a critically important food source for the larger sport fish: bull trout, rainbow trout and burbot. An alarming downward trend in kokanee numbers was noted by anglers and fisheries biologists throughout the 1990s, similar to the observations leading to the fertilization of Kootenay Lake. Although it was known that damming the Columbia River at Castlegar, Revelstoke and Mica (see Ecosystem Structure) eliminated 30% of the Arrow Lakes' kokanee spawning and rearing habitat, as well as a good proportion of the rainbow trout and bull trout spawning habitat, it didn't explain the precipitous drop in populations well after the dams were built.

Figure 2. Kokanee Out-migration and Fry Survival (BC Environment data)

Suspicions that something was wrong with Arrow Lakes itself, rather than the hatchery or some other problem, were fueled by the discovery that the survival of fry (baby fish) counted migrating out from the hatchery and again returning as adults was also declining precipitously (Figure 2, left). This suggested that, once in the lake, the fish were not getting enough to eat to grow and to escape their predators. Possible alternative explanations, such as a marked increase in predator populations or a disease, were ruled out by intensive research that began in cooperation with the University of British Columbia, the Ministry of Environment, Lands and Parks, BC Hydro and Columbia Basin Fish and Wildlife Compensation Program.

The research, which includes studies of water quality, bathymetry, limnology, nutrient sources, phytoplankton (below), zooplankton (below), mysis shrimp and kokanee, demonstrated Arrow Lakes was in a state of ecosystem collapse. After discussing these results in a series of scientific and public workshops and meetings, fertilizing began in Arrow Lake in the spring of 1999 to stimulate production in the troubled aquatic ecosystem.

Sport Fishing

Sport fishing has always been popular in the Columbia Basin. While trophy fishing for bull trout and rainbow trout provides great adventure and eating; other species including burbot, kokanee and whitefish are desirable catches also. Almost all accessible small lakes in the area are stocked with Cutthroat, rainbow or brook trout raised in the Kootenay Trout Hatchery, which, in 1996, provided 1.25 million fish for release into 174 different lakes (Thorp, BC MOELP, personal communication). Some small, glacially-fed alpine lakes in the area are currently being assessed for suitability for stocking to provide an even broader range of fishing opportunities (Bray, CBFWCP, personal communication). Fly fishing is popular in the streams and smaller lakes, while trolling the lakes for the big fish is rewarding year-round, whether in the icy cold of winter or summer's lush heat. Fishing attracts tourists from all over the region, country and world, many of whom make annual pilgrimmages to Columbia Basin lakes. It is not just the draw of "food in your belly" that brings locals and tourists out onto the water but something deeper and less definable, more spiritual and far more nourishing. As Glen Olson, third generation angler and Arrow Lakes fishing charter operator said, "It's kind of hard to explain, but they're so beautiful it's almost a shame to kill them. Sometimes they look like rainbows lying in the bottom of your boat." (from Welcome Home, Stuart McLean, 1992). For more information, link to http://www.fishbc.com or http://www.bcadventure.com

Phytoplankton - The Foundation of Aquatic Life

The entire food chain in lakes is based on algae. The algae found in the aquatic ecosystem are more technically known as phytoplankton, meaning plants suspended in water. Phytoplankton are photosynthetic, meaning they use the energy of the sun to convert carbon dioxide into high-energy carbohydrates. When consumers graze upon algae, the energy held in the carbohydrates is transferred to the consuming animal, which are then consumed by the next level of the food chain, and the energy is passed on again. Algae thus provide the energy for all other growth in the lakes and streams.

Phytoplankton are autotrophic photosynthesizers, creating their own food by converting sunlight into sugars. Because they need to be where the sunlight can penetrate, phytoplankton spend at least some of their time in the light-filled limnetic zone. Some of them are able to move around by using flagella. Phytoplankton also feed the insects, crustaceans and decomposers living in the profundal zone of the lake by sinking to the lower levels when they die.

All phytoplankton need carbon, potassium, sulfur, calcium, nitrogen and phosphorus molecules to help build their proteins and other growth molecules; they cannot make their own nutrient molecules and must therefore get them from the water in which they live. Potassium, calcium, and sulfur are in ample supply in aquatic ecosystems; nitrogen and phosphorus often aren’t. Therefore, phytoplankton growth in lakes and streams is based on the amount of phosphorus (P) and nitrogen (N) present in the water. When nutrient shortage limits plankton growth in an aquatic ecosystem, the system is called “oligotrophic” (Greek for ‘poorly nourished’). N and P are used by plankton to build proteins in an average ratio of 7 N atoms for every P atom. N is 20 times more abundant in most aquatic systems. It is most often P which is the limiting nutrient in aquatic ecosystems. Dams and reservoirs alter the natural nutrients available in aquatic ecosystems (see Aquatic Ecosystem Structure), affecting the phytoplankton first and then the rest of the aquatic food chain.

Because algae are so responsive to their environment, their population diversity and abundance can be a measure of the general health of the aquatic ecosystem. Overall, the extremely low abundance and biomass of the phytoplankton in the Arrow Lakes and the lack of seasonal blooms indicate an ultra-oligotrophic lake. The same phytoplankton are found throughout the lake. The most abundant belong to the phyla Cyanobacteria or blue green algae (>15,000 cells/mL during a September peak in the Lower Arrow), mainly represented by various species of Synechococcus. The next most abundant belong to the phyla Chrysophyta, represented by the nanoflagellate class Chrysophyceae and the diatom class Bacillariophyceae, and to the phyla Pyrrhophyta, represented by the dinoflagellate class Dinophyceae and the flagellate class Cryptophyceae. An algal bloom is a great burst of phytoplankton population growth following seasonal nutrient influxes in well nourished ecosystems. Algal blooms are no longer observed in Arrow Lakes, although phytoplankton populations do increase seasonally. The great numbers of the blue-green algae Synechococcus sp. coupled with the diverse and abundant array of Chrysophyceae and Cryptophyceae are clear and unambiguous indicators of the ultra-oligotrophic condition of Arrow Lake. Without healthy phytoplankton populations, the food web has no foundation to build upon, ultimately threatening unique stocks of fish.

In Kootenay Lake, the Dinophyceae (diatoms) have traditionally dominated, with Cryptophyceae and Chrysophyceae present and Cyanobacteria making up a very small part of the picture. A five year artificial fertilization experiment began in 1992 on Kootenay Lake, supplying phosphorus to phytoplankton, and they have increased in abundance since then (see Aquatic Ecosystem Management). The diatoms have responded particularly well, with Tabellaria, a species indicative of moderate nutrient availability, experiencing a large bloom in 1994. The following table demonstrates the positive impact fertilization has had on Kootenay Lake phytoplankton:

Year

   Annual phytoplankton biomass (mg/mm3)

 

   Station 2 (fertilized)

Station 6 (control)

1992

   445

   359

1993

   658

   364

1994

   900

   477

 

Arrow Lakes is now being fertilized also in the hopes of stimulating the food chain and preserving the trophy rainbow and bull trout stocks for which the Arrow Lake is renowned.

Zooplankton

Copepod zooplankton with egg sacs

Zooplankton are microscopic animals suspended in water. Zooplankton are heterotrophic which means they cannot make their own food and must, therefore, consume plants (herbivores) or animals (carnivores). Zooplankton are able to move about minimally to secure food or to migrate diurnally through the water column (moving up and down daily), occupying both the limnetic zone where sunlight penetrates and the dark profundal zone. Zooplankton are consumed in the light-filled limnetic zone by larger zooplankton, insects, and kokanee, which hunt visually, or in the profundal zone by crustaceans such as Mysis shrimp, decomposers and bottom feeders living there.

 

Daphnia, a Cladoceran zooplankton
drawings by Heather MacKay
 
All of the zooplankton discussed are greater than 150 um in size, as that was the pore size in the Clarke-Bumpus sampling net researchers used in the Kootenay and Arrow Lakes fertilization experiments.

Zooplankton abundance indicates that Arrow Lakes is less productive than Kootenay Lake, with 7 individuals/L as compared with 19 individuals/L, respectively. There was a greater proportion of cladocerans, the preferred food of kokanee and mysids, in the Arrow system. The Lower Arrow had an especially healthy population of water fleas, or Daphnia (see drawing), the cladoceran making up about 90% of kokanee’s diet.

 

Water flea, a Cladoceran zooplankton

Mysids

In 1949, mysid shrimp (Mysis relicta) were introduced into Kootenay Lake as an intermediate food source for rainbow trout as they grew and switched from eating Daphnia (zooplankton) to eating kokanee fry. An increase in the number and size of kokanee in the 1960’s was mistakenly attributed to the introduction of the mysid shrimp, which were thought to be acting as a food source for the kokanee. This resulted in the unfortunate introduction of mysids to hundreds of lakes in North America and Scandinavia. The mysids can be detrimental because, although some are eaten by kokanee, they also compete with the kokanee for plankton, their primary source of food.

Mysid shrimp, Mysis relicta

When fertilizing, mysid shrimp were an ecological wild card, leaving scientists unable to predict whether the shrimp would out-compete the kokanee for the new zooplankton food source expected. It is now believed that the shrimp graze on the zooplankton in the productive limnetic layer at night and then migrate down in the water column during the day where the kokanee are less able to hunt them. Kokanee hunt by sight in the limnetic layer during the day. The mysids show no growth trend as of yet, but they are being carefully monitored lest they suddenly upset the ecological apple cart.

Average annual mysid density in the Upper and Lower Arrow were 32 and 63 individuals per square meter, respectively, while Kootenay Lake had a density of 120 individuals per square meter. Although the mysid shrimp competition did not cause the collapse of the Arrow Lakes ecosystem, it could have been a direct contributor to the decline of the kokanee populations.

Fish

The Columbia Basin supports 27 native species of fish including rainbow trout, bull trout, kokanee, mountain whitefish, burbot and white sturgeon, as well as a number of smaller fish, some of which are now officially endangered (see Endangered Species). Changes to the physical structure of the system have eliminated the spawning migrations of several of these and caused other changes that have diminished the productive capacity of aquatic systems (see above). Consequently, many of the fish populations are currently in a state of stress (not to say crisis), and this is occupying considerable management attention (see Ecosystem Management).

The Columbia and its tributaries contain one of the most distinctive fish faunas in North America (Miller, 1965, in McPhail and Carveth, 1992), all of which probably survived the Pleistocene glaciations (see Earliest Beginnings) somewhere within the Columbia system. Nine Columbia species (35%) are endemic, i.e., they evolved within the system. No other drainage system in British Columbia contains this number of endemic species, and it is these Columbia endemics that set the B.C. freshwater fish fauna apart from that in the rest of Canada (McPhail and Carveth, 1992).

Because of the mountainous terrain, there are barriers (falls and rapids) on most upper Columbia tributaries, above which only trout or char occur. In the lower Columbia and Kootenay system, where the gradient lessens, the environment is more benign and the number of species increases until, near the U.S. border, all 27 native species and numerous exotics (see below) are present, either in the main rivers or their tributaries (McPhail and Carveth, 1992). However, the upstream distribution of a number of species of dace and sculpins has been limited by Bonnington Falls, on the Kootenay River below Kootenay Lake, and the 3-5 metre vertical drop where the Pend d'Orielle River enters the Columbia River (McPhail and Carveth, 1992).

In addition to the native species, some 16 exotic species (37%) now occur in the Columbia Basin. This is a higher proportion of introduced species than in any other river system in British Columbia (McPhail and Carveth, 1992). Most exotics (brook trout, brown trout, lake trout, broad whitefish, carp, goldfish, tench, brown catfish, black catfish, pumpkin seeds, black crappie, largemouth bass, smallmouth bass, yellow perch and walleye) are found in the lower Columbia and Okanagan drainages. One of these, largemouth bass, has become a sports fish (for example, at Duck Lake in the East Kootenay), but the others are mainly pests, or potential pests.

Brief notes on the major sports fish follow:

Kokanee (Oncorhynchus merka)

Kokanee, landlocked sockeye salmon, are present in large lakes and rivers throughout the Columbia Basin. They have small mouths and eat mainly zooplankton, preferring a diet of about 90% Daphnia. Kokanee feed during the day, hunting their food by sight. They will prey on mysid shrimp if possible, but the mysids feed in the dark and migrate down during the day to where no light penetrates and kokanee can't see them. In their night feedings, mysids are competitors for the limited zooplankton prey. Kokanee are a popular sport fish, and the main prey item for bull trout and large rainbow trout.

Kokanee show the first response to a decrease in lake productivity, so their numbers reflect the health of the ecosystem (Ney, 1996). The trend in Kootenay Lake kokanee numbers echoes dam construction, mysid introduction, fertilizer plant operations and lake fertilization, increasing in the1960s when the Kimberley fertilizer plant was fully operational, peaking in the early 1970s, dropping in the 1980s and declining steadily from 1986 to 1991. In 1991 kokanee numbers were about 150 fish per hectare. Research indicated a worsening crisis and convinced scientists and fisheries managers to proceed with fertilization on a trial basis. Since fertilization began in 1992, kokanee numbers have increased to their 1998 population density of 600 - 1000 fish per hectare, totalling 25 - 30 million kokanee in Kootenay Lake. There are roughly five million kokanee in the Arrow Lakes. They are found at depths between five and 35 m and preferably at temperatures between seven and 13.5 degrees C.

Bull Trout (Salvelinus confluentus)

Formerly called Dolly Varden trout (actually a char), bull trout are now recognized as a separate species. A consumate predator, bull trout have a large head, sharp teeth, and a relatively small, narrow body. They are blue-listed in British Columbia ("vulnerable") and are of management concern for various threats, including logging and hydroelectric development. For example, an estimated 4,000 adult spawners were lost to the Revelstoke dam alone (Pieters et al., 1998).

By providing more food (kokanee) for the resident Gerrard rainbow and bull trout populations in Kootenay Lake, fertilization has resulted in larger and more numerous stocks, benefiting the local sports fishery. Overall, both rainbow and bull trout in Kootenay Lake have been increasing by two pounds per year since fertilization began in 1992, with anglers now recording rainbow and bull trout as large as 29 pounds. A similar trend is hoped for in Arrow Lakes.

Bull trout raised at the Hill Creek Hatchery are released in Arrow Lakes at the mouths of various creeks. In 1996, for example, 29,077 bull trout were released into Snow, Illecillewaet, Hill and St. Leon Creeks. This program has been scaled back until fertilization has proven successful.

Cutthroat Trout (Oncorhynchus clarki lewisi)

Isolated populations of Westside cutthroats, a separate subspecies, occupy specific parts of the Columbia drainage. Blocked from migration by impassable falls, they have become so distinct that another species designation, O. c. alpestris, has been proposed (but not widely accepted) for those in the Revelstoke area, such as those in Akokolex Creek (McPhail and Carveth, 1992). Sometime after BC's last Ice Age, they occupied extensive ranges in the Columbia Basin in the absence of vigorous predators (such as bull trout). As the ice melted, the water level dropped, and natural dams, formed by massive ice chunks or terminal moraines, washed out. This isolated certain populations behind falls, while the rest occupied the lower elevation water ways. Later, predators accessed the system from downstream and eliminated all the fish below the falls. Thus, the populations above the falls diverged, evolving to succeed in their unique habitat. Thus, a legacy of variety remains in our native fish species, including unique ones like these relic populations of cutthroat trout.

Kootenay Trout Hatchery raises Westslope (Yellowstone) cutthroat trout to stock the area's smaller lakes. In 1996, for example, 33 lakes, primarily in the East Kootenays, were stocked with a total of 119,500 cutthroats for sport fishing.

Gerrard Rainbow Trout (a race of Oncohyrnchys mykiss)

22 pound (below) and 15 pound (right) Gerrard Rainbow Trout caught on Arrow Lakes Photos coutesy of Glen Olson Fishing Charters

The Gerrards, named for an abandoned mining town near their spawning grounds at the outlet of Trout Lake, are a giant race of rainbows that made Kootenay Lake famous for its fishing. However, fishing, nutrient overloading from a fertilizer plant, nutrient starvation because of power dams (Duncan, Libby) and the inappropriate introduction of an exotic crustacean (mysid shrimp) brought them to the edge of extinction, with only a few hundred breeding females observed from the early 1980s and onwards. The Gerrard rainbow trout have responded well to the fertilization of Kootenay Lake, achieving sizes of up to 29 pounds in 1998 and returning to spawn in greater numbers every year. Kootenay Trout Hatchery raises the Gerrard stock to release into smaller lakes in the East and West Kootenays and other parts of BC. In 1996, 16 lakes were stocked with 183,465 Gerrard rainbow trout. That year, a total of 1,002,628 rainbow trout (various stocks) were raised at the Kootenay Trout Hatchery and used to stock 113 different systems.

Yellowfin Rainbow Trout (a race of Oncohyrnchys mykiss)

The yellowfins, native only to Arrow Lakes, began disappearing soon after construction of the Keenleyside, Mica and Revelstoke dams, apparently having lost spawning habitat and nutrients. An estimated 3,000 adult were lost following dam construction (Pieters et al., 1998). They may be further threatened by the introduction of Gerrard rainbows into Arrow Lakes in the 1980s. These fish were large, up to 14 kg, with distinctive yellow colouration on their bellies, pectoral, pelvic and anal fins (Pieters et al., 1998). According to local anglers, a remnant population remains, yet they have proven elusive to fisheries biologists. Thus, attempts to preserve and enhance the stock have been unsuccessful so far.

Burbot or Ling Cod (Lota lota)

Ling cod caught on Arrow Lakes

Ling cod are considered primarily a coarse fish, although they are sought for food periodically. They are fished by jigging in ling holes where they swarm in small groups. They have elongated bodies, brown/yellow colouration and wide flat heads. Ling are predatory, with a diet consisting mostly of other fish. Ling cod are common in lakes throughout the Columbia Basin and all of North America.

 

 

White Sturgeon (Acipenser transmontanus)

White sturgeon are huge, long-lived fish, up to 800 kg in weight and over 100 years old (Cannings, 1993). A resident of large, cool rivers, they formerly occurred in the entire Columbia River, migrating from the ocean to spawn in its upper reaches. Until recently, because of dams, they are only found below Keenleyside Dam below Corra Linn Dam in the Kootenay system. In 1999, however, a small population has been found spawning in the Columbia River below Revelstoke Dam. They formed the basis of a commercial fishery for caviar in the early 1900s, and they still provide excellent eating where it is legal to catch them. They are not known to have spawned in these systems "...since the construction of the hydroelectric dams" altered their spawning habitat (Haas, 1996), and they may be further challenged by toxic chemicals and overfishing. According to Larson, 1998, "...construction and operation of hydropower systems have severely impacted white sturgeon populations in the Columbia River basin. Dams have not only blocked upstream spawning and feeding migrations, but they have also altered and/or destroyed much of the spawning habitat. Dams and their associated reservoirs have also altered food availability, natural flow patterns, and water temperatures." For more information: http://www.worldstar.com/~dlarson/SturgeonoftheColumbia.htm

References

Ashley et al., 1996. Fisheries Project Report No. RD 49, 1996.
Cannings, S., 1993. Rare Freshwater fish of British Columbia. B.C. Conservation Data Centre Report No. 1.
Haas, G.R., 1996. Categorization and assessment of indigenous fish species at risk in British Columbia, with recommendations and prioritizations for research, inventory and conservation. Fisheries Management and Environment Report, Ministry of Environment Lands and Parks.
Larson, D., 1998. Notes posted at http://www.worldstar.com/~dlarson/SturgeonoftheColumbia.htm
McLean, Stuart, 1992. Welcome Home. McGraw-Hill, Toronto.
McPhail, J.D. and R. Carveth, 1992. A foundation for conservation: The nature and origin of the freshwater fish fauna of British Columbia. Univ. of B.C.
Ney, 1996.
Pieters, R., L.C. Thompson, L. Vidmanic, S. Pond, J. Stockner, P. Hamblin, M. Young, K. Ashley, B. Lindsay, G. Lawrence, D. Sebastian, G. Scholten and D. L. Lombard, 1998.  Arrow Reservoir limnology and trophic status - Year 1 (1997/98) Report. B.C. Ministry of Environment, Lands and Parks.
 
 
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